Contents

A&A 439, 129-151 (2005)
DOI: 10.1051/0004-6361:20052967

The Hamburg/ESO R-process enhanced star survey (HERES)[*],[*]

II. Spectroscopic analysis of the survey sample

P. S. Barklem1 - N. Christlieb2 - T. C. Beers3 - V. Hill 4 - M. S. Bessell5 - J. Holmberg 6,7,8 - B. Marsteller 3 - S. Rossi 9 - F.-J. Zickgraf 2 - D. Reimers2


1 - Department of Astronomy and Space Physics, Uppsala University, Box 515, 751-20 Uppsala, Sweden
2 - Hamburger Sternwarte, Universität Hamburg, Gojenbergsweg 112, 21029 Hamburg, Germany
3 - Department of Physics and Astronomy and JINA: Joint Institute for Nuclear Astrophysics, Michigan State University, East Lansing, MI 48824, USA
4 - GEPI, Observatoire de Paris Meudon, 92125 Meudon Cedex, France
5 - Research School of Astronomy and Astrophysics, Australian National University, Cotter Rd, Weston ACT 2611, Australia
6 - Tuorla Observatory, Väisäläntie 20, 21500 Piikkiö, Finland
7 - Astronomical Observatory, NBIfAFG, Juliane Meries Vej 30, 2100 Copenhagen, Denmark
8 - Nordic Optical Telescope Scientific Association, Apartado 474, 38700 Santa Cruz de La Palma, Spain
9 - Departamento de Astronomia, IAG, Universidade de São Paulo, Rua do Matão 1226, 05508-900 São Paulo - SP, Brazil

Received 2 March 2005 / Accepted 2 May 2005

Abstract
We present the results of analysis of "snapshot'' spectra of 253 metal-poor halo stars $-3.8\leq {\rm [Fe/H]} \leq -1.5$ obtained in the HERES survey. The snapshot spectra have been obtained with VLT/UVES and have typically $S/N\sim 54$ per pixel (ranging from 17 to 308), $R\sim20~ 000$, $\lambda = 3760$-4980 Å. This sample represents the major part of the complete HERES sample of 373 stars; however, the CH strong content of the sample is not dealt with here.

The spectra are analysed using an automated line profile analysis method based on the Spectroscopy Made Easy (SME) codes of Valenti & Piskunov. Elemental abundances of moderate precision (absolute rms errors of order 0.25 dex, relative rms errors of order 0.15 dex) have been obtained for 22 elements, C, Mg, Al, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Zn, Sr, Y, Zr, Ba, La, Ce, Nd, Sm, and Eu, where detectable. Of these elements, 14 are usually detectable at the 3$\sigma $ confidence level for our typical spectra. The remainder can be detected in the least metal-poor stars of the sample, spectra with higher than average S/N, or when the abundance is enhanced.

Among the sample of 253 stars, disregarding four previously known comparison stars, we find 8 r-II stars and 35 r-I stars. The r-II stars, including the two previously known examples CS 22892-052 and CS 31082-001, are centred on a metallicity of ${\rm [Fe/H]} = -2.81$, with a very small scatter, on the order of 0.16 dex. The r-I stars are found across practically the entire metallicity range of our sample. We also find three stars with strong enhancements of Eu which are s-process rich. A significant number of new very metal-poor stars are confirmed: 49 stars with ${\rm [Fe/H]}<-3$ and 181 stars with $-3<{\rm [Fe/H]}<-2$. We find one star with ${\rm [Fe/H]}<-3.5$.

We find the scatter in the abundance ratios of Mg, Ca, Sc, Ti, Cr, Fe, Co, and Ni, with respect to Fe and Mg, to be similar to the estimated relative errors and thus the cosmic scatter to be small, perhaps even non-existent. The elements C, Sr, Y, Ba and Eu, and perhaps Zr, show scatter at ${\rm [Fe/H]} \la -2.5$ significantly larger than can be explained from the errors in the analysis, implying scatter which is cosmic in origin. Significant scatter is observed in abundance ratios between light and heavy neutron-capture elements at low metallicity and low levels of r-process enrichment.

Key words: stars: abundances - stars: population II - Galaxy: abundances - Galaxy: evolution - Galaxy: halo

1 Introduction

The Hamburg/ESO R-process Enhanced Star (HERES) survey has been described in the preceding paper in this series (Christlieb et al. 2004, hereafter Paper I). In this survey, "snapshot'' spectra of 373 very metal-poor stars, here meaning with ${\rm [Fe/H]} \leq -1.5$[*] as judged from medium resolution spectra, have been obtained with VLT2-UVES, with the main goal of finding stars enhanced in the r-process elements through detection of strong Eu II lines. Though the snapshot spectra are of what would generally be considered low quality for abundance analysis (typically $S/N\sim 54$, $R\sim20~ 000$, $\lambda = 3760$-4980 Å), they contain a wealth of information and abundances may be derived for a significant number of elements with moderate precision (absolute rms errors of order 0.25 dex, relative errors of order 0.15 dex). Modern surveys of metal-poor stars, such as the ESO "First Stars'' Large programme (Cayrel et al. 2004; Hill et al. 2002, and references therein), now obtain significantly better quality spectra for of the order of 70 stars, yet just a decade ago spectra of similar quality to our snapshot spectra were typical for studies of very metal-poor stars (e.g. McWilliam et al. 1995a,b). While high precision (better than 0.1 dex) is expected to be needed to discern detailed patterns in abundance distributions which might serve as diagnostics of early nucleosynthesis (e.g. Karlsson & Gustafsson 2001), the large number of stars observed in the HERES survey offers the possibility to investigate more general trends in metal-poor star abundances in a previously unexplored statistical regime. In particular, the scatter in abundance distributions may provide insights into mixing and the diversity of supernovae at early epochs. The study of Norris et al. (2001), which investigated such scatter, drawing from different surveys in the literature, had of order 70 stars in this metallicity regime. This project provides a homogeneously analysed sample of several hundred stars.

In this paper we analyse a total of 253 of the spectra using an automated spectrum analysis technique based on the Spectroscopy Made Easy (SME) codes by Valenti & Piskunov (1996). In Sect. 2 the sample, observations, and choice of initial stellar parameters will be described. In Sect. 3 the automated analysis technique and codes are described, including the line list, detection classification and error analysis, and the method is tested through comparisons with previously studied stars and tests of the robustness of the method. The results are presented in Sect. 4, including the new interesting stars found in the survey. In Sect. 5, we discuss general trends in the results and other interesting features to emerge. Finally, in Sect. 6 we present our conclusions and discuss possible uses for the data set.

 

 
Table 1: The sample. The entire table is available only electronically. Coordinates of the HES stars (prefix HE) have been derived from the Digitized Sky Survey I and are accurate to 1 $^{\prime \prime }$; the coordinates of the HK survey stars (prefix CS) are from identifications of the sources in the 2MASS All Sky Release. Barycentric radial velocities $v_{\rm rad}$ were measured from the snapshot spectra and are accurate to a few km s-1.
Star $\alpha(2000.0)$ $\delta(2000.0)$ $v_{\rm rad}$
      [km s-1]
CS 22175-007 02 17 26.6 -09 00 45 -18.3
CS 22186-023 04 19 45.5 -36 51 35 51.9
CS 22186-025 04 24 32.8 -37 09 02 -122.6
CS 22886-042 22 20 25.8 -10 23 20 -220.6
CS 22892-052 22 17 01.6 -16 39 27 14.5
CS 22945-028 23 31 13.5 -66 29 57 388.9
CS 22957-013 23 55 49.0 -05 22 52 -213.5
CS 22958-083 02 15 42.7 -53 59 56 175.6
CS 22960-010 22 08 25.3 -44 53 56 49.2
CS 29491-069 22 31 02.1 -32 38 36 -375.5
 $\vdots$ $\vdots$ $\vdots$ $\vdots$
HE 2338-1618 23 40 36.2 -16 01 28 -219.4
HE 2345-1919 23 47 55.4 -19 02 37 119.4
HE 2347-1254 23 50 09.8 -12 37 50 -43.5
HE 2347-1334 23 50 26.9 -13 17 39 -54.8
HE 2347-1448 23 49 58.3 -14 32 16 -165.1



 

 
Table 2: Derived stellar atmosphere parameters and elemental abundances for the sample. The entire table is available only electronically. This portion of the table is given as a guide to its form. For each star we report the average signal-to-noise ratio per pixel for the whole observed spectrum, the stellar parameters with their respective relative and absolute rms error estimates, $\sigma ^{\rm rel}$ and $\sigma ^{\rm abs}$, then for each element X the abundance $\log \epsilon_{\rm X}$ and its relative and absolute rms error estimates $\sigma_{\log\epsilon_{\rm X}}$, [X/Fe] and its relative and absolute rms error estimates $\sigma _{\rm [X/Fe]}$. N gives the number of features of the element used in each star, noting that this varies from star to star as certain features may be automatically rejected if the star has a strong G band, if the feature is near a Balmer line in warmer stars (see Sect. 3.2), or if they are determined to be affected by a cosmic ray hit or bad pixel. N3 then gives the number of those features classified as 3$\sigma $ detections. In the case of CH bands we simply classify detections and non-detections with 1 and 0 respectively. In the case of a non-detection, this is signified by an abundance of -9.99 and error of 0.00.
Star $S/N_{\rm av}$ $T_{\rm eff}$ $\sigma_{T_{\rm eff}}$ $\log g$ $\sigma_{\log g}^{\rm rel}$ $\sigma_{\log g}^{\rm abs}$ [Fe/H] $\sigma_{\rm [Fe/H]}^{\rm rel}$ $\sigma_{\rm [Fe/H]}^{\rm abs}$ $\xi $ $\sigma_\xi^{\rm rel}$ $\sigma_\xi^{\rm abs}$ $\log\epsilon_{\rm C}$ $\sigma_{\log\epsilon_{\rm C}}^{\rm rel}$ $\sigma_{\log\epsilon_{\rm C}}^{\rm abs}$ [C/Fe] $\sigma_{\rm [C/Fe]}^{\rm rel}$ $\sigma_{\rm [C/Fe]}^{\rm abs}$ N N3 ...
    [K]   [cm s-2]           [km s-1]                     ...
CS 22175-007 31 5108 100 2.46 0.26 0.36 -2.81 0.13 0.18 1.67 0.14 0.24 5.77 0.19 0.26 0.19 0.18 0.27 1 1 $\ldots$
CS 22186-023 55 5066 100 2.19 0.24 0.34 -2.72 0.13 0.18 1.58 0.11 0.21 5.97 0.19 0.25 0.30 0.18 0.27 1 1 $\ldots$
CS 22186-025 32 4985 100 1.70 0.26 0.36 -2.87 0.14 0.19 2.14 0.13 0.23 4.83 0.20 0.27 -0.68 0.19 0.29 1 1 $\ldots$
CS 22886-042 39 4881 100 1.85 0.25 0.35 -2.68 0.12 0.18 1.84 0.12 0.22 5.72 0.19 0.26 0.01 0.19 0.28 1 1 $\ldots$
CS 22892-052 46 4884 100 1.81 0.26 0.36 -2.95 0.14 0.19 1.67 0.12 0.22 6.44 0.19 0.26 1.00 0.18 0.28 1 1 $\ldots$
CS 22945-028 31 5126 100 2.55 0.26 0.36 -2.66 0.13 0.18 1.53 0.14 0.24 5.93 0.19 0.26 0.21 0.18 0.27 1 1 $\ldots$
CS 22957-013 35 4904 100 1.96 0.25 0.35 -2.64 0.14 0.19 1.79 0.12 0.22 5.85 0.19 0.26 0.10 0.17 0.27 1 1 $\ldots$
CS 22958-083 32 5101 100 2.40 0.26 0.36 -2.79 0.12 0.18 1.50 0.13 0.23 6.24 0.20 0.26 0.64 0.18 0.27 1 1 $\ldots$
CS 22960-010 35 5737 100 4.85 0.25 0.35 -2.65 0.12 0.17 1.53 0.17 0.27 6.56 0.17 0.24 0.82 0.16 0.25 1 1 $\ldots$
CS 29491-069 57 5103 100 2.45 0.24 0.34 -2.81 0.13 0.18 1.54 0.12 0.22 5.76 0.19 0.25 0.18 0.17 0.27 1 1 $\ldots$
$\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\vdots$ $\ldots$
HE 2338-1618 40 5515 100 3.38 0.27 0.37 -2.65 0.12 0.18 1.43 0.16 0.26 6.22 0.18 0.25 0.47 0.18 0.27 1 1 $\ldots$
HE 2345-1919 44 5617 100 4.46 0.25 0.35 -2.46 0.12 0.18 1.47 0.16 0.26 6.17 0.19 0.24 0.24 0.17 0.26 1 1 $\ldots$
HE 2347-1254 80 6132 100 3.95 0.24 0.34 -1.83 0.13 0.18 1.67 0.12 0.22 6.83 0.15 0.22 0.27 0.16 0.26 1 1 $\ldots$
HE 2347-1334 81 4453 100 0.95 0.24 0.34 -2.55 0.12 0.19 2.38 0.11 0.21 5.33 0.21 0.26 -0.50 0.18 0.27 1 1 $\ldots$
HE 2347-1448 43 6162 100 3.98 0.27 0.37 -2.31 0.12 0.18 0.84 0.17 0.27 6.58 0.18 0.24 0.50 0.19 0.27 1 1 $\ldots$


   
2 Observations and sample

The target selection for HERES and observational details have been described in Sect. 3 of Paper I. The spectra were obtained with the ESO-VLT2 and UVES, and cover a wavelength range of 3760-4980 Å, and have an average signal-to-noise ratio of $S/N\sim 54$ per pixel over the spectral range, though some spectra have S/N as low as 17 and as high as 308. A 2 $^{\prime \prime }$ slit is employed giving a minimum resolving power of $R\approx 20~000$, though typically the resolving power is seeing limited and thus slightly better. As mentioned in Paper I, the pipeline-reduced spectra are employed, corrected to the stellar rest frame. The sample of analysed stars is given in the electronic Table 1 with coordinates and barycentric radial velocities. The final stellar parameters of the sample are presented in Table 2, together with the abundances for convenience, and are plotted in Fig. 1. The [Fe/H] distribution for the sample from the final analysis is shown in Fig. 2. Though observations of adequate quality have been obtained for 373 stars, not all are analysed in this paper. Spectra showing strong molecular carbon features cannot be analysed by our current method, and thus 72 such spectra from the survey are not included in this sample for this reason. These spectra are, however, of great interest and it is planned that they will be analysed separately in future. Further, some stars which turned out to be too Fe-rich ( ${\rm [Fe/H]}>-1.5$) or too cool for our analysis method (<4200 K), or are suspected to be spectroscopic binaries or rotators, were also removed from the sample. For a small number of stars, we have not yet obtained adequate photometry and they are also removed from the sample. Thus, the final sample of stars analysed in this work presented in Tables 1 and 2 contains 253 stars.

   
2.1 Photometry and effective temperatures

To begin our analysis we require as accurate as possible estimates of the effective temperatures of HERES targets. This is particularly the case since, as noted below, the snapshot spectra we obtain are not generally of sufficiently high quality to derive precise spectroscopic temperature estimates. Hence, over the course of the past few years, we have obtained broadband $BVR_{\rm C}I_{\rm C}$ (where the subscript "C'' indicates the Cousins system) observations for as many HERES targets as possible, using the ESO/Danish 1.5 m telescope on La Silla and the DFOSC instrument. The observing and reduction techniques for this data are described in Beers et al. (2005, in preparation). We also make use of near-infrared ${\it JHK}$ photometry from the 2MASS Point Source Catalog (Cutri et al. 2003). The complete set of available photometry for stars in the HERES sample will be published in Beers et al. (2005, in preparation), a compilation of photometry for more than 1500 metal-poor stars and horizontal-branch candidates. The adopted reddening is taken from the maps of Schlegel et al. (1998), adjusted to account for distance. Note, all but the brightest giants of our sample lie outside the reddening layer and thus for most stars the full reddening is applied. The reddening data will also be presented in Beers et al.

  \begin{figure}
\par\includegraphics[width=7.1cm,clip]{2967f1.eps}
\end{figure} Figure 1: The $T_{\rm eff}$ versus $\log g$ Kiel diagram for the sample. The diameter of the circle for each star is proportional to [C/Fe]; cases where C is undetected are shown with an asterisk. The mean error bar is shown in the bottom right.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f2.eps}
\end{figure} Figure 2: The distribution of analysed stars in [Fe/H]. The [Fe/H] values are from the final analysis of the spectra.

Temperature estimates are obtained on the scale of Alonso et al. (1999). Note that, while the majority of the colour calibrations of Alonso et al. require measurements on the Johnson system, the near-IR colours J-H and J-K are on the TCS system (the photometric system at the 1.54 m Carlos Sanchez telescope; Arribas & Martinez-Roger 1987). Thus we first have to apply several transformations of our observed colours. We follow the prescription described by Sivarani et al. (2004). In performing our transformations, and for carrying out the Alonso et al. estimates of effective temperature, we made use of a program kindly provided to us by Sivarani. In order to arrive at a final "best estimate'' of the effective temperatures for our HERES pilot sample stars, we take a straight average of the derived estimates from different colour criteria, after trimming off the highest and lowest estimates for each star. The estimated effective temperatures, for the colours we had available, are provided in Table 2. Although errors in the determinations of temperature for individual colours arising from photometric errors can range from 50-100 K (for the optical colours), and up to several hundred K for the near-IR colours (owing to the generally larger errors in the 2MASS photometry), we conservatively estimate that our final determination of effective temperature has an absolute rms error of 100 K. We note that our photometry is incomplete, i.e. we do not have measurements of all colours for every star, and this incompleteness, together with the trimming in the averaging procedure, means there is an error introduced due to differences in the temperature scales from different colour criteria. Since the incompleteness is effectively random, this should lead only to a slight increase in random scatter. This has been considered in our error estimates. The error due to uncertain reddening (see discussion below) was also considered. We plan to obtain improved photometric estimates of $T_{\rm eff}$ for stars of particular interest on the HERES program (for instance, those noted to be r- and/or s-process enhanced) by measuring more precise ${\it JHK}$ photometry in the near future.

As will be discussed in Sect. 3.5.1, our temperatures are found to be systematically warmer than those found in the literature for the stars where comparisons can be made. This discrepancy was traced primarily to the use of different reddening maps. In this work, the maps of Schlegel et al. (1998) have been employed, while in the past most workers have used the maps of Burstein & Heiles (1982). We computed reddenings and effective temperatures using both maps and find systematic differences as seen in Fig. 3, the results using the maps of Burstein & Heiles being cooler than those found using Schlegel et al. by $70\pm58$ K. We have chosen to use the Schlegel et al. estimates, which have superior spatial resolution and are thought to have a better determined zero point. We note, however, that Arce & Goodman (1999) have pointed out that the Schlegel et al. maps may overestimate the reddening values when E(B-V) exceeds about 0.15 mag, though none of the stars considered here exceed that value (see also Beers et al. 2002 for further discussion).

It should be noted that while the HERES target selection aims at a cutoff of B-V>0.5, a number of warmer stars which turned out to be bluer than our targeted cutoff have also been included due to incorrect estimated B-V colours from the HES prism plates.

  \begin{figure}
\par\includegraphics[width=7.7cm,clip]{2967f3a.eps}\par\vspace*{3mm}
\hspace*{2mm}\includegraphics[width=8cm,clip]{2967f3b.eps}
\end{figure} Figure 3: Change in E(B-V) ( upper panel) and $T_{\rm eff}$ ( lower panel) if we adopt the reddening maps of Burstein & Heiles (1982) instead of those of Schlegel et al. (1998). The reddening corrections are usually reduced and thus the temperatures become somewhat cooler.

As will be described later in Sect. 3.3, we compute individual abundances for all Fe lines and thus can compare our adopted temperature scale with that implied by excitation equilibrium. Given the lines available to us, the spectroscopic data are not of sufficient quality to determine precise excitation temperatures, but one can make a comparison of the average temperature scale. Figure 4 plots the histogram of slopes of the best fit to the Fe I line abundances against excitation. On average the distribution is skewed towards negative slopes, indicating that our temperature scale is on average warmer than would be obtained from excitation equilibrium. Such trends have been noted in previous works on metal-poor giants and dwarfs, for example by Norris et al. (2001) and Cohen et al. (2004).


  \begin{figure}
\par\includegraphics[width=6.5cm,clip]{2967f4.eps}
\end{figure} Figure 4: Histogram of the slopes of fits to the trends of Fe I line abundances with excitation for the sample.

   
2.2 Other atmospheric parameters

Estimates of the metallicity, [Fe/H], which serve as initial guesses for our automated analysis, are derived from the medium-resolution spectra obtained during the course of the large-scale campaign to identify suitable targets for the HERES program (see Paper I), in combination with available B-V and J-K photometry. Estimates of [Fe/H] were obtained from the calibration of the Ca II K-line index, KP, along with the B-V colour, described by Beers et al. (1999). For most stars this calibration should be accurate to on the order of 0.2 dex, given spectra and photometry of suitable quality. In addition, we carried out a new calibration, making use of available J-K colours, and a newly-trained artificial neural network procedure (see Snider et al. 2001), to provide an alternative initial estimate of [Fe/H]. This latter step was taken because the HERES targets include objects that are known to be carbon-enhanced; the strong CH G-bands in these objects could possibly perturb the B-V colours used in the Beers et al. calibration. We take the average of the two determinations as our initial guess for [Fe/H]. The differences between the adopted initial guess and the final [Fe/H] values from the automated analysis of the high-resolution spectra are plotted in Fig. 5, and application of robust methods (see, e.g., Beers et al. 1990) to the set of differences in the initial and final metallicity determinations yield estimates of the mean offset and standard deviation of +0.04 dex and 0.27 dex, respectively. The mean estimated relative error for the high-resolution abundance determinations of [Fe/H] is 0.12 dex (see Sect. 3.4 and Table 2), indicating that the medium-resolution estimates have relative errors of about 0.24 dex. Note that the [Fe/H] estimates for the worst outliers were often based on rather noisy medium-resolution spectra.


  \begin{figure}
\par\includegraphics[width=7.5cm,clip]{2967f5a.eps}\par\vspace*{3mm}
\includegraphics[width=7.5cm,clip]{2967f5b.eps}
\end{figure} Figure 5: Difference between the final [Fe/H] as determined from the spectrum and the initial guess determined from medium-resolution follow-up spectroscopy, where $\Delta $[Fe/H] = [Fe/H](initial)-[Fe/H](final), plotted against $T_{\rm eff}$ and [Fe/H](final).

An initial estimate of the surface gravity, $\log g$, is also required, which is refined in the automated analysis. For stars on the subgiant and giant-branch stages of evolution, it is well known that $\log g$ correlates very well with effective temperature. Hence, in order to obtain a first-pass estimate of surface gravity we used the reported temperatures and surface gravities by Honda et al. (2004) to derive the regression relation:

 \begin{displaymath}\log g = -9.301 + 2.273 \; T_{\rm eff} / 1000 .
\end{displaymath} (1)

Note that the Honda et al. program considers stars over a very similar range of metallicities and temperatures as the HERES program. For warmer stars, this fit leads to overly high initial estimates, so we limited the initial guess to a maximum value of $\log g=4$. That is, if $T_{\rm eff} > 5850$ K an initial guess of $\log g=4$ is adopted, which was found to be adequate. Figure 6 shows the differences between the adopted initial estimate and the determination obtained from automated analysis of the snapshot spectra.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f6.eps}
\end{figure} Figure 6: Difference between the final $\log g$ as determined from the spectrum and the initial guess as described in the text, where $\Delta \log g = \log g {\rm (initial)} - \log g {\rm (final)}$.

As will be described in the next section, a 1D analysis is employed and turbulent line broadening is modelled via the classical microturbulence $\xi $ and macroturbulence $v_{\rm macro}$ parameters. These parameters are derived from the spectrum. Initial guesses of $\xi=1.8$ km s-1 and $v_{\rm macro}=1.5$ km s-1 were employed. The final values of $\xi $ derived from the spectrum are given in Table 2 and plotted in Fig. 7, showing the usual correlation with gravity. Note that the stars lying above the main trend, around $\log g \sim 2$ are the red horizontal branch stars (see Fig. 1).


  \begin{figure}
\par\includegraphics[width=7.6cm,clip]{2967f7.eps}
\end{figure} Figure 7: Plot of final microturbulence values $\xi $ as derived from the spectrum against gravity. Note that the stars lying higher than the general trend are the red horizontal branch stars (see Fig. 1).

   
3 Automated spectrum analysis

   
3.1 Analysis code

Software for automated analysis of the spectrum has been developed, based on the Spectroscopy Made Easy (SME) package by Valenti & Piskunov (1996). SME consists of three components: a spectrum synthesis component written in C++, a parameter optimisation component written in IDL, and a user interface written in IDL. In this work we make use of the first two components. Our developed software is written in IDL, and essentially provides an alternative interface to the parameter optimisation component, which in turn calls the spectrum synthesis component. We also made some minor adaptations and improvements to the SME codes, the most important of which are discussed below. The new interface software takes our input data and provides it to the parameter optimisation component without any need for user interaction. The input data in this case consist of a pipeline-reduced count spectrum with corresponding measurement error spectrum (corrected to the stellar rest frame), initial guess stellar atmosphere parameters and abundances (see Sect. 3.3), and a list of spectral features with corresponding atomic or molecular data (see Sect. 3.2). The main tasks of the new interface software are, in a completely automated fashion, to extract relevant spectral regions appropriate for the line list, to identify continuum points and normalise the spectra relative to the continuum, to make small adjustments (within the error of the wavelength calibration) to line central wavelengths such that they match the observed line centres, and to reject lines polluted by artifacts such as cosmic ray hits. The continuum points are identified by an automated procedure where for each spectral region required for the analysis, the continuum is determined for a wide region, including the desired spectral region and 7 Å on each side by iteratively fitting a low order polynomial to the count spectrum and discarding points more than one standard deviation below the fitted line in the subsequent iteration, thereby converging to the continuum high points. Cosmic ray hits are identified by being significantly above this fit.

Given the input data in the correct form, the SME parameter optimisation code can then solve for any desired model parameters. The parameter optimisation code uses the Marquardt algorithm (Marquardt 1963; Press et al. 1992) to obtain estimates of the parameters, through minimising the $\chi^2$ statistic comparing model and observed spectra.

The spectrum synthesis assumes LTE and a 1D plane-parallel model of the atmosphere, where turbulence is modelled through the classical microturbulence and macroturbulence parameters. Note that in recent versions of SME, molecular line formation is supported (see Valenti et al. 1998), and for speed the radiative transfer is solved using a Feautrier scheme (e.g. Mihalas 1978) not a Runge-Kutta scheme (cf. Valenti & Piskunov 1996). The original spectrum synthesis code did not account for scattering in the source function, i.e. continuous scattering is treated as absorption and thus $S_\nu = B_\nu$. Rayleigh scattering by neutral hydrogen can be an important contributor to continuous opacity particularly in the ultraviolet for metal-poor stars, especially giants, and thus it is important to treat continuous scattering correctly in the source function (e.g. Griffin et al. 1982). It should be computed as $S_\nu = (1-\epsilon_\nu) J_\nu + \epsilon_\nu B_\nu$ where $\epsilon_\nu$ is the photon thermalisation probability given by $\kappa_\nu/(\kappa_\nu+\sigma_\nu)$ where $\kappa_\nu$ is the absorption coefficient (including line absorption) and $\sigma_\nu$ is the continuum scattering coefficient. This has been implemented into the SME spectrum synthesis code, where the mean intensity $J_\nu$ has been solved using the perturbation technique of Cannon (1971). Further minor improvements included correction of Thorium partition functions (see Paper I), and the ability to handle data for line broadening by neutral hydrogen collisions from the Anstee, Barklem & O'Mara theory (see Sect. 3.2).

A grid of 1D, plane-parallel, LTE models covering the stellar atmosphere parameter space of the stars of interest, namely low metallicity F, G, and K stars from the main sequence to the giant stage, was computed using the 1997 MARCS code (Asplund et al. 1997; Gustafsson et al. 1975). All models use scaled solar abundances with the exception of the alpha-elements, which are enhanced by 0.4 dex. Throughout this paper solar abundances means those of Grevesse & Sauval (1998), except C which is taken from Allende Prieto et al. (2002). Microturbulence in the line blanketing of 2 km s-1 was adopted as most of our stars are giants (see Fig. 7). This should not have a great effect in metal-poor stars in any case. This model grid was incorporated into SME, allowing SME to solve for atmospheric parameters, where specific models are obtained by interpolation.

In Sect. 3.3 we will describe how we apply this code. First we describe the adopted line list.

   
3.2 Line list

A list of spectral lines and corresponding atomic and molecular data, suitable for our sample of stars, observational data, and analysis technique is required. For our automated line profile analysis technique, spectral windows where the model and observed spectrum are to be compared need also to be defined.

The lines and spectral windows used are listed in Tables A.1-A.5 in Appendix A, along with comments on each element. Note that in order to avoid the cores of strong lines, any wavelength points in the chosen spectral windows where the observed flux is less than 0.5 of the continuum are automatically rejected. The line list and windows were, for the most part, built by selecting suitable lines from previous studies, particularly McWilliam et al. (1995a,b), Norris et al. (1996), and Sneden et al. (1996). As our technique is automated, our aim is to build a line list which requires either no adjustment from star to star, or possibly a small amount of adjustment that can be automated based on criteria that are known in advance of the analysis, such as stellar temperature. We must therefore be more selective than in interactive analyses. One must keep in mind, however, the need to have as many lines as possible to provide better statistics, which is particularly important for low-quality spectra. Ideally we would like to choose lines which for all stars of the type we are examining are unblended, or which are partially blended in such a way that they can be used if an appropriate comparison window is chosen that neglects the blended part of the line (usually one wing of the line).

Our first step for selecting the lines was to apply all candidate lines to an automated abundance analysis of four stars viewed to be extreme cases of possible blending for metal-poor stars. We used HD 20, moderately r-process enhanced, which is one of the most metal-rich of our stars, non-carbon-enhanced; CS 31082-001, an r-process enhanced, non-carbon-enhanced star; CS 22892-052 an r-process enhanced, carbon-enhanced star; and HE 0338-3945, an r- and s-process enhanced, carbon-enhanced star. Based on examination of the four spectra we chose appropriate spectral windows for each line, rejecting lines where a suitable window for all four stars could not be easily chosen. We then performed an abundance analysis of each star and rejected lines which were not well fit by the derived abundance with respect to the majority of lines of that element, indicating most likely an unresolved blend, or possibly poor atomic data. Special attention was paid to lines that were blended in the carbon-enhanced stars, but not in the carbon-normal stars. We chose to only make use of these lines for the carbon-normal stars, as described below. These lines are marked with an asterisk in the line list. To err on the side of caution, we also used some other very carbon-enhanced stars in the sample, which we deemed too carbon-rich for our present method, to indicate other lines which could be blended by carbon features. Finally, the line list and windows were refined based on testing using the complete sample.

We empirically determined that the lines noted above to be blended in the carbon-enhanced stars, could be safely applied in stars where the G band has a depth not greater than 0.6 of the continuum flux. Further, in the warmer stars some chosen lines lie in the wings of high Balmer lines. Thus, we empirically derived a scheme for application of the line list to a given star. The list is applied to all stars with the following adjustments:

These adjustments are fully automated.

While the employed spectral lines were chosen from the above mentioned previous studies, we compiled our own atomic data for these lines, though often guided by these works. In particular, we attempted to update the data. The adopted oscillator strengths are discussed for each element in Appendix A. The VALD database[*] (Kupka et al. 1999) and NIST Atomic Spectra Database[*] (see also Wiese et al. 1969; Wiese & Martin 1980; Martin et al. 1988; Fuhr et al. 1988) were used extensively, particularly for wavelengths and excitation energies. Radiative broadening, Stark broadening and collisional broadening by neutral hydrogen are included, though the data have not been presented in the tables; they may be obtained from the authors on request. Radiative broadening is taken in all cases from VALD, which is supplied from the calculations by Kurucz (1995). Collisional broadening by neutral hydrogen is, where possible, described by the Anstee, Barklem and O'Mara theory (e.g. Anstee & O'Mara 1991; Barklem et al. 2000 and references therein). In the absence of such calculations the data are taken from VALD which again originates from Kurucz (1995) using the van der Waals theory (Unsöld 1955) with a detailed calculation of the long range interaction constant C6. In the absence of data from both of these sources the classical van der Waals theory is used, where C6 is estimated by the usual Unsöld approximation. In both the last two cases we apply an enhancement of a factor of 2. Stark broadening is taken from VALD where available, which often originates from Kurucz (1995). We note that since the lines are typically weak, collisional mechanisms are generally not important, except in a few lines which attain significant strength (e.g. the strongest lines of Mg, Sr and Ba).

Where possible we have considered the hyperfine structure of spectral lines. Hyperfine structure is typically seen in elements with odd atomic numbers. Though Sr and Ba have even atomic numbers, in the solar system they have non-negligible abundances of isotopes with odd atomic masses, and thus hyperfine structure must be considered in these elements also. Isotopic mixtures and splitting have been considered in Sr, Ba and Eu. In all other elements the dominating natural isotope is assumed (or equivalently in the case of even atomic numbers that isotopes with even atomic masses dominate and they have negligible isotope shift). Details of adopted hyperfine structure and isotopic ratios are discussed for each element in Appendix A where it is considered. Hyperfine structure and isotopic splitting have been omitted from the tables for compactness. They may be obtained on request from the authors.

   
3.3 Procedure

We now describe the procedure used for analysis of the spectra. The goal is to determine the required stellar atmosphere parameters and abundances from the spectra in the best possible way. In Sect. 3.1 a code was described which can analyse a given spectrum to obtain best estimates of chosen model parameters. While the code can in principal analyse the entire set of spectral lines and obtain all desired stellar parameters and abundances simultaneously in one step, this is not done, since for cases with many free model parameters such a procedure is susceptible to errors if strong dual dependencies of the model spectra on parameters exists. Thus, our procedure, like traditional analyses, separates the determination of stellar parameters using appropriate spectral features from the determination of abundances as we now describe.

First, the $T_{\rm eff}$ from Sect. 2.1 is adopted and held fixed throughout. We experimented with refining $T_{\rm eff}$ from the spectra (essentially excitation equilibrium of Fe I), but found that the spectra are not of sufficiently high quality given the spectral features available to us. Thus we need to solve for the atmosphere parameters surface gravity $\log g$, microturbulence $\xi $, macroturbulence $v_{\rm macro}$, and metallicity [Fe/H]. Once these parameters are known we then solve for the individual abundances. All stars are assumed to be slow rotators; we adopt $v \sin i = 1$ km s-1 for all stars, and this has no effect on the final abundances. Since the resolving power of observations can vary from star to star, we fix the instrumental broadening at a value R=50 000, significantly higher than expected and allow the derived macroturbulence to compensate for the difference. Thus our derived $v_{\rm macro}$ includes both the macroturbulence and a degree of the instrumental profile.

Our basic procedure is broken into three steps. In the first two steps we employ only the Fe and Ti lines of our list. In the first step initial estimates of $T_{\rm eff}$, $\log g$, [Fe/H], $\xi $ and $v_{\rm macro}$ as described in Sects. 2.1 and 2.2 are adopted. The initial guess Ti abundance is chosen to be a scaled solar value based on the [Fe/H] initial guess. We then solve for the Fe and Ti abundances, $\log \epsilon_{\rm Fe}$[*] and $\log \epsilon_{\rm Ti}$ to obtain better initial estimates of these parameters before solving for the remaining stellar parameters.

The second step repeats the first, but now $\log g$, $\xi $ and $v_{\rm macro}$ are also free parameters. The minimisation to solve for $\log g$ is in essence equivalent to performing an ionisation equilibrium procedure for Fe and Ti. The resultant parameters ($\log g$, $\xi $, $v_{\rm macro}$, [Fe/H], $\log \epsilon_{\rm Ti}$) are then adopted and held fixed for stage three, the analysis of lines of elements other than Fe and Ti in the list, where the only free parameters are the elemental abundances. All the remaining elements are considered separately, as this is most computationally efficient. Solar abundances scaled by [Fe/H] are adopted as initial guesses, which was found usually to be satisfactory; on rare occasions where convergence was not achieved this could be solved by searching for an initial guess which resulted in convergence. Note that in all steps, the single abundance which gives the best global fit to the spectrum is derived. It is also worth noting that we adopt scaled solar abundances for all elements which we do not analyse, except O which we assume enhanced by +0.4 dex; these abundances enter the molecular equilibrium and continuous opacity calculations.

An additional stage is performed for checking purposes. In this stage we analyse the Fe and Ti line list keeping all parameters fixed to those derived in the above stages except the abundance which may now vary from line to line (in SME this can be achieved in practice by fixing the abundance and solving for $\log gf$ for each line, and observing the change from the $\log gf$-value in the line list). This permits us to check for trends with excitation and ionisation stage, which might warn of deficiencies in the adopted model.

Three further steps are then performed which are required for the error analysis, the details of which will be described below in Sect. 3.4 and in Appendix B. However, for the error analysis we will require partial derivatives describing the dependence of each abundance on $T_{\rm eff}$, $\log g$ and $\xi $. Thus we solve for all abundances with fixed stellar parameters except that $T_{\rm eff}$, $\log g$ and $\xi $ are offset by 100 K, 0.3 dex and 0.2 km s-1 in each step respectively. We note that these last three steps increase computing time significantly (they comprise more than 1/2 of the computing time). However, we view the error analysis as important enough to justify this increase.

It is worthwhile to make some comment on computing times. With the large number of molecular lines, isotopic and hyperfine components, our line list results in approximately 900 individual line components to be included in the spectrum synthesis, which is where the vast majority of computation is used. Model convergence typically requires approximately 3.5N+13 model spectrum calculations, where N is the number of free parameters (Valenti & Piskunov 1996). This means for the main abundance step (step 3) we require of the order of 15 model spectrum calculations of the complete spectrum. This is repeated three additional times for the error calculations. With a modern workstation typical computation times per star are of the order of 2-3 hours.

   
3.4 Elemental detections and errors

A first important step before assigning an error to a derived abundance is to determine if there is in fact a reliable detection. A Gaussian is fit to each line and the approximate equivalent width W is determined. Following Norris et al. (2001), the error in W is then computed as $\sigma_W = \lambda\sqrt{n}/(R[S/N])$ where R is the resolving power, n the number of pixels integrated to obtain W, and S/N the signal to noise ratio per pixel. In all cases we adopted R=20000 and adopted the full-width of the fitted Gaussian measured in pixels for n. By then computing $m= W/\sigma_W$ we classify a $m\sigma$ detection of the line. For each element we count the number of lines detected at the $3\sigma$ level or better. If the element has at least one line detected at the $3\sigma$ level we assign the abundance as a detection. Otherwise the element is regarded as undetected, and the derived abundance discarded. Due to the possibility of weak blending, even in high quality spectra, it was further required that a line must be deeper than 10% of the continuum flux for a valid detection. Due to decreased likelihood of blending in the redder parts of the spectrum, we relaxed this condition to 5% for lines redder than 4500 Å. A similar detection scheme was used for CH bands, though W and n for the considered band must be estimated by a different technique.

 

 
Table 3: Comparison of our final stellar parameters with those adopted in the literature for the comparison stars. $T_{\rm eff}$ derived with the reddening maps of Burstein & Heiles (1982) instead of Schlegel et al. (1998) are also given for comparison.
Star This work Literature Reference/note
  $T_{\rm eff}$ $\log g$ [Fe/H] $\xi $ $T_{\rm eff}$ $\log g$ [Fe/H] $\xi $  
  [K] [cm s-2]   [km s-1] [K] [cm s-2]   [km s-1]  
HD 20 5445 2.39 -1.58 2.30 5351       Alonso et al. (1999)
          5475 2.8 -1.4 2.0 Burris et al. (2000)
          5375 2.41 -1.4 1.90 Fulbright & Johnson (2003)
  5416               Using Burstein & Heiles (1982)
HD 221170 4648 1.57 -2.14 2.22 4410       Alonso et al. (1999)
          4425 1.0 -2.0 1.5 Burris et al. (2000)
          4500 0.9 -2.1 2.75 Fulbright (2000)
          4475 1.15 -2.2 2.40 Fulbright & Johnson (2003)
  4548               Using Burstein & Heiles (1982)
CS 22186-025 4985 1.70 -2.87 2.14 4900 1.5 -3.0 2.0 Cayrel et al. (2004)
  4887               Using Burstein & Heiles (1982)
CS 22892-052 4884 1.81 -2.95 1.67 4800 1.5 -3.1 1.95 Sneden et al. (2003)
  4843               Using Burstein & Heiles (1982)
CS 31082-001 4922 1.90 -2.78 1.88 4825 1.5 -2.9 1.8 Hill et al. (2002)
  4874               Using Burstein & Heiles (1982)


As one of the main goals of this work is to look at abundance scatter at low metallicities, and given the relatively low quality of the data, it is vital to have error estimates which are as accurate as possible to distinguish real scatter from that due to uncertainties. Thus, we have put significant effort into obtaining realistic error estimates.

Usually in analyses of stellar spectra, systematic errors are expected to dominate. This is not necessarily the case here. For elements with a small number of spectral features, the low S/N means that random measurement errors can be significant. However, for elements with a significant number of spectral features, e.g. Fe, measurement errors are in fact quite small, and systematic errors will dominate.

Our method for calculating errors in abundances and abundance ratios is detailed in Appendix B. First, we should emphasise that we make a distinction between absolute and relative errors. In our discussion we will refer to the uncertainty in the absolute abundance or abundance ratio as the absolute error, and the uncertainty in the relative abundance between stars, that is from star to star, as the relative error. Appendix B provides a formalism for calculation of both absolute and relative errors; however, throughout this paper, unless otherwise stated we discuss the relative error. This is of most interest as we are interested in distributions of abundances. The main difference between absolute errors and relative errors is that some systematic sources of error are presumed to cancel in the latter, in particular, errors in oscillator strengths and some part of the errors incurred from modelling uncertainties such as LTE and 1D. We note however, that as our sample covers such a large stellar parameter space, the cancellation of errors from the modelling will be only partial.

The error estimates include contributions from uncertainties in the observations, atomic and molecular data, continuum fitting, stellar parameters, model atmospheres and inherent assumptions in the spectrum modelling such as LTE and 1D. We have included as many sources of error as possible, however, some of these uncertainties are difficult to estimate quantitatively, particularly those related to the model atmospheres and modelling assumptions. Our abundances and error estimates are provided with the explicit understanding that they are based on traditional 1D LTE models and spectrum synthesis. Corrections for 3D and non-LTE effects often should be applied by the user. For example, it is known that the resonance line of Al is subject to strong deviations from LTE (e.g. Baumüller & Gehren 1997). While corrections for cases such as Al where only a single line is employed are relatively straight forward, we point out that for other elements one needs to consider the correction to the best fit to all spectral features used here.

3.5 Tests of the automated method

Before presenting the results for the sample, we present the results of some tests on our automated method. In particular, we compare our results where possible with the literature, and perform test calculations to assess the robustness of the automated method at low S/N.

   
3.5.1 Comparison stars

Five stars, namely HD 20, HD 221170, CS 22186-025, CS 22892-052 and CS 31082-001, which have been studied in detail with better quality observational material by others, were included in our pilot sample. Four of these were included in the sample for the specific purpose of use as comparison stars, while CS 22186-025 has been recently observed as part of the ESO First Stars programme (Cayrel et al. 2004). We now present a comparison of our results with some of the literature studies. For CS 22186-025, CS 22892-052, and CS 31082-001, we compare with the studies of Cayrel et al., Sneden et al. (2003), and Hill et al. (2002), respectively. For HD 20 and HD 221170 there are a number of different studies which have included these stars. For the purpose of clarity, for the abundances of these two stars we chose to concentrate our comparison on just one study, that of Burris et al. (2000), which includes both these stars and has reasonable overlap with our work in terms of the elements analysed.

First, in Table 3 we compare our stellar parameters for these stars with those used in the literature. Our temperatures are seen to be systematically warmer than those found in the literature for the comparison stars by of order 100 K. As mentioned in Sect. 2.1, and has been noted by other authors for individual stars (e.g. Hill et al. 2002, Sneden et al. 2003), the reddening maps of Schlegel et al. (1998) give larger reddenings than those of Burstein & Heiles (1982). As shown in Fig. 3 this leads to systematic differences in $T_{\rm eff}$, of around 100 K. In Table 3 we also quote our temperatures using the lower reddenings of Burstein & Heiles. These temperatures agree well with the literature within error (of order $\pm 100$ K). The remaining parameters agree reasonably well, given the typical absolute error bars of $\sigma_{\log g} \sim 0.35$ dex, $\sigma_{\rm [Fe/H]}\sim 0.10$ dex, and $\sigma_\xi \sim 0.15$ km s-1. Considering the effect of the systematic offset in $T_{\rm eff}$ we see, in line with expectations, that it usually leads to slightly higher $\log g$ values (+100 K  $\rightarrow$ +0.2 dex), and slightly higher metallicities (+100 K  $\rightarrow$ +0.1 dex).

To demonstrate the quality of the stellar parameter solutions, Fig. 8 plots abundances derived for individual Fe and Ti lines (the checking step of the procedure) against lower level excitation potential and wavelength of the line. Lines of the neutral and singly ionised species are distinguished in the plots, and thus it is clearly seen that the derived $\log g$ values satisfy ionisation equilibrium for both Fe and Ti. The plots against excitation potential, particularly for Fe, demonstrate that our spectra are not of sufficiently high quality to specify $T_{\rm eff}$ with the required precision as seen from the large scatter in the plot for CS 22186-025 which has $S/N\sim 32$. The plots show our temperatures are reasonably consistent with excitation equilibrium (noting of course that one may question the validity of 1D LTE excitation equilibria); however, as discussed in Sect. 2.1 we find that on average excitation equilibria would give a cooler temperature scale. Finally, the plots against line wavelength indicate no significant systematic effects in the bluer lines due to blending or continuum placement. We also checked for significant trends with line strength and found none. Similar results were obtained for all stars in the sample.


  \begin{figure}
\par\includegraphics[width=6.7cm,clip]{2967f8a.eps}\hspace*{3mm}
...
...c.eps}\hspace*{3mm}
\includegraphics[width=6.7cm,clip]{2967f8d.eps}
\end{figure} Figure 8: Plots showing trends of abundances found from individual Fe and Ti lines with excitation potential $\chi $ ( left column) and wavelength $\lambda $ ( right column) for two comparison stars, CS 22186-025 $S/N\sim 32$ and CS 31082-001 $S/N\sim 90$. Circles and crosses indicate lines from the neutral and singly ionised species respectively. The dashed line in each case shows the determined abundance from the simultaneous best fit to all lines.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f9a.eps}\hspace*{3mm}
...
...mm}
\includegraphics[width=7.4cm,clip]{2967f9e.eps}\hspace*{7.2cm}\end{figure} Figure 9: Comparison of abundances for stars previously studied in the literature. Differences are in the sense of $\Delta \log \epsilon = \log \epsilon_{\rm this\; work} - \log \epsilon_{\rm literature}$. Error bars indicate the estimated absolute error in our result. The mean difference and standard deviation $\sigma $ are reported.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f10a.eps}\includegraphics[width=7.4cm,clip]{2967f10b.eps}
\end{figure} Figure 10: Comparison of abundances as in Fig. 9, where we have adopted the same temperature as the literature study.

Figure 9 compares abundances for our comparison stars with results from the literature. The results show generally reasonable agreement within error, thus supporting not only our method for obtaining abundances, but our error estimates as well. For CS 22892-052 and CS 31082-001 there is a systematic offset which is a result of our slightly warmer temperatures. This is clearly demonstrated by Fig. 10, where we compare results for CS 22892-052 and CS 31082-001 where we have reanalysed the spectra adopting the temperatures used in the relevant literature work. The remaining small differences are likely attributable to use of different lines and atomic data, particularly oscillator strengths and hyperfine structure.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f11.eps}
\end{figure} Figure 11: Comparison of abundances as in Fig. 9, for HD 20 where we have adopted the same temperature, gravity and microturbulence as Burris et al. (2000).

The differences for HD 20 and HD 221170 are not improved by adopting temperatures used by Burris et al. (2000), which originate from Pilachowski et al. (1996). For HD 20, our temperature is already in reasonable agreement with that of Burris et al., yet we obtain systematically lower abundances by of the order of 0.3 dex. We reanalysed the spectrum adopting the stellar parameters of Burris et al., and the new comparison shown in Fig. 11 shows a significant improvement. Thus, the main reasons for the differences are our significantly higher microturbulence and lower gravity. We found no evidence of a significant trend of Fe abundance with line strength or ionisation stage to indicate our microturbulence or gravity solutions are in error. In spite of the fact that our stellar parameters for HD 221170 differ significantly from those adopted in Burris et al., the abundances are in reasonable agreement, probably due to compensation of the $T_{\rm eff}$, $\log g$ and microturbulence differences. Note that this star has a large colour excess $E(B-V)\approx 0.12$ in our sample, and a large discrepancy with the Burstein & Heiles maps (see Fig. 3).

While these systematic offsets, of order 0.1-0.2 dex, are present and attributed to differences in stellar parameters, perhaps the most important result is the scatter in the difference, as this indicates the accuracy with which the abundance pattern in a given star is reproduced. We find for all comparisons scatter of 0.1 to 0.15 dex. Thus we conclude that the relative abundance patterns are accurate to of order 0.15 dex, within our quoted error bars.

   
3.5.2 Robustness at low S/N

Since most of our comparison stars are relatively bright, the spectra are usually of higher S/N than is typical for this project. The lowest quality comparison star spectrum is that of CS 22186-025, which has on average $S/N\approx 32$ per pixel. As some of our spectra are of even lower quality, it is important to ascertain what effect S/N has on our results. It should be pointed out that, provided our detection classification method and error estimates are reasonable, the pertinent issues are: (a) what is the minimum precision in abundances that is useful, and (b) what S/N is necessary to achieve it.

 

 
Table 4: Comparison of results for CS 31082-001 using spectra with degraded S/N. The difference from our results using the original spectrum $S/N\approx 90$ in Table 2 is quoted, with the relative error in the derived abundance for the degraded S/N in parentheses. A blank means a non-detection (below 3$\sigma $) at this S/N for this star.
Parameter $\Delta $ Parameter
  S/N = 30 20 15 10
$\log g$ +0.01 (0.26) +0.05 (0.27) -0.08 (0.26) 0.00 (0.34)
$\xi $ -0.04 (0.18) -0.07 (0.18) -0.08 (0.18) -0.16 (0.20)
$\log\epsilon({\rm C}) $ -0.02 (0.20) -0.10 (0.20) -0.07 (0.20) -0.19 (0.22)
$\log\epsilon({\rm Mg})$ -0.04 (0.12) -0.06 (0.12) -0.02 (0.12) -0.02 (0.13)
$\log\epsilon({\rm Al})$ -0.19 (0.19) -0.14 (0.30) -- --
$\log\epsilon({\rm Ca})$ -0.02 (0.12) -0.04 (0.12) -0.06 (0.11) -0.06 (0.14)
$\log\epsilon({\rm Sc})$ -0.02 (0.17) 0.00 (0.18) -0.09 (0.19) --
$\log\epsilon({\rm Ti})$ -0.03 (0.16) -0.02 (0.16) -0.04 (0.16) --
$\log\epsilon({\rm V}) $ -- -- -- --
$\log\epsilon({\rm Cr})$ -0.06 (0.17) -0.09 (0.19) -- --
$\log\epsilon({\rm Mn})$ -0.07 (0.16) -0.11 (0.18) -0.03 (0.19) --
$\log\epsilon({\rm Fe})$ -0.02 (0.13) 0.00 (0.12) -0.02 (0.13) 0.00 (0.15)
$\log\epsilon({\rm Co})$ -0.05 (0.16) -- -- --
$\log\epsilon({\rm Ni})$ -0.08 (0.20) -0.09 (0.23) -0.21 (0.25) --
$\log\epsilon({\rm Zn})$ -- -- -- --
$\log\epsilon({\rm Sr})$ +0.01 (0.15) +0.01 (0.17) 0.00 (0.19) -0.07 (0.23)
$\log\epsilon({\rm Y}) $ -0.04 (0.18) -0.03 (0.19) -- --
$\log\epsilon({\rm Zr})$ -0.04 (0.18) -- -- --
$\log\epsilon({\rm Ba})$ -0.04 (0.15) -0.03 (0.16) +0.05 (0.16) +0.01 (0.21)
$\log\epsilon({\rm La})$ -0.02 (0.18) -- -- --
$\log\epsilon({\rm Ce})$ -- -- -- --
$\log\epsilon({\rm Nd})$ -0.02 (0.19) -- -- --
$\log\epsilon({\rm Sm})$ -- -- -- --
$\log\epsilon({\rm Eu})$ -0.01 (0.18) -0.01 (0.19) -0.15 (0.19) --


To investigate this we took the spectrum of CS 31082-001, which has $S/N\approx 90$, and degraded it to lower S/N values by multiplying with appropriate Poisson noise and rescaling so that count numbers are consistent with the noise level. These spectra were then run through the entire automated spectrum analysis process completely independently from the original spectrum. The differences in derived atmosphere parameters (noting the model [Fe/H] is determined by the Fe abundance) and abundances for four degraded spectra compared to the original spectrum are given in Table 4, along with the relative error bar for that derived parameter. First, we note that almost every difference reported was less than our computed error bar for the degraded spectrum, giving confidence in our estimated errors. Secondly, the differences are generally reasonable for most elements, less than 0.1 dex. However, it is immediately obvious that for most elements there is a systematic trend towards slight underestimation of the abundances. We attribute this systematic trend to systematically lower continuum placement, which is to be expected, since at low S/N it is impossible to distinguish weak lines from continuum. Therefore, there should be a natural trend towards the continuum being placed too low, and thus underestimation of abundances, as the weak lines make the continuum appear slightly lower. This problem could perhaps be circumvented if one a priori defined continuum regions from higher quality spectra to be used for normalising the spectra; however such a procedure would be dependent on the similarity of the spectra. As noted, the error in the abundance at this S/N is much larger in any case.

Based on these results, we conclude that our method seems to be reasonably robust even at S/N as low as 15 for elements with a large number of lines, such as Fe and Ti. However, as one expects, detections for a number of elements cannot be made at such low S/N for stars of this metallicity. Elements with a small number of lines which are still detectable at low S/N at this metallicity, for example Mg, Ca and Ni, are less robust, but at S/N>15 the induced error usually does not appear to exceed of order 0.1 dex.

3.5.3 Example fits to spectra

Examples of portions of the spectra, and fits to the data obtained, are shown in Fig. 12 for an r-process enhanced star HE 1127-1143. The example was chosen to be representative of the sample; it is a giant star with $S/N\sim 49$, typical for the sample.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f12a.eps}\hspace*{3mm}...
...\vspace*{3mm}
\par\includegraphics[width=16.4cm,clip]{2967f12c.eps}
\end{figure} Figure 12: Examples of the spectra and fits for HE 1127-1143 (an r-process rich star), which has average $S/N\sim 49$, $T_{{\rm eff}}=5224$ K, $\log g\sim2.6$, ${\rm [Fe/H]}\sim -2.7$, and is thus reasonably typical for the sample. The double line is the observed spectrum and the single line the fitted model spectrum (noting that it is not only the plotted observations which are being fit, but all considered lines of the element). The shaded regions are the comparison windows used for fitting.

   
4 Results

The derived stellar parameters and elemental abundances for the sample are presented in Table 2. Below, we note and discuss objects of particular interest found in the sample. In the next section we will discuss the more general behaviour of the abundances and implications for understanding the chemical evolution of the Galactic halo.

It is worth emphasising that some care must be taken in interpreting the results presented here involving elements which are not always, or even usually, detected in our spectra, which may lead to selection effects. Fourteen elements, C, Mg, Al, Ca, Sc, Ti, Cr, Mn, Fe, Co, Ni, Sr, Y and Ba, are almost always detectable at the 3$\sigma $ level in the spectra. Another eight elements are analysed, V, Zn, Zr, La, Ce, Nd, Sm and Eu, which can usually only be detected in the spectra of the least metal-poor stars of our sample, spectra with higher than usual S/N, if the abundance is enhanced, or a combination of these factors. Thus, particular care must be taken in interpreting results involving these eight elements as the data are incomplete.

   
4.1 Objects of interest

The complete sample consists of 253 stars, of which four were comparison stars already known to be r-process enhanced metal-poor stars. Among the remainder we have identified a number of interesting objects, which we will now summarise. For the discussion in this subsection (Sect. 4.1) we consider only the 249 other stars as "the sample''. Though CS 22186-025 has been recently observed by Cayrel et al. (2004) it is included in our statistics as it had not been observed at the time of selection.

First, this work adds significantly to the number of confirmed very metal-poor stars. The [Fe/H] distribution for the sample is shown in Fig. 2. The sample contains 49 stars with ${\rm [Fe/H]}<-3$, and 181 stars with $-3<{\rm [Fe/H]}<-2$. Only 12 stars are currently known with ${\rm [Fe/H]}<-3.5$ (Beers & Christlieb 2005) and we find just one new star in this regime, HE 1300+0157 with ${\rm [Fe/H]}=-3.76\pm0.18$. This star is at the base of the giant branch ( $T_{\rm eff}\sim 5400$ K, $\log g \sim 3.4$) and is carbon enhanced with ${\rm [C/Fe]} \sim 1.2$.

The main goal of the HERES survey is to identify r-process enhanced stars, to address questions about the r-process. We were able to detect both Eu and Ba at the $3\sigma$ level in 62 stars in the sample. Of these, 57 are judged to be "pure'' r-process stars, as they have ${\rm [Ba/Eu]}<0$, see Fig. 13. In Paper I we made the distinction between r-I and r-II stars, $0.3 \leq {\rm [Eu/Fe]} \leq 1.0$ and ${\rm [Eu/Fe]} > 1.0$ respectively (and ${\rm [Ba/Eu]}<0$ in both cases), on the basis that previous work had suggested a bimodal distribution of [Eu/Fe] with a lack of stars found in the range between 1.0 and 1.5. A histogram of detected [Eu/Fe], is plotted in Fig. 14; however, due to the significant incompleteness of the Eu abundances and the detection bias towards high [Eu/Fe], only the high [Eu/Fe] side of this distribution is reliable, and thus this plot gives little information about the cosmic distribution. We will return to the question of the distribution of r-process enhancement in Sect. 5.3. Following this classification system, of these 57 stars, eight are r-II stars ( ${\rm [Eu/Fe]} > 1.0$) which are listed in Table 5 (two of which were announced in Paper I), and 35 are r-I stars ( $0.3 \leq {\rm [Eu/Fe]} \leq 1.0$), while 14 do not have r-process enhancement ( ${\rm [Eu/Fe]} < 0.3$). This implies a frequency of around 3% and >14% for r-II and r-I stars respectively among metal-poor stars ( ${\rm [Fe/H]}<-1.5$). It must be borne in mind that these frequencies are dependent on detection in our spectra, and thus are certainly lower limits, particularly for r-I stars. For example, at the lowest metallicities, an r-I star would often not be detectable with our typical spectra.

  \begin{figure}
\par\hspace*{2mm}\includegraphics[width=7.6cm,clip]{2967f13a.eps}\par\vspace*{3mm}
\includegraphics[width=7.3cm,clip]{2967f13b.eps}
\end{figure} Figure 13: A plot of [Ba/Eu] vs. [Fe/H] (upper panel) and [C/H] (lower panel). The horizontal full line shows the pure solar r-process value, computed from the solar r-process fractions of Arlandini et al. (1999), and the dashed line the solar s-process value. The pure r-II stars are shown as stars, the r-I stars as diamonds, the pure r-process stars without excess r-process elements as triangles, the s-II stars as asterisks, and the two remaining s-process-rich stars as squares. The average relative error bar is shown in the bottom left.


  \begin{figure}
\par\includegraphics[width=7.1cm,clip]{2967f14.eps}
\end{figure} Figure 14: Histogram of [Eu/Fe] values. The dashed line includes all stars where Eu was detected, including the four comparison stars. The full line includes the pure r-process stars only (i.e. ${\rm [Ba/Eu]}<0$ noting Ba must be detected; for a small number of stars where Eu was detected, Ba was not detected due to cosmic ray pollution of the Ba II resonance line) and excludes the comparison stars.

The abundance patterns for the neutron-capture elements for the eight r-II stars are shown in Fig. 15, along with the scaled solar system r-process abundances, demonstrating that these elements follow this pattern in these stars. In fact, all 57 pure r-process stars, as judged from Ba/Eu, follow the pattern quite well for Ba and heavier elements. The lighter neutron-capture elements, Sr, Y and Zr, tend to deviate from the solar-r-process pattern in stars of lower r-process enrichment, which will be discussed in Sect. 5.4. The scaled solar system s- and r-process abundances used throughout this paper are based on the s-process fractions from the stellar model of Arlandini et al. (1999), the assumption that the remainder of neutron-capture elements are produced by the r-process, and meteoritic abundances from Grevesse & Sauval (1998). We chose the Arlandini et al. (1999) fractions over those of Burris et al. (2000) for our comparisons, since we found consistently better agreement with Y abundances in the pure r-process stars. The abundance patterns are otherwise very similar for the other neutron-capture elements considered here.


 

 
Table 5: New r-II and s-II objects. Quoted error estimates are relative errors. N3 is defined in the caption to Table 2.
Star $T_{\rm eff}$ $\log g$ [Fe/H] N3 [C/Fe] N3 [Ba/Fe] N3 [Eu/Fe] N3 [Ba/Eu]
  [K] [cm s-2]                  
r-II stars
CS 29491-069 5103 2.45 $ -2.81\pm 0.13$ 46 $ 0.18 \pm 0.17$ 1 $ 0.34 \pm 0.19$ 1 $ 1.06\pm 0.15$ 2 $ -0.71\pm 0.17$
CS 29497-004 5013 2.23 $ -2.81\pm 0.13$ 42 $ 0.22 \pm 0.18$ 1 $ 1.21 \pm 0.15$ 1 $ 1.62\pm 0.15$ 4 $ -0.41\pm 0.17$
HE 0430-4901 5296 3.12 $ -2.72\pm 0.12$ 46 $ 0.09 \pm 0.18$ 1 $ 0.50 \pm 0.20$ 1 $ 1.16\pm 0.17$ 3 $ -0.65\pm 0.17$
HE 0432-0923 5131 2.64 $ -3.19\pm 0.13$ 41 $ 0.24 \pm 0.17$ 1 $ 0.72 \pm 0.18$ 1 $ 1.25\pm 0.15$ 2 $ -0.53\pm 0.16$
HE 1127-1143 5224 2.64 $ -2.73\pm 0.14$ 46 $ 0.54 \pm 0.17$ 1 $ 0.63 \pm 0.19$ 1 $ 1.08\pm 0.15$ 3 $ -0.45\pm 0.18$
HE 1219-0312 5140 2.40 $ -2.81\pm 0.12$ 44 $ -0.08 \pm 0.19$ 1 $ 0.51 \pm 0.25$ 1 $ 1.41\pm 0.17$ 3 $ -0.91\pm 0.21$
HE 2224+0143 5198 2.66 $ -2.58\pm 0.12$ 54 $ 0.35 \pm 0.17$ 1 $ 0.59 \pm 0.18$ 1 $ 1.05\pm 0.15$ 4 $ -0.46\pm 0.16$
HE 2327-5642 5048 2.22 $ -2.95\pm 0.12$ 50 $ 0.43 \pm 0.19$ 1 $ 0.66 \pm 0.19$ 1 $ 1.22\pm 0.17$ 4 $ -0.56\pm 0.17$
s-II stars
HE 0131-3953 5928 3.83 $ -2.71\pm 0.11$ 22 $ 2.45 \pm 0.18$ 1 $ 2.20 \pm 0.16$ 2 $ 1.62\pm 0.19$ 2 $ 0.58\pm 0.18$
HE 0338-3945 6162 4.09 $ -2.41\pm 0.13$ 23 $ 2.07 \pm 0.16$ 1 $ 2.41 \pm 0.15$ 2 $ 1.89\pm 0.16$ 2 $ 0.51\pm 0.16$
HE 1105+0027 6132 3.45 $ -2.42\pm 0.13$ 34 $ 2.00 \pm 0.17$ 1 $ 2.45 \pm 0.16$ 2 $ 1.81\pm 0.16$ 4 $ 0.64\pm 0.19$



  \begin{figure}
\par\includegraphics[width=4.7cm,clip]{2967f15a.eps}\hspace*{1.5m...
...hics[width=4.7cm,clip]{2967f15h.eps}\hspace*{1.5mm}\hspace*{4.7cm}\end{figure} Figure 15: Abundance patterns for neutron-capture elements in the r-II stars of the sample. The full line shows the scaled solar system r-process abundances based on the r-process fractions from Arlandini et al. (1999), meteoritic abundances from Grevesse & Sauval (1998), scaled to match our observed Eu abundance. Plotted error estimates are relative errors.

The eight r-II stars are all giants with $T_{\rm eff}\sim 5100$ K, and have a quite narrow range in metallicity, $-3.2 \leq {\rm [Fe/H]} \leq -2.6$. The r-II stars, including the two previously known examples CS 22892-052 and CS 31082-001, are centred on a metallicity of ${\rm [Fe/H]} = -2.81$, with a very small scatter, on the order of 0.16 dex. Note, we find one r-II star with ${\rm [Fe/H]}<-3$ among 49 stars in our sample, a frequency of 2%, and 7 r-II stars among 118 stars in the range $-3<{\rm [Fe/H]}<-2.5$, a frequency of 6%. This perhaps indicates that r-II stars are more rare at ${\rm [Fe/H]}<-3$; further study in a larger sample with better spectra would be desirable to resolve this question more definitively. All eight r-II stars have quite normal C/Fe abundances, the largest being ${\rm [C/Fe]} \sim 0.5$, noting of course that the present sample is biased towards CH weak stars. The low C abundances mean that these stars are all candidates for studies of the actinide elements, particularly Th and U, in such stars. CS 22892-052 remains a unique object as the only r-II star known with ${\rm [C/Fe]}\sim 1$.

The majority of the r-I stars are also giants, however, four such stars are unevolved (i.e. not yet on the giant branch $T_{\rm eff} > 5500$ K, $\log g > 3$), namely HE 0341-4024, HE 0534-4615, HE 0538-4515 and HE 2301-4024. As seen in Fig. 17 the r-I stars span the range $-3.4 \leq {\rm [Fe/H]} \leq -1.5$, practically the entire metallicity range of our sample. We note that the four unevolved stars all have ${\rm [Fe/H]} \geq -2.1$, but that there is a selection effect at work here; the Eu II lines observed will be weaker in unevolved stars than in evolved stars with the same abundances, and thus our survey preferentially detects Eu in giant stars. Our survey is also biased towards cool giants as described in Paper I.

  \begin{figure}
\par\includegraphics[width=4.7cm,clip]{2967f16a.eps}\hspace*{2mm}...
....eps}\hspace*{2mm}
\includegraphics[width=4.4cm,clip]{2967f16c.eps}
\end{figure} Figure 16: Abundance patterns for neutron-capture elements in the s-process rich stars of the sample with strong Eu enhancement, ${\rm [Eu/Fe]}> 1.5$, the s-II stars. The full line shows the scaled solar system r-process abundances based on the r-process fractions from Arlandini et al. (1999), meteoritic abundances from Grevesse & Sauval (1998), scaled to match our observed Eu abundance. The dashed line shows the equivalent scaled solar system s-process abundances, scaled to match our observed Ba abundance. Plotted error estimates are relative errors.

Five stars in which both Eu and Ba were detected are found to be s-process rich as judged from their having ${\rm [Ba/Eu]}>0.5$[*]. All five are carbon-enhanced, and three are strongly Eu enhanced with ${\rm [Eu/Fe]} > 1.0$. The three stars with ${\rm [Ba/Eu]}>0.5$ and ${\rm [Eu/Fe]} > 1.0$, are listed in Table 5. A number of similar stars are known; e.g. Hill et al. (2000), Aoki et al. (2002b) and Cohen et al. (2003). We shall refer to these stars as "s-II'' stars, though we note that whether the neutron-capture elements in such stars are produced predominantly by the s-process or by both the s- and r-processes is a matter of current debate (e.g. Johnson & Bolte 2004). We note that these three stars all have large C enhancements ${\rm [C/Fe]}>1.5$, and are unevolved. It must be borne in mind, however, that since this sample is limited to the stars with spectra only weakly polluted by CH features, we were only able to analyse the warmest strongly C enhanced stars. The complete HERES sample contains 72 CH strong stars which were not analysed here, among which there will be a large number of s-process rich stars. As we will discuss in the next section, a further such s-II star is suspected based on other abundances, but is not confirmed as Eu is detected at below the 3$\sigma $ level.

The remaining two s-process rich stars with ${\rm [Ba/Eu]}>0.0$ yet more normal Eu enhancement ( ${\rm [Eu/Fe]}<0.6$) have abundance patterns of neutron-capture elements which are reasonably well matched by a scaled solar s-process abundance pattern. Figure 16 shows the abundance patterns for the three s-II stars. In these cases the Ba, La, Ce and Nd abundances can be well reproduced by a scaled solar-system s-process abundance pattern. The Sr and Y abundances, however, are much lower. We notice, however, that these abundances are consistent with the scaled solar system r-process abundance pattern normalised to Eu. On the other hand, the s-process is expected to be skewed towards heavier elements in metal-poor environments (e.g. Busso et al. 1999). A summary of suggested possible production scenarios for the s-process rich metal-poor stars has been recently given by Johnson & Bolte (2004). As stated by those authors, to distinguish different scenarios more strongly, measurements of as many heavy elements as possible are needed, and studies of these stars using better observational material will be the subject of future work as part of the HERES survey.

   
5 Discussion

5.1 Abundance trends and scatter with metallicity

We now discuss the general behaviour of the abundances, particularly trends and scatter in abundance ratios of interest. The abundance ratio trends of [X/Fe] with [Fe/H] and [X/Mg] with [Mg/H] have been plotted in Figs. 17 and 18 respectively for elements with a reasonable number of detections. The estimated $1\sigma $ scatter in the y-variable is shown, following the definition for the scatter used by Karlsson & Gustafsson (2005), such that at a given x-coordinate 32% of the stars lie outside the $1\sigma $ scatter lines, 16% above and below. In practice, this has been computed for a given x-coordinate by taking the n nearest stars in the x-variable, where n is the lesser of n=50 or $n_{\rm stars}/3$, with $n_{\rm stars}$ being the number of stars in the diagram. The results are smoothed over the average width of bins containing n stars to remove transient behaviour caused by outliers. In Table 6 we compare the mean measured scatter in [X/Fe] and [X/Mg], across the range of [Fe/H] and [Mg/H] respectively, with the average error estimates. The minimum and maximum measured scatters are also reported to give an indication of the range of variation with [Fe/H] and [Mg/H].


  \begin{figure}
\par\includegraphics[width=5cm,clip]{2967f17a.eps}\hspace*{2mm}
\...
...egraphics[width=5cm,clip]{2967f17q.eps}\hspace*{2mm}
\hspace*{5cm}\end{figure} Figure 17: Abundances ratios [X/Fe] plotted against [Fe/H] for elements with significant numbers of detections. Full lines show estimated $1\sigma $ scatter. The average relative error bars are shown in the bottom left. Note differing scales on the y-axes.


  \begin{figure}
\par\includegraphics[width=5cm,clip]{2967f18a.eps}\hspace*{2mm}
\...
...egraphics[width=5cm,clip]{2967f18q.eps}\hspace*{2mm}
\hspace*{5cm}\end{figure} Figure 18: Abundances ratios [X/Mg] plotted against [Mg/H] for elements with significant numbers of detections. Full lines show estimated $1\sigma $ scatter. The average relative error bars are shown in the bottom left. Note differing scales on the y-axes.


 

 
Table 6: Comparison of measured scatter in Figs. 17 and 18 with relative errors in the abundance ratios. For each plot we report the minimum, mean and maximum measured $1\sigma $ scatter $\sigma _{\rm meas}$ across the range of [Fe/H] or [Mg/H], which is compared to the average relative error in the abundance ratio $\sigma ^{\rm rel}$. The ratio of the mean measured scatter to the estimated error $\langle \sigma_{\rm meas} \rangle /\sigma^{\rm rel}$ is reported in the last column.
  min( $\sigma _{\rm meas}$) $\langle \sigma_{\rm meas} \rangle$ max( $\sigma _{\rm meas}$) $\sigma ^{\rm rel}$ $\langle \sigma_{\rm meas} \rangle /\sigma^{\rm rel}$
[C/Fe] 0.22 0.32 0.53 0.18 1.73
[Mg/Fe] 0.07 0.09 0.12 0.15 0.59
[Al/Fe] 0.17 0.20 0.21 0.17 1.13
[Ca/Fe] 0.08 0.09 0.10 0.15 0.59
[Sc/Fe] 0.09 0.11 0.13 0.16 0.69
[Ti/Fe] 0.08 0.09 0.12 0.15 0.61
[V/Fe] 0.06 0.09 0.11 0.15 0.60
[Cr/Fe] 0.10 0.12 0.14 0.16 0.72
[Mn/Fe] 0.13 0.16 0.21 0.16 1.03
[Co/Fe] 0.10 0.11 0.13 0.16 0.71
[Ni/Fe] 0.12 0.14 0.17 0.18 0.80
[Zn/Fe] 0.08 0.15 0.19 0.15 1.01
[Sr/Fe] 0.19 0.32 0.59 0.19 1.71
[Y/Fe] 0.21 0.25 0.32 0.17 1.47
[Zr/Fe] 0.13 0.19 0.23 0.16 1.18
[Ba/Fe] 0.37 0.50 0.69 0.18 2.77
[Eu/Fe] 0.21 0.37 0.62 0.16 2.34
[C/Mg] 0.24 0.35 0.51 0.18 1.89
[Al/Mg] 0.15 0.19 0.23 0.18 1.03
[Ca/Mg] 0.07 0.08 0.09 0.15 0.56
[Sc/Mg] 0.10 0.11 0.12 0.18 0.60
[Ti/Mg] 0.08 0.09 0.11 0.17 0.55
[V/Mg] 0.12 0.13 0.14 0.16 0.79
[Cr/Mg] 0.12 0.15 0.19 0.18 0.84
[Mn/Mg] 0.17 0.21 0.30 0.17 1.26
[Fe/Mg] 0.08 0.10 0.14 0.15 0.63
[Co/Mg] 0.11 0.13 0.16 0.17 0.79
[Ni/Mg] 0.15 0.17 0.19 0.19 0.88
[Zn/Mg] 0.09 0.18 0.26 0.15 1.16
[Sr/Mg] 0.18 0.29 0.55 0.21 1.41
[Y/Mg] 0.23 0.25 0.30 0.19 1.36
[Zr/Mg] 0.15 0.22 0.29 0.17 1.27
[Ba/Mg] 0.33 0.48 0.60 0.20 2.40
[Eu/Mg] 0.22 0.39 0.60 0.18 2.18


For Mg, Ca, Sc, Ti, Cr, Fe, Co, and Ni, the measured scatters are slightly less than the scatters expected from the typical estimated relative error in the abundance ratios, suggesting that our computed errors overestimate the real relative error. Bearing in mind the difficulties in accurately calculating the errors, this suggests that the cosmic scatter is small (or even non-existent) at these metallicities. These results are in line with previous results for smaller samples with smaller uncertainties for some of these elements, such as the studies by Arnone et al. (2005), Cayrel et al. (2004) and Cohen et al. (2004). It should be noted that in all these elements, apparent outliers may perhaps be explained simply by the errors in the analysis; in a sample of 253 stars outliers due to random errors are expected. In particular, examining the outliers we noted that they often showed trends in the abundances derived from individual Fe I lines with excitation that were at the edge of the distribution of such slopes for the entire sample (see Fig. 4), and occur in elements where particularly temperature sensitive spectral features have been employed, such as Co and Ni. Thus, we believe that more often than not for these elements, the outliers are more likely due to errors in the analysis, such as $T_{\rm eff}$ being in error, than indicative of any real over- or under-abundance of the element in question.

The results for Al, V, Mn and Zn are less clear. In the case of Al, the scatters are marginally larger than the typical error bars; however, we note the Al abundances are based on a single line and are very sensitive to the S/N of the spectrum (see Table 4). Further, this line is known to be subject to deviations from LTE. Both these facts may lead to increased scatter in the derived abundances. In the cases of V and Zn, the number of detections is small and the abundances for these elements are based on quite weak features and are therefore susceptible to overestimation due to unresolved blends. For Mn, the scatter at low metallicity does marginally exceed the error estimates, with the hint of a "bump'' of Mn enhanced stars at around ${\rm [Fe/H]}\sim -3$. A similar feature is suggested by the results of Cayrel et al. (2004).

The elements C, Sr, Y, Ba and Eu, and perhaps Zr, show scatter at low metallicities, ${\rm [Fe/H]} \la -2.5$ and ${\rm [Mg/H]} \la -2.2$, significantly larger than can be explained from the errors in the analysis, implying the scatter is cosmic in origin. At higher metallicities the scatter among the non-C-rich stars, does not greatly exceed that expected from the errors in the analysis, but perhaps indicates some cosmic scatter. Note, the scatter in [Ba/Fe] and [Ba/Mg], and to a lesser degree Sr and Y, at higher [Fe/H] and [Mg/H] is affected by C-enhanced stars which have high Ba/Fe and Ba/Mg ratios, see Fig. 28. The scatter at low metallicity seems, in most cases, to be increasing monotonically with decreasing metallicity. Similar results have been found, for example, by McWilliam et al. (1995b), McWilliam (1998), Norris et al. (2001), and Burris et al. (2000). The results of Norris et al. (2001) suggested the existence of a larger scatter in [Sr/Fe] than for [Ba/Fe] at the lowest [Fe/H]. We do not find this result; the scatters are of comparable magnitude. Note that in contrast to the results for lighter elements discussed above, the cases of under-abundances and over-abundances of these elements with respect to the general trends are sometimes significant.

In summary, among the stars without strong C enhancement, at about ${\rm [Fe/H]} \ga -2.5$ or equivalently ${\rm [Mg/H]} \ga -2.2$, our analysis indicates that the cosmic scatter in all abundance ratios is small. This implies that at around this level of enrichment the Galactic halo was reasonably well mixed. At lower metallicities C, Sr, Y, Ba and Eu all show evidence for real cosmic scatter, while the results for the remaining elements still admit only a small amount of cosmic scatter within the errors of our analysis. This dichotomy implies that while the lack of scatter in these elements at ${\rm [Fe/H]} \ga -2.5$ might be explained by a well mixed Galactic halo, the small scatter at ${\rm [Fe/H]} \la -2.5$ has a different explanation. One possibilty is suggested by the stochastic models of metal-poor enrichment by Karlsson & Gustafsson (2005). The small scatter among the most metal-poor stars may be tentatively explained by cosmic selection effects in contributing supernova masses, and a relatively narrow range of masses of gas the newly synthesised elements mix with (so called mixing masses). Alternatively, as suggested by Arnone et al. (2005), the scatter in C, Sr, Y, Ba and Eu at these metallicities might be explained by the addition of sources of these elements which produce negligible amounts of the other elements such as Mg and Fe, such as low mass supernovae of type II.

5.2 Carbon

The work of Bromm & Loeb (2003) suggests that halo stars with low C abundances, ${\rm [C/H]}\sim-3.5$ according to their model, and low oxygen abundances, are probably true second generation stars. In Fig. 19 we plot the [C/H] values for our sample, identifying evolved (on the giant branch or red horizontal branch) and unevolved stars (all others). Though we do not have oxygen abundances, we see the majority of stars lie above the -3.5 level. It would be interesting to obtain O abundances for the stars lying near or below ${\rm [C/H]}\sim-3.5$ to identify likely second generation stars among this sample.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f19.eps}
\end{figure} Figure 19: A plot of [C/H] versus [C/Fe] following Bromm & Loeb (2003). Giants and red horizontal branch stars are plotted as open circles, while the subgiants and dwarfs are plotted as filled circles.

   
5.3 Heavy neutron-capture elements, Ba-Eu

Figure 13, which we used earlier as a measure of r- vs. s-process enrichment, plots [Ba/Eu] against Fe and C abundances. The plots show a clear separation between two groupsin the halo, a separation which correlates with C enrichment. This distinction was first seen in McWilliam (1998), though with fewer stars. The scatter among the pure r-process stars is consistent with the observational uncertainties and we thus conclude that the cosmic scatter in Ba/Eu among pure r-process halo stars is small. This implies that the Ba/Eu abundances produced by the r-process in the early Galaxy are universal. Taking the weighted mean (weights are based on absolute errors), we find for the pure r-process stars analysed in this work $\langle {\rm [Ba/Eu]} \rangle = -0.58 \pm 0.03$, where the quoted error is the weighted standard deviation. The solar system r-process abundance ratio, based on the data from Arlandini et al. (1999), is -0.65. Our result seems to be in disagreement with that found at low metallicities by Truran et al. (2002), who compiled data from a number of studies, and found a large scatter in Ba/Eu. They noted the difficulties in analysing Ba in metal-poor spectra due to dependence on hyperfine and isotopic structure and microturbulence. This is particularly problematic when combining data from different studies. Our data on the other hand are homogeneously analysed, but the Eu abundances are incomplete and biased towards stars with strong r-process enhancement.

It has been suggested (e.g. Burris et al. 2000; Truran et al. 2002; Simmerer et al. 2004) that La may be a better alternative as a tracer of the s-process enrichment. Unfortunately, as the lines available to us are typically weak, La is often undetected in our low S/N spectra according to our detection criteria. When plotting [La/Eu] vs. [Fe/H], Fig. 20, we see no trend or significant scatter. Among the pure r-process stars $\langle {\rm [La/Eu]} \rangle = -0.40 \pm 0.05$. The solar system r-process abundance ratio is -0.38.


  \begin{figure}
\par\includegraphics[width=7.6cm,clip]{2967f20.eps}
\end{figure} Figure 20: A plot of [La/Eu] vs. [Fe/H]. Symbols and lines have the same meanings as in Fig. 13.

As mentioned in Sect. 4.1, the distribution of r-process enhancement in the early Galaxy is of great interest. This is usually traced by [Eu/Fe], but our data are incomplete due to the inability to reliably detect low Eu abundances in our snapshot spectra. One may, however, try to reconstruct the r-process enhancement by instead using the Ba abundances, which are practically complete due to the ease of detecting the Ba II resonance line at 4554 Å. Following Raiteri et al. (1999) and Burris et al. (2000), where possible we attempt to reconstruct the r-process-only contribution to Ba. We define the ratio ${\rm [Ba/Fe]}_{r-{\rm process}} = \log ( N_{{\rm Ba},r} / N_{\rm Fe} )_\star - \log (N_{{\rm Ba},r} / N_{\rm Fe})_{\rm\odot}$, where $N_{{\rm Ba},r}$ indicates the r-process-only Ba abundance. Note, the zero point of the scale is set at the solar r-process-only Ba abundance, not the total solar Ba abundance. For the pure r-process stars, ${\rm [Ba/Fe]}_{r-{\rm process}} = {\rm [Eu/Fe]}$, since the Ba/Eu r-process ratio is fixed at the solar r-process-only ratio and Eu is produced practically entirely by the r-process. Previous studies indicate that the main s-process does not become important until ${\rm [Fe/H]} \ga -2.5$, e.g. Burris et al. and Truran et al. (2002). Thus we assume that at lower metallicities all Ba in non-C-rich stars is produced by the r-process. That is, for stars with ${\rm [C/Fe]}<0.3$ and ${\rm [Fe/H]}<-2.5$, ${\rm [Ba/Fe]}_{r-\rm process} = {\rm [Ba/Fe]} + 0.721$. Those stars that are not pure r-process stars with higher C enrichment and higher metallicity are disregarded.

The results for ${\rm [Ba/Fe]}_{r-{\rm process}}$ are plotted against [Fe/H] in Fig. 21. Note, since we can only estimate ${\rm [Ba/Fe]}_{r\rm -process}$ in stars with ${\rm [Fe/H]} > -2.5$ if Eu is detected, there is an observational bias here; we will miss stars with low r-process enhancements at ${\rm [Fe/H]} > -2.5$. The results of Burris et al., which cover this metallicity regime and are much more complete, indicate the scatter in the region $-2.5 <{\rm [Fe/H]}<-1.5$ is larger than seen in our results. They find stars in this regime with ${\rm [Eu/Fe]}$ ranging from as low as $\sim $-0.4 (significantly lower than in our data) to as high as $\sim $0.8 (similar to our data). In any case, even accounting for the fact that this bias leads to an underestimation of the scatter at ${\rm [Fe/H]} > -2.5$, the scatter at ${\rm [Fe/H]}<-2.5$ in our data is significantly larger than seen at higher metallicity in the results of Burris et al. If we consider only the upper envelope of the abundance distribution, which should be well defined by our sample, there is an rapid transition from a maximum value of [Eu/Fe] of $\sim $1.0 to $\sim $1.7 at ${\rm [Fe/H]} \sim -2.5$. Thus, Fig. 21 and the occurrence of r-II stars only at ${\rm [Fe/H]}<-2.5$, suggests the r-II stars are extreme cases of a wide range of r-process enrichment in the early, chemically inhomogeneous Galaxy. Note, the cutoff of ${\rm [Eu/Fe]}=1.0$ between r-I and r-II is suggested by the maximum enrichment levels at higher metallicity.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f21.eps}
\end{figure} Figure 21: A plot of ${\rm [Ba/Fe]}_{r\rm -process}$ vs. [Fe/H]. Symbols have the same meanings as in Fig. 13. For the closed symbols (pure r-process stars) ${\rm [Ba/Fe]}_ {r\rm -process} = {\rm [Eu/Fe]}$. Open circles show stars where ${\rm [C/Fe]}<0.3$ and ${\rm [Fe/H]}<-2.5$, for which we assume ${\rm [Ba/Fe]}_{r \rm -process} = {\rm [Ba/Fe]+0.721}$. Note the scatter is underestimated at ${\rm [Fe/H]} > -2.5$; see text.


  \begin{figure}
\par\includegraphics[width=7.4cm,clip]{2967f22a.eps}\par\vspace*{3mm}
\includegraphics[width=7.1cm,clip]{2967f22b.eps}
\end{figure} Figure 22: A plot of [Sr/Ba] vs. [Fe/H] ( upper panel) and [C/H] ( lower panel). Symbols and lines have the same meanings as in Fig. 13, with circles representing stars where Eu is undetected.


  \begin{figure}
\par\includegraphics[width=7.7cm,clip]{2967f23a.eps}\par\vspace*{3mm}
\includegraphics[width=7.4cm,clip]{2967f23b.eps}
\end{figure} Figure 23: A plot of [Sr/Eu] vs. [Fe/H] ( upper panel) and [C/H] ( lower panel). Symbols and lines have the same meanings as in Fig. 13, with circles representing stars where Ba is undetected. The solar s-process value is 1.08.


  \begin{figure}
\par\includegraphics[width=5.6cm,clip]{2967f24.eps}
\end{figure} Figure 24: A plot of [Sr/Ba] vs. [Ba/Fe]. Symbols and lines have the same meanings as in Fig. 13, with circles representing stars where Eu is undetected.


  \begin{figure}
\par\includegraphics[width=5.9cm,clip]{2967f25.eps}
\end{figure} Figure 25: A plot of [Sr/Eu] vs. [Eu/Fe]. Symbols and lines have the same meanings as in Fig. 23.

   
5.4 Light neutron-capture elements, Sr, Y and Zr

The production of light neutron-capture elements (particularly Sr, Y, Zr) versus heavy neutron-capture elements (such as Ba, Eu), has become a topic of interest due to evidence of production of the former without significant production of the latter, e.g. McWilliam  (1998), Burris et al. (2000), Truran et al. (2002), Travaglio et al. (2004) and Aoki et al. (2005). Figures 22 and 23 plot [Sr/Ba] and [Sr/Eu] against Fe and C abundances. Significant scatter is seen in Sr/Ba at low metallicity, as found by McWilliam and Burris et al. In both cases, Sr/Ba and Sr/Eu, even among the pure r-process stars, a significant amount of scatter is seen at ${\rm [Fe/H]}<-2.5$. For Sr/Ba, the scatter appears to increase quite uniformly with decreasing [Fe/H], the data showing quite clear upper and lower boundaries, apart from a small number of outliers which are usually C enhanced. Sr/Eu shows similar tendencies when the s-process rich stars are disregarded, though not as clearly due to the smaller number of stars. The r-II stars all have similar Sr/Ba and Sr/Eu ratios, which are always among lowest of the non-C-enhanced stars. For Sr/Ba the weighted mean of the results for r-II stars, is $\langle {\rm [Sr/Ba]} \rangle_{\rm r-II} = -0.44 \pm 0.08$, and for Sr/Eu $\langle {\rm [Sr/Eu]} \rangle_{\rm r-II} = -0.98 \pm 0.09$. The solar system r-process values are -0.24 and -0.89 respectively.

Truran et al. (2002) examined the variation of Sr/Ba with r-process enrichment, as traced by Ba/Fe and Eu/Fe. Figure 24 shows Sr/Ba with Ba/Fe, and Fig. 25 shows Sr/Eu with Eu/Fe. We find similar results; however, with our large and homogeneously analysed sample the scatter is well defined, and we see a trend for decreasing scatter in Sr/Ba and Sr/Eu with increasing r-process enrichment.

Similar plots are shown for Y/Ba in Figs. 26 and 27. The results are similar to those for Sr/Ba, in particular, increasing scatter in Y/Ba with decreasing metallicity and decreasing heavy r-process enrichment, and similar Y/Ba among the r-II stars. For the r-II stars we find $\langle {\rm [Y/Ba]} \rangle_{\rm r-II} = -0.47 \pm 0.08$; the solar system r-process value is ${\rm [Y/Ba]} = -0.48$.


  \begin{figure}
\par\includegraphics[width=7.5cm,clip]{2967f26a.eps}\par\vspace*{3mm}
\includegraphics[width=7.2cm,clip]{2967f26b.eps}
\end{figure} Figure 26: A plot of [Y/Ba] vs. [Fe/H] ( upper panel) and [C/H] ( lower panel). Symbols and lines have the same meanings as in Fig. 13, with circles representing stars where Eu is undetected.


  \begin{figure}
\par\includegraphics[width=5.6cm,clip]{2967f27.eps}
\end{figure} Figure 27: A plot of [Y/Ba] vs. [Ba/Fe]. Symbols and lines have the same meanings as in Fig. 26.

Figures 222426 and 27 identify two stars of interest, two metal-poor stars with ${\rm [Sr,Y/Ba]} \la -1$ which are not carbon-rich or overly Ba-rich, which are HE 0305-4520 ( ${\rm [C/Fe]}\sim +0.3$, ${\rm [Sr/Fe]}\sim -0.7$, ${\rm [Y/Fe]}\sim -0.4$, ${\rm [Ba/Fe]}\sim +0.6$) and HE 2156-3130 ( ${\rm [C/Fe]}\sim +0.7$, ${\rm [Sr/Fe]}\sim -0.9$, ${\rm [Y/Fe]}\sim -0.9$, ${\rm [Ba/Fe]}\sim +0.5$ ), the latter being the more metal-poor of the two. These stars perhaps warrant further study.

We note that Figs. 22 and 24 show 6 stars with similar Sr/Ba ratios and similar C/H and Fe/H to the stars identified as s-process-rich stars. These stars also stand out clearly in a plot of [Ba/Fe] vs. [C/Fe], see Fig. 28, occupying a similar region of the plot as the s-process-rich stars. As Eu has not been detected at the 3 sigma level according to our criteria they have not been classified in terms of the likely neutron-capture processes that have contributed to the heavy elements. It is interesting to look at these stars in more detail. We find that all these stars appear to be s-process-rich stars based on Eu abundances obtained, though we emphasise the abundances are not 3 sigma detections and thus not completely reliable. HE 1430-1123, the star with the lowest [Sr/Ba] of the six, and thus more closely associated with the s-II stars in Fig. 22, appears also to be a s-II star as we determine ${\rm [Eu/Fe]}\sim 1.4$. The other five stars, HE 0231-4016, HE 0430-4404, HE 2150-0825, HE 2227-4044, and HE 2240-0412, which seem more closely associated with the remaining mildly Eu enhanced s-process-rich stars in Fig. 22, appear to be similar stars with ${\rm [Eu/Fe]}\sim 0.7\leftrightarrow 1.0$.


  \begin{figure}
\par\includegraphics[width=5.6cm,clip]{2967f28.eps}
\end{figure} Figure 28: A plot of [Ba/Fe] vs. [C/Fe]. Symbols have the same meanings as in Fig. 22.

Figure 28 also identifies a number of mildly carbon-enhanced stars without enhancement of neutron-capture elements, a class of objects identified by Aoki et al. (2002a). The five objects with ${\rm [C/Fe]}>0.8$ and ${\rm [Ba/Fe]}<0.2$ are, from largest [C/Fe] to smallest, HE 1351-1049, HE 1300-0641, HE 1330-0354, HE 1300-2201, and HE 1124-2335.

   
6 Conclusions

We have analysed snapshot spectra of a sample of 253 metal-poor stars, deriving abundances for 22 elements, where detectable, using an automated technique based on SME by Valenti & Piskunov (1996). The technique has been shown to give results in agreement with previous work within errors, when one considers differences in temperature scale. For our particular case (namely resolving power, spectral coverage and line list) the technique has been shown to be quite robust (at around the 0.1 dex level) even for S/N as low as 15. Our error estimates and comparisons with studies in the literature show the derived elemental abundances to be of moderate precision, relative and absolute errors of order 0.15 and 0.25 dex respectively. This work has dealt with the CH weak content of the sample. The CH strong content will also be examined as part of the HERES programme. It would be interesting to obtain additional spectra for (the most interesting of) these stars, particularly covering the Eu II lines at 6437 and 6645 Å.

Our main goal here has been to identify stars of interest, particularly those enhanced in r-process elements. We identified 8 new r-II stars, 35 r-I stars and 3 s-process rich stars with strong Eu enhancement. Notably, the r-II stars were found only in a rather narrow metallicity range, $-3.2\la{\rm [Fe/H]}\la-2.6$. These interesting stars should be investigated in more detail, and such work is underway as part of the HERES project large programme. The spectra obtained will be of much higher quality, in terms of S/N, resolving power, and spectral coverage. The higher quality data, together with a careful manual spectrum analysis, will naturally permit abundances and stellar parameters to be obtained with higher precision and abundances for additional elements to be obtained. It will also be possible to obtain isotopic ratios for some elements. Ideally, such analyses should be performed with reference to deviations from the assumptions of LTE and 1D model atmospheres.

The results presented here provide a database of confirmed metal-poor stars, including a number of new r-process and s-process rich stars, which may be used for selection of stars for further studies. The results also provide a homogeneous database of moderate precision abundances for comparison with Galactic chemical evolution models. We stress that such comparisons must consider the limitations of our data set, most importantly the selection effects arising from the significant incompleteness of the data for some elements, but also the precision of the abundances and the assumptions of the modelling such as LTE and the use of 1D model atmospheres.

We investigated trends and scatter in some measured abundance ratios of interest. Among the stars without strong C enhancement, at about ${\rm [Fe/H]} \ga -2.5$ we find that the cosmic scatter in any abundance ratio is small (perhaps even non-existent), implying that at around this level of enrichment the Galactic halo was reasonably well mixed. At lower metallicities C, Sr, Y, Ba and Eu, and perhaps Zr, show evidence for cosmic scatter, while the results for the Mg, Ca, Sc, Ti, Cr, Fe, Co and Ni still indicate at most small cosmic scatter within the errors of our analysis. Due to the difficulties in accurately estimating errors, and thus disentangling the observational and modelling uncertainties from the real cosmic scatter, we conclude that to determine the magnitude of the scatter in the cases where it is small will require high precision studies of a large number of stars.

Acknowledgements

We are indebted to Jeff Valenti and Nikolai Piskunov for making their code SME available to the community, and to Nikolai for help in understanding it. We are further indebted to the many people who work on the MARCS code for making it available to us. Bertrand Plez and Alain Jorissen are thanked for providing their CH line list, and permitting us to publish the parts employed. Bengt Gustafsson is thanked for helpful comments on early versions of the manuscript, and pointing out the importance of correctly treating scattering. We are grateful to the ESO staff at Paranal and Garching for obtaining the observations and reducing the data respectively. We also thank T. Sivarani for supplying the routine used for the colour transformations and determination of the effective temperatures. This work made extensive use of the VALD database and the NIST Atomic Spectra Database. P.B. acknowledges the support of the Swedish Research Council. N.C. acknowledges financial support through a Henri Chretien International Research Grant administered by the American Astronomical Society, and from Deutsche Forschungsgemeinschaft under grants CH 214/3-1 and Re 353/44-1. T.C.B. acknowledges partial funding for this work from grants AST 00-98508, AST 00-98549 and AST-04 06784 awarded by the U.S. National Science Foundation, and from award PHY 02-16783: Physics Frontiers Center/Joint Institute for Nuclear Astrophysics (JINA). S.R. acknowledges partial financial support from FAPESP and CNPq.

References

 

  
7 Online Material

   
Appendix A: Line list

The lines and spectral windows used are listed in Tables A.1-A.5. The most important atomic and molecular data, wavelength $\lambda $, excitation potential $\chi $, and $\log gf$, are tabulated. Line broadening data used may be obtained from the authors on request. Below we briefly comment on line selection issues and data sources for each element.

First, it is worth commenting on Si which is notably omitted from our analysis. Our spectra include two Si lines, at 3905 and 4102 Å. The $\lambda $4102 line lies in the wing of H$\delta$ and thus presents a considerable challenge for automated analysis. The $\lambda $3905 line is known to be blended by CH lines (e.g. Cayrel et al. 2004). Even with known CH lines from the lists of Plez & Jorrisen (see below) included in the synthesis, our Si abundances were found to differ from the literature values (see Sect. 3.5.2), which are usually based on the $\lambda $4102 line, and the difference was seen to correlate with carbon-enhancement. We have reasonable agreement with the literature for CS 22186-025 which has $\rm [C/Fe]\sim-0.7$, while we have mild disagreement for CS 31082-001 which has $\rm [C/Fe]\sim 0.2$ and strong disagreement for CS 22892-052 which has ${\rm [C/Fe]}\sim 1$. This suggests that the $\lambda $3905 line may be affected by further blends of features involving C, and thus we chose to omit Si from our analysis.

Carbon
Abundances are derived from selected clean regions of CH A-X bands at 4310-4313 Å (G band) and 4362-4367 Å. We limited ourselves to these regions to reduce computing times due to the large number of components in these bands. Comparisons with results using larger regions showed no differences to those using the final adopted regions. We note, however, that we consider it important to use at least two different regions of differing strengths, in particular because the G band region at 4310 Å can become saturated in carbon-enhanced stars. The observations are not of sufficient quality to determine isotopic abundances, and so we made the assumption that all carbon is in the form of 12C and there is no 13C. The adopted line list given in Tables A.1 and A.2 was extracted from a list compiled by Plez & Jorissen (private communication), which is described by Hill et al. (2002).

Magnesium
We employed 7 spectral features of Mg I. The features consist of the generally strong UV triplet near 3835 Å from the 3P $^{\rm o}-^3$D transition, plus some weaker yet cleaner features farther to the red, the strongest of which is generally $\lambda $4703. Our employed lines are practically the same as those adopted by McWilliam et al. (1995b) and Norris et al. (1996) (see also Ryan et al. 1996), though we note that there are some significant differences in the adopted $\log gf$ values, particularly for the triplet where the two works adopt values which differ by as much as 0.5 dex. This warrants some discussion. McWilliam et al. adopted $\log gf$ values for the triplet from the NIST compilation of Wiese et al. (1969), which are based on theoretical calculations of Weiss (1967) and re-normalised measurements by Penkin & Shabanova (1962); the compilation can be consulted for details. We note that the 3P $^{\rm o}-^3$D transition is actually a sextuplet, but due to the practically non-existent fine-structure splitting of the 3D level only 3 lines are observed. Wiese et al. (1969) present $\log gf$ values for each of the 6 components, but McWilliam et al. seem only to have included the strongest component for each line. We have also adopted the NIST data, but have added together the appropriate components. Thus, two of the lines have $\log gf$ values of order 0.1 dex stronger than those used by McWilliam et al (1995b). Norris et al. seem not to have been aware of the NIST data, and adopted what amounts to empirical f-values guided by the desire to obtain abundances from these lines consistent with those from the other lines, particularly the $\lambda $4703 line, where the theoretical calculations of Froese Fischer (1975) are employed (which we also adopt for these lines). Their adopted values for the triplet differ from our adopted values by as much as 0.6 dex. Thus, we would expect to find largely discrepant results from the triplet and the remaining lines with our f-values. However, in our sample we always found a good general global fit with a single abundance. We suspect this apparent discrepancy is due to the fact that we use a profile fitting technique with the line cores removed, while Norris et al. fit equivalent widths. The triplet lines are quite strong, having equivalent widths often of order 100 mÅ even for stars with ${\rm [Fe/H]}<-3$, and our fits to the triplet show the observed cores to be typically much deeper than those from the best fit to the wings. This is a well known problem of LTE analyses with no modelling of chromospheres. This effect goes in the correct direction, in the sense that Norris et al. would need to underestimate the f-values in order to correct for the overestimation of abundance due to the influence of the line cores. We note that, since the Norris et al. f-values for the triplet are calibrated to the weaker line abundances, their final abundances should be correct.

Aluminium
Only one line of Al I was employed, the resonance line $\lambda $3961. The second resonance line $\lambda $3944 was too blended to be considered reliable. Hyperfine structure was adopted from McWilliam et al. (1995b).

Calcium
The Ca abundance is determined from 9 lines of Ca I. The f-values are adopted from the NIST critical compilations.

Scandium
The f-values are taken from Lawler & Dakin (1989). Hyperfine structure is taken directly from McWilliam et al. (1995b).

Titanium
Oscillator strengths for neutral lines are adopted from Blackwell et al. (1982a,1982b). For singly ionised lines, the situation has been markedly improved by the experimental work of Pickering et al. (2001), and their oscillator strengths have been adopted. For two useful lines where data were not available from this source, we adopted the solar values from Ryabchikova et al. (1994). We note that for the other Ti II lines we used these two sources agreed within 0.1 dex.

Vanadium
The $\log gf$ data for V I is taken from Doerr et al. (1985), and for V II from Biémont et al. (1989a). McWilliam et al. (1995b) noted the lack of hyperfine structure data for the transitions used here, and to our knowledge this situation has not changed. However, as noted by McWilliam et al. these lines are weak and unsaturated and therefore our abundances should not be greatly affected by this omission. We note that in the case there was some effect, our abundances would be an upper limit.

Chromium
The f-values are taken from the NIST compilation (Martin et al. 1988). The values are based on a critical averaging of number of sources, which are detailed in the compilation.

Manganese
We adopted oscillator strengths from Booth et al. (1984). The hyperfine structure was computed using the data compiled in Lefèbvre et al. (2003), which for the lines employed here draws on data from Davis et al. (1971), and Handrich et al. (1969), as well as their own measurements.

Iron
A total of 55 lines were used of which 45 were Fe I lines and 10 Fe II. For the neutral lines the oscillator strengths of O'Brian et al. (1991) were adopted. Oscillator strengths for the Fe II lines were adopted from Schnabel et al. (2004) where possible. Data for some other useful lines were taken from Biémont et al. (1991) and Moity (1983). We note that the Fe II line f-values are of lower precision, typically 20%, than the Fe I lines, typically 7%.

Cobalt
Oscillator strengths for the employed lines were taken from Nitz et al. (1999) where possible, otherwise from Cardon et al. (1982). Hyperfine structure was included using the data of Pickering (1996).

Nickel
Four lines of Ni I are employed. For 3 lines we employed the oscillator strengths from Blackwell et al. (1989); for the remaining line we used the f-value from Huber & Sandeman (1980).

Zinc
Two neutral lines were employed and the f-values taken from Biémont & Godefroid (1980).

Strontium
One line of Sr I and two of Sr II were analysed. Hyperfine and isotopic splitting was accounted for in the $\lambda $4215 line, using the data from Borghs et al. (1983), where solar isotopic ratios have been assumed. There are unfortunately no data to our knowledge for the upper state of the other resonance line $\lambda $4077. However, noting that the splitting in the $\lambda $4215 line is dominated by the common lower level 2S1/2, we computed hyperfine splitting for the $\lambda $4077 line where we neglected the splitting of the upper level. The main isotope shifts for the $\lambda $4215 line are interpreted as due to the volume effect which affects the s state most strongly (e.g. Cowan 1981; pg 506). We therefore adopted the same isotopic shifts for $\lambda $4077 as for the $\lambda $4215 line. We did not find hyperfine structure data for the remaining line. However, as it is weak, this should not be important.

Yttrium
The f-values for the employed lines of Y II are from Hannaford et al. (1982). 89Y has a small nuclear spin of I=1/2, and thus hyperfine splitting is negligible.

Zirconium
Three lines of Zr II are analysed employing the f-values from Biémont et al. (1981).

Barium
Our analysis of Ba is based on 2 lines of Ba II, with oscillator strengths from Gallagher (1967) which for common lines are in excellent agreement with Davidson et al. (1992). Hyperfine structure was included from McWilliam (1998), assuming the pure r-process isotopic composition from that paper. As pointed out by McWilliam (1998), if a star would have a significant s-process contribution, then our derived Ba abundance would be a lower limit. This is because the s-process causes a higher fraction of the Ba to be in even isotopes which have no hyperfine splitting, and thus the stronger lines saturate more quickly, meaning the same line strength would require a higher abundance.

Lanthanum
The oscillator strengths of Lawler et al. (2001a) are used. Hyperfine structure is included using the constants from Lawler et al., which for our lines draws from their own measurements and those of Höhle et al. (1982).

Cerium
We employed 10 lines of Ce II, the same as those employed by Sneden et al. (1996), with the addition of the line $\lambda $3999. We adopted the same oscillator strengths as used by Sneden et al (1996). For $\lambda $3999 we adopted the VALD value, which is essentially a solar value averaged from various sources (see Piskunov et al. 1995).

Neodymium
We employ 9 lines of Nd II using laboratory f-values from Den Hartog et al. (2003), which are a significant improvement on those previously available.

Samarium
Eight lines of Sm II are employed and the f-values from Biemont et al. (1989b) were used.

Europium
Our Eu abundances are based on 4 lines of Eu II. Lines at 4435 and 4522 Å were found to be too strongly blended in non-r-process-enhanced stars to be employed. The line $\lambda $3971 was considered too blended for automated analysis. Oscillator strengths and hyperfine splitting from Lawler et al. (2001b) were employed, assuming solar r-process isotopic fractions (supported by measurements by Sneden et al. 2002).


 

 
Table A.1: Molecular line data for A-X system of the CH molecule near 4310 Å from Plez & Jorissen. The spectral windows employed for this molecular band are defined with respect to an arbitrary $\lambda $ and span from $\lambda +d\lambda _{\rm blue}$ to $\lambda +d\lambda _{\rm red}$.
Species $\lambda $ $\chi $ $\log gf$ d $\lambda_{\rm blue}$ d $\lambda_{\rm red}$
  [Å] [eV]   [mÅ] [mÅ]
CH 4310.150     -100 2300
CH 4310.038 0.096 -3.183    
CH 4310.090 0.096 -1.412    
CH 4310.110 0.096 -1.474    
CH 4310.149 0.431 -3.202    
CH 4310.162 0.096 -3.025    
CH 4310.203 0.431 -1.443    
CH 4310.220 0.431 -1.505    
CH 4310.272 0.431 -3.039    
CH 4310.404 0.096 -3.183    
CH 4310.430 0.408 -1.581    
CH 4310.458 0.096 -1.412    
CH 4310.504 0.432 -3.202    
CH 4310.508 0.408 -2.966    
CH 4310.556 0.432 -1.443    
CH 4310.679 0.072 -1.550    
CH 4310.729 0.408 -1.581    
CH 4310.757 0.072 -2.952    
CH 4310.807 0.408 -2.966    
CH 4310.811 0.408 -3.155    
CH 4310.889 0.408 -1.508    
CH 4310.937 0.388 -1.677    
CH 4310.969 1.107 -2.269    
CH 4310.991 0.072 -1.550    
CH 4311.045 0.388 -2.879    
CH 4311.069 0.072 -2.952    
CH 4311.075 0.408 -3.155    
CH 4311.075 0.072 -3.136    
CH 4311.084 0.987 -4.123    
CH 4311.145 0.987 -4.123    
CH 4311.153 0.408 -1.508    
CH 4311.153 0.388 -1.677    
CH 4311.153 0.072 -1.477    
CH 4311.196 1.108 -3.922    
CH 4311.196 1.108 -2.229    
CH 4311.261 0.388 -2.879    
CH 4311.328 0.371 -1.805    
CH 4311.348 0.072 -3.136    
CH 4311.394 0.388 -3.105    
CH 4311.426 0.072 -1.477    
CH 4311.473 0.371 -1.805    
CH 4311.476 0.371 -2.771    
CH 4311.502 0.388 -1.587    
CH 4311.502 0.051 -1.646    
CH 4311.545 1.108 -2.269    
CH 4311.547 0.347 -2.386    
CH 4311.567 0.357 -2.002    
CH 4311.580 0.388 -3.105    
CH 4311.592 0.347 -2.386    
CH 4311.612 0.051 -2.865    
CH 4311.618 0.662 -2.054    
CH 4311.618 0.662 -2.054    
CH 4311.621 0.371 -2.771    
CH 4311.655 0.357 -2.002    
CH 4311.688 0.388 -1.587    
CH 4311.722 1.108 -3.923    
CH 4311.727 0.051 -1.646    
CH 4311.729 1.108 -2.229    
CH 4311.776 0.357 -2.632    
CH 4311.837 0.051 -2.866    
CH 4311.861 0.347 -2.432    
CH 4311.863 0.357 -2.632    
CH 4311.897 0.371 -3.052    
CH 4311.906 0.347 -2.432    
CH 4311.978 0.051 -3.085    
CH 4312.017 0.371 -3.052    
CH 4312.045 0.371 -1.688    
CH 4312.088 0.051 -1.557    
CH 4312.153 0.033 -1.773    
CH 4312.164 0.371 -1.688    
CH 4312.172 0.051 -3.085    
CH 4312.280 0.051 -1.557    
CH 4312.304 0.033 -1.773    
CH 4312.304 0.033 -2.759    
CH 4312.317 0.358 -3.007    
CH 4312.386 0.358 -3.007    
CH 4312.456 0.033 -2.759    
CH 4312.527 0.358 -1.831    
CH 4312.594 0.358 -1.831    
CH 4312.594 0.019 -1.969    
CH 4313.620     -200 200
CH 4313.377 0.020 -2.985    
CH 4313.446 0.020 -2.985    
CH 4313.590 0.020 -1.800    
CH 4313.660 0.020 -1.800    
CH 4313.876 0.009 -3.033    
CH 4313.906 0.009 -3.033    



 

 
Table A.2: Molecular line data for A-X system of the CH molecule near 4363 Å from Plez & Jorissen. The spectral window employed for this molecular band is defined with respect to two arbitrary wavelengths $\lambda $ and span from $\lambda +d\lambda _{\rm blue}$ to $\lambda +d\lambda _{\rm red}$.
Species $\lambda $ $\chi $ $\log gf$ d $\lambda_{\rm blue}$ d $\lambda_{\rm red}$
  [Å] [eV]   [mÅ] [mÅ]
CH 4363.300     -1000 3700
CH 4362.021 1.247 -4.054    
CH 4362.061 1.247 -1.976    
CH 4362.172 1.247 -1.943    
CH 4362.202 0.777 -1.982    
CH 4362.204 1.247 -4.149    
CH 4362.255 0.777 -3.284    
CH 4362.531 0.777 -1.917    
CH 4362.549 0.557 -1.749    
CH 4362.551 0.557 -3.392    
CH 4362.697 0.777 -1.982    
CH 4362.749 0.557 -1.705    
CH 4362.750 0.777 -3.285    
CH 4362.985 0.777 -1.917    
CH 4363.086 0.227 -3.380    
CH 4363.087 0.227 -1.716    
CH 4363.162 1.248 -4.055    
CH 4363.186 1.248 -1.976    
CH 4363.242 1.248 -1.943    
CH 4363.276 1.248 -4.149    
CH 4363.291 0.227 -1.673    
CH 4363.461 0.558 -1.749    
CH 4363.463 0.558 -3.392    
CH 4363.605 0.558 -1.705    
CH 4364.034 0.228 -3.380    
CH 4364.036 0.228 -1.716    
CH 4364.114 1.289 -4.093    
CH 4364.167 1.289 -1.947    
CH 4364.181 0.228 -1.673    
CH 4364.253 1.289 -1.916    
CH 4364.295 1.289 -4.181    
CH 4365.416 1.290 -4.093    
CH 4365.450 1.290 -1.947    
CH 4365.477 1.290 -1.916    
CH 4365.522 1.290 -4.181    
CH 4365.929 0.987 -3.729    
CH 4366.010 0.987 -3.729    
CH 4366.230 0.987 -3.828    
CH 4366.312 0.987 -3.828    
CH 4366.398 0.597 -3.426    
CH 4366.407 0.597 -1.699    
CH 4366.482 0.268 -3.414    
CH 4366.497 0.268 -1.666    
CH 4366.520 1.333 -4.129    
CH 4366.573 0.597 -1.659    
CH 4366.588 1.333 -1.920    
CH 4366.647 1.333 -1.892    
CH 4366.663 0.268 -1.627    
CH 4366.699 1.333 -4.211    
CH 4366.897 0.805 -1.903    
CH 4366.928 0.987 -3.495    
CH 4366.930 0.805 -3.326    
CH 4366.991 0.987 -3.495    
CH 4367.172 0.805 -1.848    



   
Table A.3: Data for atomic lines for species lighter than Fe. The spectral window employed for the line is from $\lambda +{\rm d}\lambda _{\rm blue}$ to $\lambda +{\rm d}\lambda _{\rm red}$. Lines which are removed in carbon-enhanced stars are marked with asterisks in the wavelength column.
Species $\lambda $ $\chi $ $\log gf$ d $\lambda_{\rm blue}$ d $\lambda_{\rm red}$ Refs.
  [Å] [eV]   [mÅ] [mÅ]  
Mg I 3829.355 2.707 -0.208 -150 100 WSM69
Mg I 3832.304 2.710 0.270 -300 200 WSM69
Mg I 3838.292 2.715 0.490 -230 150 WSM69
Mg I *4057.505 4.346 -0.890 -120 100 FF75
Mg I *4167.271 4.346 -0.710 -250 200 FF75
Mg I 4571.096 0.000 -5.393 -300 300 WSM69
Mg I 4702.990 4.330 -0.380 -300 300 FF75
Al I 3961.529 0.014 -0.336 -200 170 WM80
Ca I 4226.728 0.000 0.244 -150 400 WM80
Ca I *4283.011 1.886 -0.224 -120 300 WM80
Ca I *4289.367 1.879 -0.304 -120 170 WM80
Ca I 4318.652 1.890 -0.207 -120 120 WM80
Ca I *4425.437 1.879 -0.358 -300 300 WM80
Ca I *4434.957 1.886 -0.005 -300 50 WM80
Ca I 4454.780 1.898 0.258 -50 200 WM80
Ca I 4455.887 1.899 -0.526 -300 300 WM80
Ca I 4578.551 2.521 -0.558 -200 100 WM80
Sc II 4246.837 0.315 0.240 -350 250 LD89
Sc II *4314.095 0.618 -0.100 -250 70 LD89
Sc II *4400.399 0.605 -0.540 -150 200 LD89
Sc II 4415.563 0.595 -0.670 -180 300 LD89
Sc II 4670.417 1.357 -0.580 -150 50 LD89
Ti I 3989.759 0.021 -0.140 -200 100 GBP89, BPSL82
Ti I 3998.636 0.048 0.000 -250 150 GBP89, BPSL82
Ti I 4533.249 0.848 0.530 -150 300 GBP89, BMPS82
Ti I 4534.776 0.836 0.340 -300 300 GBP89, BMPS82
Ti I 4656.469 0.000 -1.290 -300 300 GBP89, BPSL82
Ti I *4681.909 0.048 -1.020 -300 150 GBP89, BPSL82
Ti II *4337.915 1.080 -0.960 -150 150 PTP01
Ti II *4394.051 1.221 -1.780 -100 300 PTP01
Ti II *4395.850 1.243 -1.930 -200 100 PTP01
Ti II *4417.719 1.165 -1.190 -200 300 PTP01
Ti II 4443.794 1.080 -0.720 -300 250 PTP01
Ti II 4468.507 1.131 -0.600 -150 300 RHLPS94
Ti II *4470.857 1.165 -2.020 -250 150 PTP01
Ti II 4501.273 1.116 -0.770 -300 300 PTP01
Ti II 4563.761 1.221 -0.690 -300 300 PTP01
Ti II 4571.968 1.572 -0.320 -300 150 PTP01
Ti II 4589.958 1.237 -1.620 -300 300 RHLPS94
V I *4379.230 0.301 0.550 -150 150 DKKWZ85
V I *4389.976 0.275 0.270 -150 150 DKKWZ85
V II *3951.960 1.480 -0.784 -150 60 BGFML89
Cr I 4254.332 0.000 -0.114 -150 200 see MFW88
Cr I *4274.796 0.000 -0.231 -200 100 see MFW88
Cr I *4289.716 0.000 -0.361 -150 100 see MFW88
Mn I 4030.763 0.000 -0.470 -150 250 BBPS84
Mn I 4033.060 0.000 -0.618 -200 150 BBPS84
Mn I *4034.492 0.000 -0.811 -150 300 BBPS84
Mn I 4754.040 2.282 -0.086 -200 200 BBPS84
Mn I 4823.496 2.319 0.144 -100 200 BBPS84
References: BBPS84 = Booth et al. (1984), BGFML89 = Biémont et al. (1989a), BMPS82 = Blackwell et al. (1982a), BPSL82 = Blackwell et al. (1982b), DKKWZ85 = Doerr et al. (1985), FF75 = Froese Fischer (1975), GBP89 = Grevesse et al. (1989), LD89 = Lawler & Dakin (1989), MFW88 = Martin, Fuhr & Wiese (1988), PTP01 = Pickering et al. (2001), RHLPS94 = Ryabchikova et al. (1994), WM80 = Wiese & Martin (1980), WSM = Wiese et al. (1969).


 

 
Table A.4: Data for atomic lines of Fe. The spectral window employed for the line is from $\lambda +{\rm d}\lambda _{\rm blue}$ to $\lambda +{\rm d}\lambda _{\rm red}$. Lines which are removed in carbon-enhanced stars are marked with asterisks in the wavelength column.
Species $\lambda $ $\chi $ $\log gf$ d $\lambda_{\rm blue}$ d $\lambda_{\rm red}$ Refs.
  [Å] [eV]   [mÅ] [mÅ]  
Fe I *3856.372 0.052 -1.286 -200 400 OWLWB91
Fe I *3859.911 0.000 -0.710 -400 350 OWLWB91
Fe I 3865.523 1.011 -0.950 -250 250 OWLWB91
Fe I *3878.018 0.958 -0.896 -300 100 OWLWB91
Fe I 4005.242 1.557 -0.583 -150 150 OWLWB91
Fe I 4045.812 1.485 0.284 -100 150 OWLWB91
Fe I 4063.594 1.558 0.062 -100 300 OWLWB91
Fe I 4071.738 1.608 -0.008 -100 300 OWLWB91
Fe I 4114.445 2.831 -1.303 -250 250 OWLWB91
Fe I 4132.058 1.608 -0.675 -300 100 OWLWB91
Fe I 4143.868 1.557 -0.511 -200 300 OWLWB91
Fe I *4175.636 2.845 -0.827 -150 300 OWLWB91
Fe I *4187.039 2.449 -0.514 -150 200 OWLWB91
Fe I *4199.095 3.047 0.156 -200 300 OWLWB91
Fe I 4202.029 1.485 -0.689 -200 150 OWLWB91
Fe I 4222.213 2.449 -0.914 -300 200 OWLWB91
Fe I 4227.426 3.332 0.266 -150 150 OWLWB91
Fe I *4233.603 2.482 -0.579 -150 100 OWLWB91
Fe I *4250.120 2.469 -0.380 -100 300 OWLWB91
Fe I 4250.787 1.557 -0.713 -300 300 OWLWB91
Fe I 4260.474 2.400 0.077 -150 200 OWLWB91
Fe I *4271.154 2.449 -0.337 -300 100 OWLWB91
Fe I *4271.761 1.485 -0.173 -150 300 OWLWB91
Fe I 4282.403 2.176 -0.779 -250 150 OWLWB91
Fe I *4325.762 1.608 0.006 -250 100 OWLWB91
Fe I *4375.930 0.000 -3.031 -150 300 OWLWB91
Fe I *4383.545 1.485 0.208 -300 300 OWLWB91
Fe I *4404.750 1.557 -0.147 -250 200 OWLWB91
Fe I *4415.123 1.608 -0.621 -300 200 OWLWB91
Fe I *4430.614 2.223 -1.728 -250 250 OWLWB91
Fe I *4442.339 2.198 -1.228 -300 300 OWLWB91
Fe I 4443.194 2.858 -1.043 -100 250 OWLWB91
Fe I 4447.717 2.223 -1.339 -300 300 OWLWB91
Fe I 4489.739 0.121 -3.899 -300 200 OWLWB91
Fe I 4494.563 2.198 -1.143 -300 300 OWLWB91
Fe I 4528.614 2.176 -0.887 -100 300 OWLWB91
Fe I 4602.941 1.485 -2.208 -300 300 OWLWB91
Fe I *4736.773 3.211 -0.752 -200 200 OWLWB91
Fe I 4872.137 2.882 -0.567 -300 300 OWLWB91
Fe I 4890.755 2.876 -0.394 -350 350 OWLWB91
Fe I 4891.492 2.852 -0.112 -300 300 OWLWB91
Fe I 4918.994 2.845 -0.342 -350 350 OWLWB91
Fe I 4920.503 2.832 0.068 -400 100 OWLWB91
Fe I 4938.814 2.875 -1.077 -300 200 OWLWB91
Fe I 4939.687 0.859 -3.252 -250 300 OWLWB91
Fe II *4178.862 2.583 -2.443 -100 200 SSK04
Fe II 4233.172 2.583 -1.809 -150 200 SSK04
Fe II 4416.828 2.778 -2.540 -240 300 M83
Fe II 4508.289 2.856 -2.318 -300 300 BBKAP91
Fe II 4515.343 2.844 -2.362 -100 300 SSK04
Fe II 4520.224 2.807 -2.550 -200 300 M83
Fe II *4541.524 2.856 -2.990 -100 200 M83
Fe II *4555.893 2.828 -2.250 -150 100 SSK04
Fe II 4583.839 2.807 -1.740 -250 300 SSK04
Fe II 4923.927 2.891 -1.206 -400 400 SSK04
References: BBKAP91 = Biémont et al. (1991), M83 = Moity (1983),
OWLWB91 = O'Brian et al. 1991, SSK04 = Schnabel et al. (2004).



   
Table A.5: Data for atomic lines of species heavier than Fe. The spectral window employed for the line is from $\lambda +{\rm d}\lambda _{\rm blue}$ to $\lambda +{\rm d}\lambda _{\rm red}$. Lines which are removed in carbon-enhanced stars are marked with asterisks in the wavelength column.
Species $\lambda $ $\chi $ $\log gf$ d $\lambda_{\rm blue}$ d $\lambda_{\rm red}$ Refs.
  [Å] [eV]   [mÅ] [mÅ]  
Co I *3842.046 0.923 -0.770 -200 100 CSSTW82
Co I *3845.461 0.923 0.010 -150 150 CSSTW82
Co I 3894.073 1.049 0.090 -50 200 NKWL99
Co I 3995.302 0.922 -0.140 -250 250 NKWL99
Co I 4118.767 1.049 -0.470 -100 200 NKWL99
Co I 4121.311 0.922 -0.300 -250 250 NKWL99
Ni I 3775.565 0.423 -1.408 -200 200 BBPL89
Ni I 3783.524 0.423 -1.304 -70 300 HS80
Ni I 3807.138 0.423 -1.220 -200 150 BBPL89
Ni I 3858.292 0.423 -0.951 -300 100 BBPL89
Zn I *4722.163 4.030 -0.390 -300 300 BG80
Zn I 4810.537 4.078 -0.170 -300 300 BG80
Sr I *4607.327 0.000 0.283 -300 100 MB87
Sr II 4077.709 0.000 0.158 -150 100 PBL95
Sr II 4215.519 0.000 -0.155 -300 200 PBL95
Y II 3774.331 0.130 0.210 -250 150 HLGBW82
Y II *3788.694 0.104 -0.070 -150 300 HLGBW82
Y II 3818.314 0.130 -0.980 -300 150 HLGBW82
Y II 3950.352 0.104 -0.490 -200 300 HLGBW82
Y II *4398.013 0.130 -1.000 -250 150 HLGBW82
Y II 4883.684 1.084 0.070 -200 200 HLGBW82
Zr II *4161.213 0.713 -0.720 -300 130 BGHL81
Zr II 4208.985 0.713 -0.460 -200 200 BGHL81
Zr II 4317.299 0.713 -1.380 -300 300 BGHL81
Ba II 4130.645 2.722 0.560 -150 300 G67
Ba II 4554.000 0.000 0.163 -500 220 G67
La II *3988.515 0.403 0.210 -300 300 LBS01
La II 3995.745 0.173 -0.060 -250 150 LBS01
La II 4086.709 0.000 -0.070 -200 200 LBS01
La II 4123.218 0.321 0.130 -300 180 LBS01
La II *4322.503 0.173 -0.930 -300 150 LBS01
La II *4333.753 0.173 -0.060 -300 100 LBS01
Ce II 3999.237 0.295 0.232 -100 300 VALD95
Ce II 4073.474 0.478 0.320 -150 150 SMPCBA96
Ce II *4083.222 0.701 0.240 -150 200 SMPCBA96
Ce II 4120.827 0.320 -0.240 -300 300 SMPCBA96
Ce II *4127.364 0.684 0.240 -300 70 SMPCBA96
Ce II 4222.597 0.122 -0.180 -150 150 GS94
Ce II *4418.780 0.864 0.310 -200 150 SMPCBA96
Ce II 4486.909 0.295 -0.360 -300 300 GS94
Ce II 4562.359 0.478 0.330 -300 300 GS94
Ce II 4628.161 0.516 0.260 -300 300 GS94
Nd II *4018.823 0.064 -0.850 -300 120 DLSC03
Nd II 4021.327 0.321 -0.100 -200 200 DLSC03
Nd II 4061.085 0.471 0.550 -300 300 DLSC03
Nd II 4069.265 0.064 -0.570 -200 300 DLSC03
Nd II *4109.448 0.321 0.350 -150 150 DLSC03
Nd II 4232.374 0.064 -0.470 -200 200 DLSC03
Nd II *4358.161 0.321 -0.160 -200 150 DLSC03
Nd II 4446.384 0.205 -0.350 -300 300 DLSC03
Nd II *4462.979 0.559 0.040 -300 300 DLSC03
Sm II 3896.972 0.041 -0.578 -100 200 BGHL89
Sm II 4068.324 0.434 -0.710 -150 150 BGHL89
Sm II *4318.936 0.277 -0.270 -150 150 BGHL89
Sm II 4499.475 0.248 -1.010 -200 200 BGHL89
Sm II 4519.630 0.544 -0.432 -300 300 BGHL89
Sm II 4537.954 0.485 -0.230 -300 300 BGHL89
Sm II 4577.688 0.248 -0.775 -300 300 BGHL89
Sm II *4642.232 0.378 -0.520 -150 150 BGHL89
Eu II 3819.670 0.000 0.510 -150 300 LWDS01
Eu II 3907.110 0.207 0.170 -150 200 LWDS01
Eu II 4129.720 0.000 0.220 -150 400 LWDS01
Eu II *4205.040 0.000 0.210 -50 200 LWDS01
References: BBPL89 = Blackwell et al. (1989), BG80 = Biemont & Godefroid (1980), BGHL81 = Biémont et al. (1981), CSSTW82 = Cardon et al. (1982), DLSC03 = Den Hartog et al. (2003), G67 = Gallagher (1967), GS94 = Gratton & Sneden (1994), HLGBW82 = Hannaford et al. (1982), HS80 = Huber & Sandeman (1980), LBS01 = Lawler et al. (2001a), LWDS01 = Lawler et al. (2001b), MB87 = Migdalek & Baylis (1987), NKWL99 = Nitz et al. (1999), PBL95 = Pinnington et al. (1995), VALD95 = see Piskunov et al. (1995).

   
Appendix B: Error estimates

Our method for estimating error propagation is similar to the approach devised by McWilliam et al. (1995b), but modified to suit our abundance analysis method. The important difference is that our approach fits the spectral features of a given element globally rather than fitting individual lines. Further, as discussed in Sect. 3.4, we will make a distinction between absolute (the uncertainty in the absolute abundance) and relative (the uncertainty in the relative abundance between stars) error estimates. First, we develop the formalism quite generally, and later specify the difference between the calculations for these two types of errors.

We consider the propagation of errors in model atmosphere parameters $T_{\rm eff}$, $\log g$, $\xi $. For low metallicity models of the type used here, typical errors in metallicity have negligible effect on the model structure and can be neglected. Errors due to propagation of uncertainties in $\log gf$, observational error, continuum placement and spectrum modelling uncertainties are also considered. For compactness, in the following discussion we define the abundance parameter $\varepsilon\equiv\log\epsilon$. Assuming the behaviour of the considered abundance with small changes in these parameters can be approximated by a first-order Taylor expansion, i.e. that the abundance $\varepsilon\equiv\log\epsilon$ varies approximately linearly with changes in parameters on scales of the parameter uncertainties, we obtain (e.g. McWilliam et al. 1995b; Taylor 1982) for the variance in the abundance

                                      $\displaystyle \sigma_{\varepsilon}^2$ = $\displaystyle \left(\frac{\partial\varepsilon}{\partial T}\right)^2 \sigma_T^2
...
...g g}^2
+ \left(\frac{\partial\varepsilon}{\partial \xi}\right)^2 \sigma_{\xi}^2$  
    $\displaystyle + \sigma_{\log gf}^2 + \sigma_{\varepsilon}^2({\rm obs}) + \sigma_{\varepsilon}^2 ({\rm cont}) + \sigma_{\varepsilon}^2 ({\rm model})$  
    $\displaystyle + 2 \left\{ \frac{\partial\varepsilon}{\partial T} \frac{\partial...
...on}{\partial T} \frac{\partial\varepsilon}{\partial \xi} \sigma_{T,\xi} \right.$  
    $\displaystyle \left.
+ \frac{\partial\varepsilon}{\partial \log g} \frac{\partial\varepsilon}{\partial \xi} \sigma_{\log g, \xi} \right\} ,$ (B.1)

where $\sigma_i^2$ is the variance in parameter i, and $\sigma_{i,j}$ the covariance of i and j. The variances $\sigma_{\varepsilon}^2({\rm obs})$ and $\sigma_{\varepsilon}^2 ({\rm cont})$ represent the variance in the abundance $\varepsilon$ due to observational error and continuum placement uncertainties respectively. The variance $\sigma_{\varepsilon}^2({\rm model})$ represents the variance in the abundance $\varepsilon$ due to spectrum modelling uncertainties, such as the assumptions of 1D modelling and LTE. Terms involving covariances of independent parameters have been omitted. We have used the fact that $\partial\varepsilon / \partial \log gf = 1$.

We adopt $\sigma_{T,\xi}=0$ and $\sigma_{\log g,\xi}=-0.02$ following McWilliam et al. (1995b). We obtained similar estimates for these quantities from our own numerical experiments for a subsample of stars representative of the complete sample. Based on these experiments we adopted $\sigma_{T,\log g}=+22$. Thus, the expression for the total variance becomes

 
                                        $\displaystyle \sigma_{\varepsilon}^2$ = $\displaystyle \left(\frac{\partial\varepsilon}{\partial T}\right)^2 \sigma_T^2
...
...g g}^2
+ \left(\frac{\partial\varepsilon}{\partial \xi}\right)^2 \sigma_{\xi}^2$  
    $\displaystyle + \sigma_{\log gf}^2 + \sigma_{\varepsilon}^2({\rm obs}) + \sigma_{\varepsilon}^2 ({\rm cont}) + \sigma_{\varepsilon}^2 ({\rm model})$ (B.2)
    $\displaystyle + 2 \left\{ \frac{\partial\varepsilon}{\partial T} \frac{\partial...
...\log g} \frac{\partial\varepsilon}{\partial \xi} \sigma_{\log g,\xi} \right\} .$  

The required partial derivatives are obtained individually for each star and element by direct determination of abundances for shifted stellar parameters (see Sect. 3.3).

Now it simply remains to specify each variance (or standard deviation). The input variances, however, will depend on whether we wish to estimate the absolute error or the relative error.

B.1 Relative error estimates

The relative error estimates are of interest for comparison of abundances within the sample. In particular, we wish to estimate the amount of abundance scatter which should be attributed to uncertainties in the data and analysis.

 

 
Table B.1: Assigned average values of $\sigma_{\log gf}$ for each element.
Element $\sigma_{\log gf}$ Element $\sigma_{\log gf}$
C 0.10 Ni 0.03
Mg 0.07 Zn 0.10
Al 0.11 Sr 0.10
Ca 0.11 Y 0.03
Sc 0.04 Zr 0.03
Ti 0.05 Ba 0.03
V 0.05 La 0.03
Cr 0.05 Ce 0.10
Mn 0.06 Nd 0.03
Fe 0.03 Sm 0.05
Co 0.10 Eu 0.03


First, from Sect. 2.1, we adopt $\sigma_T=100$ K. If the measurement errors in the observed data are normally distributed, the formal random errors in derived spectrum modelling parameters due to this measurement error are given by the SME optimisation routine from the estimated covariance matrix, which is the inverse of the curvature matrix at the solution (see e.g. Press et al 1992). These errors represent the propagation of the random observational uncertainties in each point in the spectrum (dominated by photon noise) to the relevant parameter and is computed by the parameter optimisation procedure. Such contributions are obtained for $\sigma_{\varepsilon}({\rm obs})$, $\sigma_{\log g}$ and $\sigma_{\xi}$; these random components of $\sigma_{\log g}$ and $\sigma_{\xi}$ are usually quite small, around 0.05 dex and 0.05 km s-1, while $\sigma_{\varepsilon}({\rm obs})$ varies significantly from element to element. To this random component of $\sigma_{\log g}$ we add 0.22 dex reflecting the error due to uncertainty in  $T_{\rm eff}$, and to the random component of $\sigma_{\xi}$ we add 0.1 km s-1 reflecting the error due to uncertainty in $\log g$. These numbers are based on the numerical experiments for a representative subsample which were mentioned above.

As mentioned above, errors arise due to uncertainties in the spectrum modelling, for example, assumptions of 1D geometry or LTE. The contributions of these errors to relative errors in abundances would be expected to cancel if all the stars were identical; however, across our sample, which covers a wide range of stellar atmosphere parameters, we can only expect partial cancellation. Thus, such uncertainties will lead to a degree of scatter in any quantity derived from the spectrum, arising from differences in modelling errors from star to star. The relative component of $\sigma_{\varepsilon}({\rm model})$ has been estimated at 0.1 dex. This is simply an order-of-magnitude estimate based on indications from 3-D modelling, (e.g. Asplund 2004,2005) and non-LTE spectrum modelling (e.g. Korn et al. 2003; Asplund 2005). However it should be noted this quantity should vary with element and employed spectral feature. We have neglected any relative error in $\log g$ and $\xi $ which might arise from modelling uncertainties.

Since the relevant continuum points are located close to lines employed in the analysis, they will have very similar error bars to the points in the line, and thus the sensitivity of the abundance to continuum placement errors will be essentially identical to that for the points in the line. Thus we expect that the error due to uncertainty in the continuum placement can be approximated by $\sigma_{\varepsilon}({\rm cont})\approx\sigma_{\varepsilon}({\rm obs})/\sqrt{m}$, where the $1/\sqrt{m}$ factor accounts for the fact that we typically have m times more independent pixels to define the continuum than the line. Based on inspection of spectra we adopt m=5 for all elements except carbon, where we adopt m=1 since it is determined from wide molecular bands. The estimates for m approximately account for possible correlations between pixels introduced by very weak lines. The uncertainty in $\log gf$ will not contribute to relative errors, and thus we adopt $\sigma_{\log gf}=0$.

B.2 Absolute error estimates

While relative errors are generally of most interest, it is also important to have some estimate of the absolute error in our obtained abundances. The calculation of absolute errors follows that of the relative errors with a few changes which we now list.

The main differences arise in the modelling uncertainties, as there is no cancellation as in the relative error case. To $\sigma_{\log g}$ and $\sigma_{\xi}$ we add an additional 0.1 dex and 0.1 km s-1 respectively to account for modelling uncertainties. We estimate $\sigma_{\varepsilon}({\rm model})$ at 0.15 dex. Further, the errors $\sigma_{\log gf}$ must be included in the absolute errors. Since our procedure globally fits the spectral lines of a given element, the value for $\sigma_{\log gf}$ should be representative of the typical error for the chosen spectral lines. In Table B.1 we provide an estimated average uncertainty for each element with reference to the original literature, which are adopted for $\sigma_{\log gf}$.

B.3 Errors in abundance ratios

We are often interested in elemental abundance ratios. Following McWilliam et al. (1995b), if the abundances $\varepsilon_A$ and $\varepsilon_B$ are expressed in logarithms such that $\varepsilon_{A/B}=\varepsilon_A-\varepsilon_B$, the variance in the abundance ratio $\varepsilon_{A/B}$ is given by

 \begin{displaymath}\sigma_{A/B}^2 = \sigma_{A}^2 + \sigma_{B}^2 - 2 \sigma_{A,B}
\end{displaymath} (B.3)

where $\sigma_{A}^2$ and $\sigma_{B}^2$ are the variance in $\varepsilon_A$ and $\varepsilon_B$ respectively and  $\sigma_{A,B}$ is the covariance of $\varepsilon_A$ and $\varepsilon_B$ given by

                                       $\displaystyle \sigma_{A,B}$ = $\displaystyle \frac{\partial\varepsilon_A}{\partial T} \frac{\partial\varepsilo...
...silon_A}{\partial \xi}\frac{\partial\varepsilon_B}{\partial \xi} \sigma_{\xi}^2$  
    $\displaystyle + \left\{ \frac{\partial\varepsilon_A}{\partial T}\frac{\partial\...
...tial \log g}\frac{\partial\varepsilon_B}{\partial T}\right\} \sigma_{T, \log g}$  
    $\displaystyle + \left\{ \frac{\partial\varepsilon_A}{\partial \xi}\frac{\partia...
...\log g}\frac{\partial\varepsilon_B}{\partial \xi}\right\} \sigma_{\log g, \xi}.$ (B.4)

Thus, as pointed out by McWilliam et al. (1995b), there may be partial cancellation of errors if the abundances of elements A and B have similar sensitivity to atmospheric parameters, or partial compounding of errors if the elements have contrary sensitivity. Note, abundance ratio error estimates may be computed in both the absolute and relative senses.


 

 
Table 1F: Coordinates of the HES stars (prefix HE) have been derived from the Digitized Sky Survey I and are accurate to 1 $^{\prime \prime }$; the coordinates of the HK survey stars (prefix CS) are from identifications of the sources in the 2MASS All Sky Release. Barycentric radial velocities $v_{\rm rad}$ were measured from the snapshot spectra and are accurate to a few km s-1.
Star $\alpha(2000.0)$ $\delta(2000.0)$ $v_{\rm rad}$
      [km s-1]
CS 22175-007 02 17 26.6 -09 00 45 -18.3
CS 22186-023 04 19 45.5 -36 51 35 51.9
CS 22186-025 04 24 32.8 -37 09 02 -122.6
CS 22886-042 22 20 25.8 -10 23 20 -220.6
CS 22892-052 22 17 01.6 -16 39 27 14.5
CS 22945-028 23 31 13.5 -66 29 57 388.9
CS 22957-013 23 55 49.0 -05 22 52 -213.5
CS 22958-083 02 15 42.7 -53 59 56 175.6
CS 22960-010 22 08 25.3 -44 53 56 49.2
CS 29491-069 22 31 02.1 -32 38 36 -375.5
CS 29491-109 22 25 01.1 -32 14 41 160.1
CS 29497-004 00 28 06.9 -26 03 04 105.1
CS 29510-058 02 21 46.5 -24 01 58 153.1
CS 30308-035 20 45 54.1 -44 50 29 -51.8
CS 30315-001 23 37 38.8 -26 21 53 110.3
CS 30315-029 23 34 26.6 -26 42 14 -169.2
CS 30337-097 22 01 21.5 -30 57 57 -108.7
CS 30339-041 00 23 12.9 -37 01 26 -19.3
CS 30343-063 21 45 17.5 -37 22 18 -59.4
CS 31060-047 00 08 07.8 -15 54 03 106.1
CS 31062-041 00 35 03.0 -15 54 29 -173.0
CS 31072-118 05 08 53.5 -59 18 21 145.8
CS 31082-001 01 29 31.1 -16 00 45 139.4
HD 20 00 05 15.3 -27 16 18 -57.5
HD 221170 23 29 28.8 +30 25 57 -120.7
HE 0005-0002 00 08 06.8 +00 14 09 -65.4
HE 0008-3842 00 10 56.0 -38 26 10 128.9
HE 0017-4838 00 19 48.3 -48 21 24 26.8
HE 0018-1349 00 20 52.4 -13 32 29 -161.7
HE 0023-4825 00 25 50.3 -48 08 27 -21.5
HE 0029-1839 00 32 07.7 -18 22 36 -97.8
HE 0037-2657 00 39 51.7 -26 41 31 -279.0
HE 0039-4154 00 41 43.3 -41 37 58 128.9
HE 0043-2845 00 45 55.8 -28 29 16 16.4
HE 0044-2459 00 46 35.8 -24 43 02 -160.0
HE 0044-4023 00 46 29.4 -40 07 23 346.2
HE 0045-2430 00 47 40.5 -24 14 02 144.5
HE 0049-5700 00 52 06.8 -56 44 37 59.8
HE 0051-2304 00 53 51.5 -22 47 55 -135.6
HE 0054-0657 00 57 20.7 -06 41 00 51.3
HE 0057-4541 00 59 59.2 -45 24 54 13.4
HE 0104-4007 01 06 56.0 -39 51 52 200.8
HE 0104-5300 01 06 51.8 -52 44 11 185.8
HE 0105-6141 01 07 38.0 -61 25 17 3.8
HE 0109-0742 01 11 47.0 -07 26 32 -24.1
HE 0109-3711 01 11 38.4 -36 55 17 -1.0
HE 0111-1454 01 13 49.1 -14 38 23 -85.2
HE 0121-2826 01 23 37.2 -28 10 27 -2.0
HE 0131-2740 01 33 25.8 -27 25 28 51.7
HE 0131-3953 01 33 36.4 -39 37 52 67.5
HE 0143-1135 01 46 10.2 -11 20 10 -223.1
HE 0143-4108 01 45 19.9 -40 53 37 55.5
HE 0143-4146 01 45 18.0 -41 31 48 -16.3
HE 0157-3335 02 00 00.2 -33 21 23 -175.2
HE 0200-0955 02 03 16.2 -09 40 48 73.6
HE 0202-2204 02 04 50.0 -21 50 10 108.2
HE 0231-4016 02 33 44.3 -40 03 44 180.8
HE 0240-0807 02 42 57.6 -07 54 35 -98.8
HE 0240-6105 02 42 06.2 -60 53 03 153.0
HE 0243-0753 02 46 14.1 -07 40 53 -13.0
HE 0243-5238 02 45 36.2 -52 25 58 112.3
HE 0244-4111 02 45 57.4 -40 59 08 214.3
HE 0248+0039 02 50 59.0 +00 51 32 48.9
HE 0249-0126 02 51 39.7 -01 14 33 15.1
HE 0256-1109 02 59 10.1 -10 58 01 -132.3
HE 0300-0751 03 03 04.0 -07 39 42 155.5
HE 0305-4520 03 07 02.1 -45 09 00 135.3
HE 0308-1154 03 11 09.8 -11 43 20 13.4
HE 0315+0000 03 17 39.0 +00 11 04 -120.8
HE 0316+0214 03 19 09.2 +02 24 54 -161.0
HE 0317-4640 03 18 56.2 -46 29 27 9.3
HE 0323-4529 03 25 30.1 -45 19 31 180.6
HE 0328-1047 03 30 45.2 -10 37 10 -75.0
HE 0330-4004 03 32 07.3 -39 54 51 227.0
HE 0330-4144 03 32 16.1 -41 34 49 134.2
HE 0331-4939 03 32 41.8 -49 29 10 273.4
HE 0333-4001 03 35 25.7 -39 51 48 -162.3
HE 0336-3829 03 38 31.7 -38 20 15 -109.1
HE 0337-5127 03 39 13.0 -51 18 16 75.4
HE 0338-3945 03 39 54.9 -39 35 44 177.7
HE 0339-4027 03 40 49.6 -40 17 36 22.0
HE 0340-3430 03 42 04.7 -34 20 50 228.1
HE 0340-5355 03 41 34.6 -53 46 17 317.5
HE 0341-4024 03 43 07.9 -40 15 30 211.8
HE 0344+0139 03 47 15.7 +01 49 03 -232.9
HE 0347-1819 03 49 18.4 -18 10 40 -4.8
HE 0353-6024 03 53 59.5 -60 15 16 178.8
HE 0400-2917 04 02 06.4 -29 08 47 296.8
HE 0401-0138 04 03 49.8 -01 30 03 137.4
HE 0417-0821 04 19 31.4 -08 14 19 -8.5
HE 0430-4404 04 31 38.1 -43 57 49 201.5
HE 0430-4901 04 31 31.1 -48 54 42 208.7
HE 0432-0923 04 34 25.6 -09 16 50 -66.5
HE 0436-4008 04 38 11.0 -40 03 01 185.7
HE 0441-4343 04 43 20.4 -43 38 20 165.0
HE 0442-1234 04 44 51.7 -12 28 46 253.4
HE 0447-4858 04 49 01.0 -48 53 35 88.5
HE 0450-4705 04 51 33.4 -47 00 03 -6.3
HE 0454-4758 04 55 26.7 -47 53 42 240.5
HE 0501-5139 05 02 48.1 -51 35 36 199.3
HE 0501-5644 05 02 35.3 -56 40 20 70.8
HE 0512-3835 05 13 59.5 -38 31 55 276.2
HE 0513-4557 05 15 12.1 -45 54 10 51.2
HE 0516-3820 05 18 12.9 -38 17 33 153.5
HE 0517-1952 05 19 18.7 -19 49 13 42.2
HE 0519-5525 05 19 59.1 -55 22 41 377.4
HE 0520-1748 05 22 25.8 -17 46 08 1.3
HE 0524-2055 05 27 04.4 -20 52 42 255.3
HE 0534-4615 05 35 52.9 -46 13 36 280.4
HE 0538-4515 05 39 46.1 -45 13 34 59.2
HE 0547-4539 05 49 13.7 -45 39 04 488.8
HE 0858-0016 09 01 32.3 -00 28 02 48.6
HE 0926-0508 09 28 55.3 -05 21 39 191.0
HE 0938+0114 09 40 43.0 +01 00 37 -56.6
HE 0951-1152 09 54 17.4 -12 06 14 353.9
HE 1006-2218 10 09 00.7 -22 33 29 -19.6
HE 1015-0027 10 17 35.7 -00 42 24 96.8
HE 1044-2509 10 47 16.5 -25 25 17 386.7
HE 1052-2548 10 55 20.6 -26 04 47 230.4
HE 1054-0059 10 56 47.7 -01 15 29 234.0
HE 1059-0118 11 02 03.4 -01 34 15 296.6
HE 1100-0137 11 02 55.5 -01 53 41 318.1
HE 1105+0027 11 07 49.5 +00 11 38 77.0
HE 1120-0153 11 22 43.2 -02 09 36 228.4
HE 1122-1429 11 25 06.6 -14 46 04 152.0
HE 1124-2335 11 27 27.0 -23 52 06 180.4
HE 1126-1735 11 28 51.4 -17 51 44 281.9
HE 1127-1143 11 29 50.5 -12 00 13 228.5
HE 1128-0823 11 30 44.3 -08 39 56 200.2
HE 1131+0141 11 34 32.1 +01 24 41 267.7
HE 1132+0125 11 34 46.7 +01 09 01 92.0
HE 1132+0204 11 34 51.0 +01 47 27 238.2
HE 1135+0139 11 38 09.8 +01 22 44 11.0
HE 1135-0344 11 38 21.0 -04 01 24 -167.4
HE 1148-0037 11 51 15.0 -00 54 11 -36.6
HE 1207-2031 12 09 50.8 -20 47 43 113.3
HE 1210+0048 12 13 27.8 +00 32 10 110.4
HE 1210-1956 12 12 50.9 -20 12 58 123.3
HE 1212-0127 12 15 18.3 -01 43 56 279.4
HE 1214-1819 12 17 01.5 -18 35 55 180.3
HE 1215+0149 12 17 43.1 +01 32 32 124.5
HE 1217-0540 12 19 53.7 -05 57 15 151.2
HE 1219-0312 12 21 34.1 -03 28 40 163.6
HE 1221-0522 12 24 07.7 -05 39 11 48.6
HE 1221-1948 12 23 47.7 -20 04 46 31.6
HE 1222-0200 12 25 29.4 -02 17 24 226.8
HE 1222-0336 12 24 52.4 -03 53 06 -198.5
HE 1225+0155 12 28 04.8 +01 38 32 99.4
HE 1225-0515 12 28 12.4 -05 31 40 61.5
HE 1230-1724 12 32 57.0 -17 41 27 99.1
HE 1243-1425 12 46 28.1 -14 41 34 41.8
HE 1245-1616 12 47 56.8 -16 32 44 141.9
HE 1246-1344 12 49 20.2 -14 00 42 47.9
HE 1247-2114 12 50 05.1 -21 30 47 75.7
HE 1248-1800 12 51 28.0 -18 16 30 280.7
HE 1249-2932 12 52 18.4 -29 48 57 -13.3
HE 1249-3121 12 52 05.1 -31 37 44 218.7
HE 1251-0104 12 53 52.1 -01 20 36 195.1
HE 1252+0044 12 55 22.1 +00 28 00 395.5
HE 1252-0117 12 54 59.8 -01 33 35 225.7
HE 1254+0009 12 57 12.9 -00 06 41 168.5
HE 1256-0228 12 58 38.4 -02 44 18 30.4
HE 1256-0651 12 59 13.1 -07 07 18 120.1
HE 1259-0621 13 01 51.1 -06 37 14 130.6
HE 1300+0157 13 02 56.3 +01 41 51 73.6
HE 1300-0641 13 03 34.1 -06 57 21 67.9
HE 1300-0642 13 03 23.3 -06 58 23 -16.4
HE 1300-2201 13 03 17.3 -22 17 38 -62.8
HE 1300-2431 13 03 00.1 -24 47 12 308.1
HE 1305-0331 13 07 58.9 -03 47 41 -38.4
HE 1311-1412 13 13 42.0 -14 28 24 195.3
HE 1314-3036 13 17 29.2 -30 51 51 34.6
HE 1320-1339 13 22 44.1 -13 55 31 172.1
HE 1330-0354 13 33 10.7 -04 10 05 35.3
HE 1330-0607 13 32 56.6 -06 22 31 -32.4
HE 1332-0309 13 34 38.0 -03 24 53 200.3
HE 1333-0340 13 35 51.5 -03 55 49 -114.6
HE 1335+0135 13 37 53.9 +01 20 26 121.0
HE 1337+0012 13 40 02.7 -00 02 18 441.7
HE 1337-0453 13 39 58.3 -05 08 32 79.3
HE 1343-0640 13 46 09.1 -06 55 46 62.1
HE 1345-0206 13 48 16.0 -02 21 47 124.7
HE 1351-1049 13 53 57.1 -11 04 24 285.4
HE 1413-1954 14 16 04.7 -20 08 54 -100.4
HE 1419-1759 14 22 17.7 -18 13 30 201.4
HE 1421-2006 14 23 50.5 -20 20 11 3.8
HE 1430+0053 14 33 16.5 +00 40 49 -107.4
HE 1430-0026 14 33 16.2 -00 39 49 50.6
HE 1430-1123 14 33 33.7 -11 37 08 93.4
HE 1431-2142 14 34 06.7 -21 55 16 -165.0
HE 1500-1628 15 02 56.6 -16 40 07 23.5
HE 2133-1432 21 36 22.6 -14 19 20 -129.0
HE 2134+0001 21 37 08.2 +00 15 04 48.0
HE 2139-1851 21 42 29.5 -18 37 51 -91.6
HE 2143+0030 21 46 12.0 +00 44 46 -76.2
HE 2145-3025 21 48 43.3 -30 11 08 131.4
HE 2150-0825 21 53 00.2 -08 11 19 -63.3
HE 2151-2858 21 54 01.7 -28 44 20 -89.7
HE 2153-2719 21 56 04.1 -27 04 49 -111.8
HE 2154-2838 21 57 43.7 -28 24 31 -16.9
HE 2155+0136 21 57 37.7 +01 50 20 -248.2
HE 2156-3130 21 59 05.8 -31 16 12 269.8
HE 2158-3112 22 01 21.4 -30 57 57 -110.0
HE 2200-2030 22 03 02.6 -20 15 58 89.7
HE 2201-0637 22 03 44.6 -06 22 42 114.0
HE 2204-1703 22 07 12.0 -16 49 10 -11.7
HE 2206-2245 22 09 09.4 -22 30 17 -210.5
HE 2216-0621 22 18 46.1 -06 06 50 52.5
HE 2216-1548 22 19 30.5 -15 33 36 -271.0
HE 2217-0706 22 20 18.0 -06 51 17 -93.3
HE 2217-1523 22 20 33.8 -15 08 34 79.5
HE 2219-0713 22 22 15.8 -06 58 34 -111.8
HE 2221-4150 22 24 47.3 -41 35 38 40.2
HE 2222-4156 22 25 28.6 -41 40 57 -126.0
HE 2224+0143 22 27 23.0 +01 58 33 -112.3
HE 2224-4103 22 27 48.2 -40 48 25 -60.7
HE 2226-4102 22 29 04.3 -40 46 53 96.0
HE 2227-4044 22 30 19.2 -40 29 13 103.9
HE 2228-3806 22 31 02.6 -37 50 41 179.0
HE 2229-4153 22 32 49.0 -41 38 25 -139.6
HE 2231-0622 22 34 20.2 -06 06 30 -428.8
HE 2234-0521 22 36 37.7 -05 06 05 -177.8
HE 2238-2152 22 41 10.3 -21 36 19 -22.2
HE 2240-0412 22 42 58.1 -03 56 33 -163.7
HE 2242-1930 22 45 17.3 -19 14 52 -22.5
HE 2243-0151 22 46 08.9 -01 35 55 -47.4
HE 2244-1503 22 47 25.9 -14 47 30 148.1
HE 2247-3705 22 50 29.5 -36 49 17 143.6
HE 2248-3345 22 51 44.6 -33 29 25 145.4
HE 2250-2132 22 53 40.3 -21 16 24 -207.6
HE 2252-4157 22 55 34.1 -41 41 29 -94.5
HE 2252-4225 22 54 58.6 -42 09 19 -333.7
HE 2258-3456 23 00 59.8 -34 40 42 -229.0
HE 2259-3407 23 02 15.6 -33 51 11 -13.6
HE 2301-4024 23 04 13.9 -40 08 21 -221.7
HE 2301-4126 23 03 50.2 -41 10 27 252.2
HE 2304-4153 23 07 05.5 -41 37 30 -33.9
HE 2311+0129 23 14 21.4 +01 45 24 -149.0
HE 2314-1554 23 17 01.2 -15 37 49 72.8
HE 2319-0852 23 22 17.3 -08 36 17 -121.6
HE 2325-0755 23 27 59.5 -07 39 12 -237.0
HE 2326+0038 23 28 56.9 +00 54 35 -40.9
HE 2327-5642 23 30 37.2 -56 26 14 282.1
HE 2329-3702 23 32 18.0 -36 45 59 71.7
HE 2333-1358 23 35 48.5 -13 41 31 96.7
HE 2334-0604 23 37 28.6 -05 47 56 -18.5
HE 2335-5958B 23 38 19.4 -59 42 05 210.7
HE 2338-1311 23 41 08.3 -12 55 10 -84.0
HE 2338-1618 23 40 36.2 -16 01 28 -219.4
HE 2345-1919 23 47 55.4 -19 02 37 119.4
HE 2347-1254 23 50 09.8 -12 37 50 -43.5
HE 2347-1334 23 50 26.9 -13 17 39 -54.8
HE 2347-1448 23 49 58.3 -14 32 16 -165.1



 
Table 2F: Derived stellar atmosphere parameters and elemental abundances for the sample. For each star we report the average signal-to-noise ratio per pixel for the whole observed spectrum, the stellar parameters with their respective relative and absolute r.m.s. error estimates, $\sigma^\mathrm{rel}$ and $\sigma^\mathrm{abs}$, then for each element X the abundance $\log \epsilon_\mathrm{X}$ and its relative and absolute r.m.s. error estimates $\sigma_{\log\epsilon_\mathrm{X}}$, [X/Fe] and its relative and absolute r.m.s. error estimates $\sigma_\mathrm{[X/Fe]}$. N gives the number of features of the element used in each star, noting that this varies from star to star as certain features may be automatically rejected if the star has a strong G band, if the feature is near a Balmer line in warmer stars (see Sect. 3.2), or if they are determined to be affected by a cosmic ray hit or bad pixel. N3 then gives the number of those features classified as 3$\sigma $ detections. In the case of CH bands we simply classify detections and non-detections with 1 and 0 respectively. In the case of a non-detection, this is signified by an abundance of -9.99 and error of 0.00.
Star S/Nav Teff $\sigma_{T_\mathrm{eff}}$ $\log g$ $\sigma_{\log g}^\mathrm{rel}$ $\sigma_{\log g}^\mathrm{abs}$ [Fe/H] $\sigma_\mathrm{[Fe/H]}^\mathrm{rel}$ $\sigma_\mathrm{[Fe/H]}^\mathrm{abs}$ $\xi $ $\sigma_\xi^\mathrm{rel}$ $\sigma_\xi^\mathrm{abs}$ $\log\epsilon_\mathrm{C}$ $\sigma_{\log\epsilon_\mathrm{C}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{C}}^\mathrm{abs}$ [C/Fe] $\sigma_\mathrm{[C/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[C/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Mg}$ $\sigma_{\log\epsilon_\mathrm{Mg}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Mg}}^\mathrm{abs}$ [Mg/Fe] $\sigma_\mathrm{[Mg/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Mg/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Al}$ $\sigma_{\log\epsilon_\mathrm{Al}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Al}}^\mathrm{abs}$ [Al/Fe] $\sigma_\mathrm{[Al/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Al/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Ca}$ $\sigma_{\log\epsilon_\mathrm{Ca}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Ca}}^\mathrm{abs}$ [Ca/Fe] $\sigma_\mathrm{[Ca/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Ca/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Sc}$ $\sigma_{\log\epsilon_\mathrm{Sc}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Sc}}^\mathrm{abs}$ [Sc/Fe] $\sigma_\mathrm{[Sc/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Sc/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Ti}$ $\sigma_{\log\epsilon_\mathrm{Ti}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Ti}}^\mathrm{abs}$ [Ti/Fe] $\sigma_\mathrm{[Ti/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Ti/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{V}$ $\sigma_{\log\epsilon_\mathrm{V}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{V}}^\mathrm{abs}$ [V/Fe] $\sigma_\mathrm{[V/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[V/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Cr}$ $\sigma_{\log\epsilon_\mathrm{Cr}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Cr}}^\mathrm{abs}$ [Cr/Fe] $\sigma_\mathrm{[Cr/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Cr/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Mn}$ $\sigma_{\log\epsilon_\mathrm{Mn}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Mn}}^\mathrm{abs}$ [Mn/Fe] $\sigma_\mathrm{[Mn/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Mn/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Fe}$ $\sigma_{\log\epsilon_\mathrm{Fe}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Fe}}^\mathrm{abs}$ [Fe/Fe] $\sigma_\mathrm{[Fe/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Fe/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Co}$ $\sigma_{\log\epsilon_\mathrm{Co}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Co}}^\mathrm{abs}$ [Co/Fe] $\sigma_\mathrm{[Co/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Co/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Ni}$ $\sigma_{\log\epsilon_\mathrm{Ni}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Ni}}^\mathrm{abs}$ [Ni/Fe] $\sigma_\mathrm{[Ni/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Ni/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Zn}$ $\sigma_{\log\epsilon_\mathrm{Zn}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Zn}}^\mathrm{abs}$ [Zn/Fe] $\sigma_\mathrm{[Zn/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Zn/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Sr}$ $\sigma_{\log\epsilon_\mathrm{Sr}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Sr}}^\mathrm{abs}$ [Sr/Fe] $\sigma_\mathrm{[Sr/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Sr/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Y}$ $\sigma_{\log\epsilon_\mathrm{Y}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Y}}^\mathrm{abs}$ [Y/Fe] $\sigma_\mathrm{[Y/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Y/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Zr}$ $\sigma_{\log\epsilon_\mathrm{Zr}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Zr}}^\mathrm{abs}$ [Zr/Fe] $\sigma_\mathrm{[Zr/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Zr/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Ba}$ $\sigma_{\log\epsilon_\mathrm{Ba}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Ba}}^\mathrm{abs}$ [Ba/Fe] $\sigma_\mathrm{[Ba/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Ba/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{La}$ $\sigma_{\log\epsilon_\mathrm{La}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{La}}^\mathrm{abs}$ [La/Fe] $\sigma_\mathrm{[La/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[La/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Ce}$ $\sigma_{\log\epsilon_\mathrm{Ce}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Ce}}^\mathrm{abs}$ [Ce/Fe] $\sigma_\mathrm{[Ce/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Ce/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Nd}$ $\sigma_{\log\epsilon_\mathrm{Nd}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Nd}}^\mathrm{abs}$ [Nd/Fe] $\sigma_\mathrm{[Nd/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Nd/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Sm}$ $\sigma_{\log\epsilon_\mathrm{Sm}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Sm}}^\mathrm{abs}$ [Sm/Fe] $\sigma_\mathrm{[Sm/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Sm/Fe]}^\mathrm{abs}$ N N3 $\log\epsilon_\mathrm{Eu}$ $\sigma_{\log\epsilon_\mathrm{Eu}}^\mathrm{rel}$ $\sigma_{\log\epsilon_\mathrm{Eu}}^\mathrm{abs}$ [Eu/Fe] $\sigma_\mathrm{[Eu/Fe]}^\mathrm{rel}$ $\sigma_\mathrm{[Eu/Fe]}^\mathrm{abs}$ N N3
    [K]   [cm s-2]           [km s-1]                                                                                                                                                                                                                                                                                                                                                                    
CS 22175-007 31 5108 100 2.46 0.26 0.36 -2.81 0.13 0.18 1.67 0.14 0.24 5.77 0.19 0.26 0.19 0.18 0.27 1 1 5.15 0.12 0.18 0.37 0.15 0.24 7 4 2.54 0.17 0.25 -1.12 0.18 0.26 1 1 3.87 0.12 0.20 0.31 0.15 0.25 9 5 0.49 0.18 0.23 0.13 0.16 0.25 5 3 2.56 0.17 0.22 0.34 0.15 0.24 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.52 0.17 0.24 -0.35 0.16 0.24 3 3 1.84 0.17 0.22 -0.74 0.16 0.23 5 3 4.69 0.13 0.18 0.00 0.14 0.22 55 35 2.35 0.15 0.22 0.24 0.15 0.24 6 4 3.70 0.20 0.30 0.25 0.19 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.33 0.20 0.30 0.16 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.15 0.21 0.25 -0.47 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 22186-023 55 5066 100 2.19 0.24 0.34 -2.72 0.13 0.18 1.58 0.11 0.21 5.97 0.19 0.25 0.30 0.18 0.27 1 1 4.99 0.12 0.18 0.14 0.15 0.23 7 6 2.78 0.15 0.24 -0.97 0.16 0.26 1 1 3.77 0.12 0.20 0.13 0.15 0.25 9 7 0.46 0.17 0.23 0.01 0.15 0.24 5 4 2.44 0.16 0.21 0.15 0.15 0.23 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.68 0.16 0.25 -0.27 0.15 0.25 3 3 2.27 0.15 0.21 -0.39 0.15 0.23 5 3 4.78 0.13 0.18 0.00 0.14 0.22 55 50 2.33 0.16 0.22 0.13 0.15 0.24 6 5 3.56 0.17 0.28 0.03 0.17 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.10 0.19 0.30 -0.14 0.18 0.29 3 2 -0.89 0.18 0.23 -0.41 0.15 0.24 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.52 0.19 0.23 -0.93 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 22186-025 32 4985 100 1.70 0.26 0.36 -2.87 0.14 0.19 2.14 0.13 0.23 4.83 0.20 0.27 -0.68 0.19 0.29 1 1 4.99 0.12 0.18 0.28 0.15 0.24 7 3 2.60 0.21 0.27 -1.00 0.21 0.29 1 1 3.75 0.12 0.20 0.26 0.15 0.25 9 3 0.44 0.18 0.23 0.14 0.16 0.24 5 4 2.40 0.15 0.20 0.26 0.14 0.23 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.35 0.16 0.23 -0.44 0.15 0.23 3 3 1.85 0.16 0.21 -0.67 0.15 0.23 5 3 4.63 0.14 0.19 0.00 0.14 0.22 55 36 2.26 0.15 0.22 0.21 0.15 0.24 6 4 3.12 0.19 0.25 -0.26 0.18 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.20 0.25 0.35 -0.29 0.23 0.33 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.59 0.24 0.31 0.16 0.21 0.30 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 22886-042 39 4881 100 1.85 0.25 0.35 -2.68 0.12 0.18 1.84 0.12 0.22 5.72 0.19 0.26 0.01 0.19 0.28 1 1 5.13 0.12 0.18 0.23 0.15 0.23 7 6 2.70 0.17 0.26 -1.10 0.18 0.27 1 1 3.90 0.12 0.20 0.22 0.14 0.25 9 7 0.50 0.17 0.23 0.01 0.16 0.25 5 4 2.50 0.16 0.21 0.16 0.15 0.24 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.64 0.17 0.26 -0.35 0.17 0.25 3 3 2.20 0.15 0.21 -0.51 0.15 0.23 5 3 4.82 0.12 0.18 0.00 0.14 0.22 55 47 2.34 0.14 0.21 0.10 0.15 0.24 6 5 3.46 0.19 0.28 -0.11 0.19 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.13 0.20 0.30 -0.16 0.19 0.29 3 2 -0.68 0.18 0.23 -0.25 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.67 0.24 0.31 -0.12 0.22 0.30 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 22892-052 46 4884 100 1.81 0.26 0.36 -2.95 0.14 0.19 1.67 0.12 0.22 6.44 0.19 0.26 1.00 0.18 0.28 1 1 4.75 0.13 0.19 0.12 0.15 0.24 5 5 2.79 0.16 0.26 -0.72 0.18 0.28 1 1 3.63 0.12 0.20 0.22 0.15 0.25 5 3 0.20 0.17 0.22 -0.01 0.15 0.24 3 2 2.12 0.15 0.20 0.05 0.14 0.22 11 8 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 2.25 0.17 0.25 -0.47 0.17 0.25 1 1 1.77 0.12 0.20 -0.67 0.15 0.23 4 2 4.55 0.14 0.19 0.00 0.14 0.22 35 27 1.99 0.15 0.22 0.02 0.15 0.24 4 4 3.39 0.20 0.29 0.09 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 0.63 0.16 0.23 0.61 0.15 0.24 2 2 -0.26 0.18 0.23 0.45 0.15 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.37 0.16 0.21 1.19 0.15 0.23 2 1 -0.76 0.18 0.23 1.02 0.16 0.24 3 3 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -0.31 0.19 0.23 1.14 0.16 0.24 5 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -0.90 0.18 0.23 1.54 0.15 0.24 3 3
CS 22945-028 31 5126 100 2.55 0.26 0.36 -2.66 0.13 0.18 1.53 0.14 0.24 5.93 0.19 0.26 0.21 0.18 0.27 1 1 5.24 0.13 0.18 0.32 0.15 0.23 7 4 2.83 0.18 0.26 -0.97 0.19 0.28 1 1 4.03 0.11 0.20 0.33 0.15 0.25 9 6 0.47 0.18 0.23 -0.04 0.16 0.25 5 2 2.57 0.16 0.21 0.22 0.15 0.24 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.77 0.18 0.26 -0.24 0.17 0.25 3 3 2.18 0.18 0.23 -0.55 0.16 0.24 5 3 4.84 0.13 0.18 0.00 0.14 0.22 55 38 2.39 0.16 0.22 0.14 0.15 0.25 6 4 3.61 0.22 0.30 0.02 0.21 0.29 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.37 0.21 0.30 0.06 0.20 0.29 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.66 0.23 0.28 -0.13 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 22957-013 35 4904 100 1.96 0.25 0.35 -2.64 0.14 0.19 1.79 0.12 0.22 5.85 0.19 0.26 0.10 0.17 0.27 1 1 5.11 0.11 0.18 0.17 0.16 0.24 7 5 2.89 0.20 0.26 -0.94 0.20 0.28 1 1 3.91 0.12 0.20 0.19 0.15 0.25 9 7 0.59 0.18 0.23 0.06 0.15 0.24 5 4 2.54 0.15 0.21 0.16 0.14 0.22 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.49 0.18 0.26 -0.54 0.16 0.25 3 3 2.25 0.16 0.22 -0.50 0.15 0.23 5 3 4.86 0.14 0.19 0.00 0.14 0.22 55 44 2.46 0.16 0.23 0.18 0.15 0.24 6 5 3.52 0.21 0.30 -0.09 0.19 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.06 0.20 0.31 -0.27 0.19 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.06 0.21 0.27 -0.54 0.18 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 22958-083 32 5101 100 2.40 0.26 0.36 -2.79 0.12 0.18 1.50 0.13 0.23 6.24 0.20 0.26 0.64 0.18 0.27 1 1 5.19 0.12 0.18 0.40 0.15 0.23 7 6 2.80 0.17 0.26 -0.88 0.19 0.28 1 1 3.89 0.12 0.20 0.32 0.15 0.24 9 6 0.41 0.19 0.24 0.03 0.17 0.26 5 3 2.52 0.16 0.21 0.29 0.15 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.78 0.17 0.27 -0.10 0.17 0.27 3 3 2.33 0.16 0.22 -0.27 0.16 0.24 5 3 4.71 0.12 0.18 0.00 0.14 0.22 55 37 2.41 0.16 0.22 0.28 0.15 0.24 6 5 3.74 0.19 0.29 0.28 0.19 0.29 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.12 0.21 0.31 -0.06 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.65 0.19 0.24 -0.99 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 22960-010 35 5737 100 4.85 0.25 0.35 -2.65 0.12 0.17 1.53 0.17 0.27 6.56 0.17 0.24 0.82 0.16 0.25 1 1 5.18 0.13 0.19 0.25 0.15 0.24 7 1 2.90 0.14 0.21 -0.92 0.15 0.25 1 1 3.97 0.12 0.20 0.27 0.14 0.24 9 3 0.69 0.18 0.23 0.17 0.17 0.27 5 1 2.57 0.16 0.21 0.20 0.16 0.26 17 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.89 0.15 0.20 -0.13 0.15 0.23 3 3 2.46 0.15 0.20 -0.28 0.15 0.24 5 3 4.85 0.12 0.17 0.00 0.14 0.22 55 29 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.53 0.16 0.21 -0.06 0.16 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 29491-069 57 5103 100 2.45 0.24 0.34 -2.81 0.13 0.18 1.54 0.12 0.22 5.76 0.19 0.25 0.18 0.17 0.27 1 1 5.05 0.11 0.18 0.28 0.15 0.24 7 6 2.64 0.14 0.23 -1.03 0.15 0.25 1 1 3.84 0.12 0.20 0.29 0.15 0.25 9 8 0.37 0.17 0.22 0.00 0.15 0.24 5 4 2.42 0.16 0.21 0.20 0.14 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.58 0.16 0.24 -0.29 0.15 0.24 3 3 2.01 0.17 0.22 -0.57 0.15 0.23 5 3 4.69 0.13 0.18 0.00 0.14 0.22 55 46 2.28 0.16 0.22 0.16 0.15 0.24 6 5 3.40 0.18 0.26 -0.05 0.16 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.23 0.18 0.27 0.07 0.16 0.27 3 2 -0.57 0.18 0.23 0.00 0.15 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.34 0.22 0.29 0.34 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.24 0.18 0.23 1.06 0.15 0.24 4 2
CS 29491-109 50 4736 100 1.50 0.24 0.34 -2.90 0.15 0.19 1.82 0.12 0.22 5.30 0.20 0.27 -0.19 0.16 0.27 1 1 4.98 0.12 0.18 0.30 0.15 0.24 7 6 2.74 0.16 0.25 -0.83 0.17 0.30 1 1 3.71 0.11 0.20 0.25 0.15 0.26 9 8 0.25 0.17 0.22 -0.02 0.15 0.23 5 4 2.32 0.15 0.20 0.20 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.40 0.15 0.25 -0.37 0.15 0.29 3 3 1.77 0.15 0.21 -0.72 0.15 0.25 5 3 4.60 0.15 0.19 0.00 0.14 0.22 55 51 2.06 0.15 0.22 0.04 0.14 0.25 6 5 3.20 0.17 0.27 -0.15 0.17 0.31 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.31 0.21 0.31 -0.38 0.20 0.33 3 2 -1.19 0.18 0.23 -0.53 0.15 0.23 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.69 0.20 0.24 -0.92 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 29497-004 39 5013 100 2.23 0.24 0.34 -2.81 0.13 0.18 1.62 0.13 0.23 5.80 0.19 0.26 0.22 0.18 0.27 1 1 5.08 0.12 0.18 0.31 0.15 0.24 7 6 2.62 0.16 0.25 -1.04 0.17 0.26 1 1 3.83 0.12 0.20 0.28 0.15 0.25 9 6 0.41 0.18 0.22 0.05 0.15 0.24 5 4 2.42 0.16 0.21 0.21 0.14 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.51 0.18 0.26 -0.35 0.17 0.25 3 2 2.18 0.18 0.24 -0.40 0.16 0.24 5 3 4.69 0.13 0.18 0.00 0.14 0.22 55 42 2.35 0.16 0.22 0.24 0.15 0.24 6 5 3.48 0.19 0.29 0.05 0.18 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.73 0.15 0.22 0.57 0.15 0.24 3 2 0.08 0.18 0.23 0.66 0.16 0.24 6 4 0.73 0.18 0.22 0.94 0.15 0.24 3 1 0.53 0.13 0.19 1.21 0.15 0.22 2 1 -0.43 0.18 0.23 1.21 0.15 0.25 6 5 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.02 0.19 0.23 1.29 0.15 0.25 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.68 0.18 0.23 1.62 0.15 0.24 4 4
CS 29510-058 38 5108 100 2.32 0.24 0.34 -2.61 0.12 0.18 1.62 0.12 0.22 6.18 0.19 0.25 0.40 0.18 0.27 1 1 5.23 0.12 0.18 0.26 0.15 0.24 7 6 2.86 0.18 0.25 -1.00 0.18 0.27 1 1 4.04 0.11 0.20 0.29 0.15 0.25 9 7 0.48 0.18 0.23 -0.08 0.16 0.25 5 4 2.63 0.16 0.21 0.23 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.90 0.17 0.27 -0.16 0.17 0.26 3 3 2.26 0.16 0.22 -0.52 0.15 0.23 5 3 4.89 0.12 0.18 0.00 0.14 0.22 55 43 2.46 0.16 0.22 0.15 0.15 0.24 6 5 3.48 0.19 0.28 -0.16 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.53 0.17 0.25 0.17 0.16 0.26 3 2 -0.35 0.19 0.23 0.02 0.16 0.25 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.49 0.24 0.30 -0.01 0.21 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 30308-035 32 4806 100 1.78 0.27 0.37 -3.35 0.13 0.18 1.64 0.14 0.24 5.08 0.20 0.27 0.04 0.19 0.29 1 1 4.24 0.13 0.19 0.01 0.15 0.23 7 3 2.10 0.16 0.24 -1.01 0.17 0.26 1 1 3.12 0.12 0.20 0.12 0.15 0.25 9 1 -0.28 0.17 0.22 -0.09 0.16 0.24 5 2 1.67 0.16 0.21 0.00 0.15 0.23 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.78 0.16 0.22 -0.53 0.15 0.23 3 3 1.39 0.17 0.21 -0.64 0.15 0.23 5 3 4.15 0.13 0.18 0.00 0.14 0.22 55 28 1.73 0.16 0.22 0.17 0.15 0.24 6 1 3.15 0.21 0.29 0.26 0.20 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.19 0.23 0.31 -0.81 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 30315-001 37 4565 100 1.14 0.25 0.35 -2.98 0.11 0.17 1.99 0.12 0.22 4.93 0.22 0.28 -0.50 0.21 0.29 1 1 4.99 0.12 0.18 0.38 0.14 0.23 7 5 2.54 0.20 0.29 -0.97 0.22 0.30 1 1 3.65 0.11 0.20 0.25 0.14 0.24 9 7 0.28 0.17 0.22 0.08 0.16 0.25 5 4 2.21 0.16 0.21 0.16 0.16 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.08 0.16 0.25 -0.62 0.17 0.25 3 3 2.04 0.13 0.20 -0.39 0.15 0.23 5 3 4.53 0.11 0.17 0.00 0.14 0.22 55 51 2.13 0.15 0.22 0.18 0.16 0.25 6 5 3.40 0.20 0.30 0.12 0.20 0.29 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.32 0.17 0.24 0.32 0.17 0.26 3 2 -0.65 0.17 0.22 0.08 0.17 0.26 6 4 0.08 0.17 0.22 0.44 0.17 0.26 3 1 -1.66 0.19 0.24 -0.82 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 30315-029 38 4541 100 1.07 0.25 0.35 -3.33 0.12 0.18 2.06 0.13 0.23 4.63 0.21 0.28 -0.43 0.20 0.29 1 1 4.67 0.12 0.19 0.42 0.15 0.23 7 5 2.54 0.15 0.26 -0.59 0.18 0.29 1 1 3.33 0.12 0.20 0.30 0.15 0.25 9 4 -0.19 0.16 0.21 -0.03 0.15 0.23 5 4 1.87 0.15 0.20 0.18 0.15 0.23 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.82 0.15 0.22 -0.52 0.15 0.24 3 3 1.21 0.15 0.21 -0.85 0.15 0.23 5 3 4.17 0.12 0.18 0.00 0.14 0.22 55 41 1.67 0.14 0.21 0.08 0.15 0.24 6 4 2.72 0.18 0.27 -0.19 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.55 0.25 0.35 -0.19 0.22 0.33 3 2 -1.31 0.18 0.23 -0.21 0.16 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.79 0.24 0.32 0.42 0.22 0.30 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.10 0.18 0.23 0.72 0.16 0.25 4 3
CS 30337-097 44 4865 100 1.81 0.24 0.34 -2.73 0.13 0.18 1.88 0.12 0.22 5.64 0.20 0.26 -0.02 0.18 0.28 1 1 5.13 0.11 0.18 0.29 0.15 0.23 7 6 3.17 0.16 0.25 -0.57 0.17 0.27 1 1 3.79 0.12 0.20 0.17 0.15 0.25 9 7 0.51 0.17 0.22 0.07 0.15 0.24 5 4 2.40 0.15 0.20 0.11 0.14 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.58 0.16 0.25 -0.36 0.16 0.25 3 3 2.30 0.12 0.20 -0.36 0.14 0.23 5 3 4.77 0.13 0.18 0.00 0.14 0.22 55 49 2.27 0.13 0.21 0.09 0.14 0.24 6 6 3.35 0.18 0.28 -0.16 0.17 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.09 0.19 0.30 -0.15 0.18 0.29 3 2 -0.89 0.13 0.19 -0.39 0.15 0.23 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.32 0.20 0.25 -0.72 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 30339-041 37 5478 100 2.10 0.26 0.36 -2.20 0.12 0.18 2.23 0.13 0.23 5.77 0.19 0.26 -0.41 0.21 0.30 1 1 5.67 0.11 0.17 0.29 0.15 0.24 7 7 3.20 0.17 0.25 -1.07 0.18 0.27 1 1 4.48 0.12 0.20 0.33 0.15 0.25 9 8 1.12 0.18 0.23 0.15 0.16 0.24 5 4 3.11 0.16 0.21 0.29 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.12 0.17 0.24 -0.34 0.16 0.24 3 3 2.64 0.15 0.21 -0.54 0.16 0.23 5 3 5.29 0.12 0.18 0.00 0.14 0.22 55 47 2.78 0.15 0.21 0.07 0.16 0.25 6 5 4.00 0.18 0.26 -0.04 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.91 0.21 0.31 0.14 0.19 0.29 3 2 -0.11 0.18 0.23 -0.14 0.17 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.04 0.21 0.27 0.12 0.19 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 30343-063 40 4412 100 0.83 0.25 0.35 -2.95 0.12 0.18 2.26 0.11 0.21 4.75 0.22 0.28 -0.67 0.20 0.28 1 1 5.06 0.12 0.19 0.45 0.15 0.23 7 6 2.84 0.22 0.30 -0.66 0.21 0.29 1 1 3.63 0.11 0.20 0.24 0.14 0.24 9 8 0.19 0.16 0.21 -0.01 0.15 0.24 5 4 2.21 0.14 0.19 0.16 0.14 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.07 0.29 0.33 -0.63 0.25 0.30 3 3 1.78 0.20 0.24 -0.63 0.18 0.25 5 3 4.53 0.12 0.18 0.00 0.14 0.22 55 51 1.77 0.19 0.25 -0.17 0.17 0.26 6 5 3.45 0.08 0.38 0.17 0.15 0.37 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.05 0.21 0.28 -0.04 0.19 0.28 3 1 -0.79 0.18 0.22 -0.06 0.16 0.25 6 5 -0.11 0.17 0.22 0.27 0.16 0.25 3 1 -1.74 0.21 0.26 -0.90 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 31060-047 30 4749 100 1.55 0.26 0.36 -2.72 0.12 0.18 2.00 0.13 0.23 5.41 0.20 0.27 -0.26 0.20 0.29 1 1 5.11 0.12 0.18 0.25 0.15 0.23 7 5 2.64 0.23 0.30 -1.11 0.23 0.31 1 1 3.76 0.12 0.20 0.12 0.15 0.25 9 5 0.53 0.17 0.22 0.08 0.16 0.25 5 4 2.46 0.16 0.21 0.16 0.15 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.53 0.18 0.27 -0.42 0.17 0.26 3 3 2.42 0.15 0.20 -0.25 0.15 0.23 5 3 4.78 0.12 0.18 0.00 0.14 0.22 55 43 2.32 0.16 0.23 0.12 0.16 0.25 6 5 3.78 0.23 0.33 0.25 0.22 0.30 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.11 0.22 0.31 -0.13 0.20 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.61 0.19 0.23 -1.02 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 31062-041 37 4915 100 1.83 0.26 0.36 -2.67 0.14 0.19 1.84 0.13 0.23 6.20 0.20 0.26 0.49 0.19 0.29 1 1 5.23 0.12 0.19 0.33 0.16 0.25 5 5 2.94 0.16 0.25 -0.86 0.18 0.28 1 1 3.92 0.12 0.20 0.24 0.15 0.25 5 3 0.66 0.17 0.22 0.17 0.15 0.23 3 2 2.48 0.15 0.20 0.14 0.14 0.22 11 10 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 2.42 0.20 0.29 -0.57 0.19 0.28 1 1 2.08 0.15 0.22 -0.64 0.15 0.23 4 2 4.82 0.14 0.19 0.00 0.14 0.22 35 30 2.24 0.17 0.23 -0.00 0.15 0.25 4 4 3.49 0.21 0.30 -0.08 0.18 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 -0.10 0.23 0.33 -0.39 0.20 0.30 2 2 -0.95 0.19 0.24 -0.52 0.16 0.24 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.94 0.22 0.27 -0.39 0.18 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0
CS 31072-118 53 4606 100 1.25 0.24 0.34 -3.06 0.12 0.17 2.02 0.12 0.22 4.82 0.21 0.27 -0.50 0.19 0.28 1 1 4.84 0.12 0.19 0.33 0.14 0.23 7 6 2.59 0.14 0.25 -0.81 0.17 0.28 1 1 3.45 0.12 0.20 0.16 0.14 0.24 9 7 0.16 0.17 0.22 0.06 0.15 0.24 5 4 2.28 0.15 0.20 0.32 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.14 0.15 0.24 -0.47 0.15 0.25 3 3 1.62 0.14 0.22 -0.71 0.15 0.23 5 3 4.44 0.12 0.17 0.00 0.14 0.22 55 51 1.91 0.15 0.22 0.05 0.15 0.24 6 5 3.37 0.14 0.28 0.19 0.15 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.26 0.22 0.33 -0.17 0.20 0.32 3 2 -1.14 0.18 0.23 -0.32 0.16 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.97 0.18 0.22 -1.04 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
CS 31082-001 90 4922 100 1.90 0.23 0.33 -2.78 0.14 0.19 1.88 0.11 0.21 5.83 0.19 0.26 0.22 0.18 0.28 1 1 5.16 0.10 0.18 0.36 0.16 0.25 7 7 2.89 0.13 0.23 -0.80 0.15 0.26 1 1 3.91 0.11 0.20 0.33 0.15 0.25 9 8 0.51 0.17 0.23 0.12 0.14 0.23 5 5 2.49 0.15 0.20 0.25 0.14 0.22 17 16 1.24 0.15 0.19 0.02 0.15 0.23 3 2 2.53 0.15 0.23 -0.36 0.14 0.23 3 3 2.03 0.15 0.21 -0.58 0.14 0.23 5 3 4.72 0.14 0.19 0.00 0.14 0.22 55 54 2.32 0.15 0.22 0.18 0.14 0.24 6 6 3.60 0.16 0.27 0.13 0.15 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.72 0.15 0.22 0.53 0.14 0.24 3 2 0.02 0.18 0.23 0.56 0.15 0.23 6 6 0.71 0.17 0.22 0.89 0.14 0.23 3 2 0.53 0.14 0.19 1.18 0.14 0.22 2 2 -0.43 0.18 0.22 1.18 0.14 0.23 6 5 -0.14 0.18 0.24 1.06 0.15 0.25 10 8 0.02 0.18 0.23 1.30 0.15 0.23 9 9 -0.27 0.18 0.23 1.50 0.15 0.24 8 3 -0.61 0.18 0.22 1.66 0.15 0.23 4 4
HD 20 113 5445 100 2.39 0.22 0.32 -1.58 0.14 0.20 2.30 0.11 0.21 6.47 0.18 0.24 -0.34 0.17 0.27 1 1 6.17 0.11 0.18 0.17 0.15 0.24 7 6 4.07 0.12 0.23 -0.82 0.14 0.25 1 1 5.02 0.12 0.20 0.24 0.15 0.25 9 9 1.71 0.18 0.23 0.12 0.14 0.24 5 5 3.64 0.15 0.21 0.20 0.14 0.22 17 17 2.39 0.15 0.20 -0.03 0.14 0.23 3 3 3.87 0.17 0.26 -0.22 0.15 0.24 3 3 3.45 0.14 0.19 -0.36 0.14 0.23 5 5 5.92 0.14 0.20 0.00 0.14 0.22 55 54 3.42 0.15 0.22 0.08 0.14 0.24 6 6 4.58 0.18 0.28 -0.09 0.16 0.25 4 4 3.03 0.13 0.20 0.01 0.14 0.25 2 2 1.51 0.15 0.22 0.12 0.14 0.24 3 2 0.62 0.17 0.22 -0.04 0.14 0.23 6 6 1.40 0.17 0.22 0.38 0.14 0.24 3 2 0.86 0.15 0.20 0.31 0.13 0.23 2 2 -0.08 0.17 0.22 0.33 0.14 0.24 6 5 0.25 0.18 0.24 0.25 0.14 0.26 10 5 0.26 0.18 0.23 0.34 0.14 0.24 9 8 0.01 0.18 0.23 0.58 0.14 0.25 8 2 -0.27 0.18 0.23 0.80 0.14 0.24 4 4
HD 221170 51 4648 100 1.57 0.24 0.34 -2.14 0.15 0.20 2.22 0.11 0.21 5.68 0.22 0.27 -0.55 0.17 0.26 1 1 5.72 0.11 0.18 0.30 0.16 0.24 7 5 3.94 0.13 0.23 -0.37 0.16 0.26 1 1 4.48 0.12 0.21 0.27 0.15 0.25 9 9 1.24 0.17 0.22 0.22 0.14 0.23 5 5 3.10 0.16 0.22 0.24 0.14 0.23 17 17 1.93 0.17 0.21 0.08 0.14 0.22 3 3 3.29 0.22 0.30 -0.23 0.17 0.26 3 3 3.03 0.15 0.20 -0.20 0.14 0.23 5 5 5.35 0.15 0.20 0.00 0.14 0.22 55 53 3.05 0.18 0.27 0.29 0.15 0.25 6 6 3.94 0.19 0.29 -0.16 0.17 0.26 4 4 2.61 0.13 0.20 0.16 0.15 0.25 2 2 0.77 0.15 0.22 -0.05 0.15 0.24 3 1 0.04 0.18 0.23 -0.04 0.14 0.24 6 6 0.80 0.17 0.22 0.35 0.14 0.24 3 2 0.35 0.15 0.20 0.38 0.15 0.23 2 1 -0.60 0.17 0.22 0.39 0.14 0.24 6 5 -0.25 0.17 0.24 0.32 0.14 0.26 10 5 -0.16 0.18 0.23 0.49 0.14 0.24 9 7 -0.47 0.18 0.23 0.67 0.14 0.24 8 1 -0.80 0.17 0.22 0.85 0.14 0.24 4 4
HE 0005-0002 67 4726 100 1.58 0.25 0.35 -3.09 0.11 0.17 1.82 0.11 0.21 5.50 0.20 0.27 0.17 0.20 0.29 1 1 4.93 0.11 0.18 0.42 0.15 0.23 7 7 2.97 0.15 0.26 -0.43 0.18 0.27 1 1 3.65 0.11 0.20 0.36 0.14 0.24 9 8 0.20 0.17 0.22 0.09 0.16 0.25 5 4 2.13 0.16 0.21 0.18 0.16 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.92 0.16 0.22 -0.68 0.16 0.24 3 3 2.00 0.16 0.35 -0.33 0.24 0.37 5 3 4.44 0.11 0.17 0.00 0.14 0.22 55 53 2.03 0.15 0.22 0.17 0.16 0.25 6 6 3.26 0.18 0.28 0.08 0.18 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.10 0.18 0.27 0.19 0.18 0.28 3 2 -0.78 0.18 0.23 0.04 0.17 0.26 6 6 -0.02 0.18 0.22 0.45 0.17 0.26 3 2 -0.91 0.21 0.28 0.02 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0008-3842 67 4327 100 0.65 0.23 0.33 -3.35 0.11 0.18 2.39 0.12 0.22 4.17 0.21 0.28 -0.89 0.22 0.30 1 1 4.58 0.13 0.19 0.33 0.15 0.24 7 5 2.30 0.17 0.26 -0.84 0.19 0.27 1 1 2.98 0.12 0.20 -0.05 0.15 0.26 9 6 -0.15 0.15 0.20 0.01 0.15 0.24 5 4 1.66 0.15 0.20 -0.03 0.15 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.64 0.19 0.25 -0.70 0.19 0.26 3 3 1.22 0.11 0.24 -0.84 0.14 0.24 5 3 4.17 0.11 0.18 0.00 0.14 0.22 55 52 1.53 0.17 0.23 -0.06 0.18 0.26 6 6 2.75 0.27 0.32 -0.16 0.26 0.31 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.86 0.18 0.26 -1.50 0.18 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.95 0.18 0.22 -1.75 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0017-4838 42 5149 100 2.23 0.29 0.39 -3.23 0.13 0.18 1.81 0.14 0.24 4.87 0.25 0.31 -0.29 0.24 0.33 1 1 4.60 0.12 0.19 0.25 0.16 0.24 7 3 2.35 0.16 0.23 -0.89 0.17 0.26 1 1 3.40 0.12 0.20 0.27 0.15 0.25 9 3 0.17 0.18 0.23 0.23 0.16 0.25 5 3 2.15 0.17 0.22 0.36 0.15 0.24 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.06 0.16 0.21 -0.37 0.15 0.23 3 3 1.58 0.17 0.21 -0.58 0.16 0.23 5 3 4.27 0.13 0.18 0.00 0.14 0.22 55 34 2.01 0.15 0.22 0.32 0.15 0.25 6 4 3.18 0.18 0.24 0.17 0.17 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.42 0.22 0.31 0.68 0.20 0.30 3 2 -0.65 0.19 0.24 0.34 0.17 0.25 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.88 0.20 0.24 -0.78 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0018-1349 35 5719 100 4.62 0.26 0.36 -2.26 0.12 0.18 1.73 0.20 0.30 6.49 0.18 0.24 0.36 0.17 0.26 1 1 5.62 0.11 0.17 0.30 0.15 0.24 7 2 3.25 0.15 0.23 -0.95 0.17 0.26 1 1 4.32 0.12 0.20 0.23 0.14 0.25 9 6 0.95 0.18 0.23 0.05 0.18 0.28 5 2 2.96 0.15 0.20 0.21 0.16 0.26 17 7 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.32 0.15 0.22 -0.09 0.16 0.24 3 3 2.85 0.16 0.22 -0.28 0.17 0.25 5 3 5.23 0.12 0.18 0.00 0.14 0.22 55 38 2.90 0.16 0.22 0.25 0.16 0.26 6 3 4.00 0.17 0.24 0.01 0.18 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.65 0.18 0.25 -0.06 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.34 0.20 0.24 0.47 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0023-4825 42 5816 100 3.63 0.26 0.36 -2.06 0.12 0.18 1.45 0.14 0.24 6.64 0.17 0.23 0.31 0.17 0.26 1 1 5.74 0.11 0.17 0.22 0.15 0.23 7 4 3.40 0.16 0.24 -1.01 0.18 0.27 1 1 4.56 0.12 0.20 0.26 0.15 0.24 9 7 1.14 0.18 0.23 0.03 0.16 0.26 5 4 3.27 0.15 0.20 0.31 0.15 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.61 0.16 0.24 -0.00 0.16 0.25 3 3 2.88 0.16 0.21 -0.45 0.16 0.24 5 3 5.44 0.12 0.18 0.00 0.14 0.22 55 47 2.98 0.15 0.22 0.12 0.15 0.25 6 4 4.19 0.20 0.27 -0.01 0.19 0.27 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.89 0.19 0.27 -0.02 0.18 0.28 3 2 0.13 0.19 0.23 -0.05 0.17 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.01 0.22 0.27 -0.06 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0029-1839 70 5010 100 2.19 0.24 0.34 -2.50 0.12 0.18 1.67 0.12 0.22 6.21 0.19 0.25 0.31 0.18 0.27 1 1 5.08 0.12 0.18 -0.00 0.15 0.23 7 7 2.97 0.15 0.26 -1.00 0.17 0.27 1 1 3.97 0.12 0.20 0.11 0.14 0.24 9 7 0.28 0.17 0.22 -0.39 0.15 0.25 5 4 2.39 0.16 0.21 -0.13 0.15 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.04 0.16 0.27 -0.13 0.16 0.26 3 3 2.02 0.16 0.22 -0.87 0.15 0.23 5 3 5.00 0.12 0.18 0.00 0.14 0.22 55 53 2.39 0.16 0.22 -0.03 0.15 0.24 6 6 3.28 0.18 0.26 -0.47 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.50 0.16 0.25 0.03 0.16 0.25 3 2 -0.64 0.18 0.23 -0.38 0.16 0.25 6 3 0.23 0.18 0.22 0.13 0.16 0.25 3 1 -1.67 0.19 0.23 -1.30 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0037-2657 69 4982 100 2.21 0.26 0.36 -3.22 0.13 0.18 1.80 0.12 0.22 5.48 0.19 0.26 0.31 0.17 0.27 1 1 4.63 0.12 0.18 0.27 0.15 0.23 7 5 2.41 0.14 0.23 -0.84 0.15 0.25 1 1 3.46 0.12 0.20 0.32 0.15 0.25 9 7 0.08 0.18 0.23 0.13 0.16 0.24 5 4 2.02 0.16 0.21 0.22 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.06 0.16 0.22 -0.38 0.15 0.23 3 3 1.48 0.16 0.21 -0.69 0.15 0.23 5 3 4.28 0.13 0.18 0.00 0.14 0.22 55 44 1.94 0.16 0.22 0.24 0.15 0.24 6 5 3.00 0.16 0.23 -0.03 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.89 0.21 0.30 -0.64 0.19 0.29 3 2 -1.50 0.19 0.23 -0.52 0.16 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.18 0.19 0.23 -1.09 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0039-4154 70 4735 100 1.55 0.25 0.35 -3.38 0.11 0.17 2.01 0.12 0.22 4.89 0.20 0.27 -0.14 0.20 0.29 1 1 4.77 0.12 0.18 0.55 0.15 0.23 7 7 2.67 0.13 0.23 -0.44 0.15 0.26 1 1 3.23 0.11 0.20 0.23 0.15 0.25 9 7 0.04 0.17 0.22 0.23 0.16 0.25 5 4 1.79 0.16 0.21 0.13 0.15 0.24 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.70 0.15 0.21 -0.61 0.15 0.23 3 3 1.11 0.19 0.23 -0.92 0.18 0.26 5 3 4.14 0.11 0.17 0.00 0.14 0.22 55 47 1.87 0.16 0.22 0.31 0.16 0.25 6 6 2.84 0.16 0.23 -0.06 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.63 0.21 0.32 -0.24 0.20 0.31 3 2 -1.49 0.18 0.23 -0.38 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.18 0.19 0.26 0.05 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0043-2845 66 5517 100 4.42 0.25 0.35 -2.91 0.13 0.18 1.17 0.16 0.26 5.68 0.19 0.25 0.19 0.17 0.26 1 1 4.97 0.12 0.18 0.29 0.15 0.23 7 2 2.73 0.14 0.22 -0.83 0.16 0.25 1 1 3.65 0.12 0.20 0.20 0.14 0.24 9 6 0.33 0.18 0.23 0.06 0.16 0.26 5 2 2.36 0.16 0.21 0.24 0.15 0.25 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.66 0.14 0.20 -0.10 0.15 0.23 3 3 1.79 0.17 0.21 -0.70 0.15 0.24 5 3 4.59 0.13 0.18 0.00 0.14 0.22 55 37 2.37 0.16 0.22 0.36 0.15 0.25 6 4 3.35 0.16 0.21 0.00 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.71 0.19 0.25 -0.77 0.17 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0044-2459 62 5242 100 2.92 0.26 0.36 -3.28 0.13 0.18 1.55 0.14 0.24 5.56 0.19 0.26 0.45 0.18 0.27 1 1 4.65 0.11 0.20 0.34 0.17 0.26 7 4 2.30 0.14 0.22 -0.89 0.15 0.25 1 1 3.35 0.11 0.20 0.27 0.15 0.25 9 3 0.11 0.18 0.23 0.22 0.16 0.25 5 2 2.07 0.16 0.21 0.33 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.91 0.16 0.20 -0.48 0.15 0.23 3 3 1.12 0.17 0.21 -0.99 0.16 0.24 5 3 4.22 0.13 0.18 0.00 0.14 0.22 55 37 1.95 0.15 0.22 0.31 0.15 0.24 6 4 2.93 0.15 0.21 -0.04 0.15 0.22 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.96 0.19 0.25 -1.65 0.17 0.27 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0044-4023 39 5694 100 3.26 0.26 0.36 -2.56 0.13 0.18 1.49 0.14 0.24 6.23 0.18 0.24 0.40 0.17 0.27 1 1 5.26 0.12 0.18 0.24 0.15 0.23 7 2 2.86 0.15 0.23 -1.05 0.17 0.26 1 1 4.02 0.12 0.20 0.22 0.15 0.25 9 4 0.44 0.18 0.23 -0.17 0.16 0.25 5 2 2.63 0.14 0.20 0.17 0.15 0.23 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.88 0.17 0.22 -0.23 0.16 0.23 3 3 2.17 0.16 0.20 -0.66 0.15 0.23 5 3 4.94 0.13 0.18 0.00 0.14 0.22 55 37 2.50 0.16 0.22 0.14 0.15 0.25 6 3 3.54 0.22 0.26 -0.15 0.19 0.26 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.34 0.24 0.33 -0.06 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.78 0.20 0.24 -0.35 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0045-2430 59 5377 100 3.25 0.24 0.34 -1.77 0.12 0.18 1.67 0.12 0.22 6.54 0.18 0.24 -0.09 0.16 0.25 1 1 5.77 0.11 0.18 -0.04 0.14 0.23 7 6 3.61 0.14 0.23 -1.09 0.16 0.26 1 1 4.68 0.11 0.20 0.09 0.14 0.24 9 9 1.30 0.17 0.22 -0.10 0.16 0.26 5 5 3.29 0.16 0.21 0.04 0.15 0.25 17 17 2.16 0.16 0.20 -0.07 0.15 0.24 3 3 3.82 0.14 0.24 -0.09 0.16 0.24 3 3 3.37 0.14 0.19 -0.25 0.14 0.23 5 5 5.73 0.12 0.18 0.00 0.14 0.22 55 52 3.00 0.15 0.22 -0.15 0.15 0.25 6 6 4.00 0.17 0.26 -0.48 0.18 0.26 4 4 2.81 0.14 0.21 -0.02 0.14 0.26 2 1 0.46 0.20 0.30 -0.75 0.20 0.30 3 2 -0.13 0.18 0.23 -0.61 0.16 0.27 6 3 0.93 0.18 0.23 0.10 0.16 0.27 3 1 0.03 0.21 0.27 -0.34 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.93 0.18 0.23 0.33 0.15 0.27 4 3
HE 0049-5700 42 5952 100 4.08 0.26 0.36 -2.41 0.12 0.18 1.63 0.15 0.25 6.38 0.18 0.24 0.39 0.17 0.26 1 1 5.55 0.12 0.18 0.37 0.15 0.23 7 4 3.09 0.15 0.22 -0.98 0.16 0.25 1 1 4.33 0.12 0.20 0.37 0.14 0.25 9 7 0.89 0.18 0.23 0.12 0.16 0.26 5 2 2.95 0.16 0.21 0.33 0.15 0.24 17 7 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.08 0.15 0.21 -0.19 0.15 0.23 3 3 2.34 0.16 0.20 -0.66 0.15 0.24 5 3 5.10 0.12 0.18 0.00 0.14 0.22 55 37 2.59 0.16 0.22 0.07 0.16 0.25 6 1 3.62 0.12 0.18 -0.23 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.66 0.20 0.29 0.08 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.69 0.19 0.24 -0.42 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0051-2304 47 4537 100 1.22 0.25 0.35 -2.41 0.12 0.19 1.97 0.13 0.23 5.31 0.20 0.26 -0.64 0.20 0.28 1 1 5.45 0.11 0.19 0.30 0.15 0.24 7 5 3.33 0.17 0.26 -0.70 0.18 0.27 1 1 4.12 0.12 0.21 0.20 0.15 0.25 9 8 0.80 0.18 0.24 0.07 0.17 0.26 5 5 2.77 0.17 0.23 0.18 0.16 0.24 17 17 1.39 0.17 0.21 -0.18 0.17 0.24 3 3 2.72 0.48 0.56 -0.51 0.43 0.52 3 3 2.43 0.17 0.22 -0.52 0.17 0.24 5 5 5.06 0.12 0.19 0.00 0.14 0.22 55 53 2.42 0.20 0.27 -0.07 0.19 0.27 6 6 3.63 0.24 0.34 -0.18 0.22 0.30 4 4 2.32 0.13 0.20 0.16 0.15 0.26 2 2 0.46 0.17 0.23 -0.07 0.17 0.25 3 1 -0.40 0.18 0.23 -0.20 0.16 0.26 6 6 0.35 0.17 0.22 0.19 0.16 0.26 3 2 -0.37 0.23 0.31 -0.07 0.20 0.29 2 1 -1.37 0.17 0.22 -0.10 0.16 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -1.00 0.18 0.23 -0.07 0.17 0.27 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.75 0.18 0.22 0.17 0.16 0.27 4 4
HE 0054-0657 32 5908 100 4.40 0.26 0.36 -2.00 0.11 0.18 1.56 0.18 0.28 6.68 0.17 0.23 0.29 0.17 0.26 1 1 5.81 0.11 0.17 0.23 0.15 0.24 7 3 3.67 0.15 0.24 -0.80 0.18 0.27 1 1 4.47 0.12 0.20 0.10 0.15 0.25 9 7 1.06 0.18 0.23 -0.11 0.18 0.28 5 2 3.17 0.16 0.21 0.15 0.17 0.26 17 7 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.69 0.16 0.24 0.01 0.17 0.25 3 3 3.00 0.15 0.21 -0.39 0.16 0.24 5 3 5.50 0.11 0.18 0.00 0.14 0.22 55 39 3.13 0.16 0.22 0.21 0.17 0.26 6 3 4.32 0.17 0.25 0.07 0.18 0.26 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.92 0.19 0.27 -0.05 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.05 0.20 0.25 -0.08 0.21 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0057-4541 75 5083 100 2.55 0.24 0.34 -2.32 0.11 0.18 1.67 0.12 0.22 6.26 0.21 0.26 0.17 0.19 0.27 1 1 5.53 0.12 0.18 0.25 0.14 0.23 7 5 3.31 0.13 0.24 -0.85 0.16 0.25 1 1 4.30 0.11 0.20 0.24 0.14 0.24 9 9 0.93 0.18 0.23 0.07 0.16 0.26 5 5 2.87 0.16 0.21 0.16 0.15 0.24 17 17 1.66 0.16 0.20 -0.03 0.15 0.24 3 3 3.08 0.17 0.26 -0.28 0.17 0.25 3 3 2.75 0.15 0.20 -0.33 0.15 0.23 5 5 5.19 0.11 0.18 0.00 0.14 0.22 55 53 2.70 0.16 0.23 0.09 0.16 0.25 6 6 3.77 0.16 0.26 -0.17 0.17 0.25 4 4 2.43 0.14 0.21 0.14 0.14 0.26 2 1 0.72 0.14 0.23 0.06 0.15 0.24 3 2 -0.14 0.19 0.24 -0.07 0.16 0.27 6 6 0.64 0.18 0.22 0.35 0.15 0.26 3 2 -0.29 0.20 0.28 -0.11 0.19 0.28 2 1 -0.91 0.18 0.23 0.22 0.15 0.27 6 4 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.53 0.18 0.23 0.28 0.16 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.17 0.18 0.23 0.62 0.15 0.27 4 4
HE 0104-4007 48 5154 100 2.64 0.26 0.36 -3.30 0.13 0.18 1.72 0.14 0.24 5.59 0.19 0.26 0.50 0.18 0.28 1 1 4.49 0.11 0.20 0.21 0.16 0.25 7 3 2.14 0.15 0.22 -1.03 0.16 0.25 1 1 3.41 0.12 0.20 0.36 0.15 0.25 9 3 0.17 0.18 0.23 0.31 0.16 0.24 5 4 2.11 0.15 0.21 0.40 0.15 0.23 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.93 0.16 0.21 -0.44 0.15 0.23 3 2 1.43 0.17 0.21 -0.66 0.15 0.23 5 3 4.20 0.13 0.18 0.00 0.14 0.22 55 35 2.02 0.16 0.22 0.40 0.15 0.24 6 4 3.02 0.17 0.23 0.07 0.16 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.31 0.20 0.26 -0.98 0.17 0.27 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.81 0.19 0.24 -0.64 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0104-5300 52 4732 100 1.43 0.27 0.37 -3.42 0.11 0.19 1.99 0.13 0.23 5.07 0.20 0.28 -0.01 0.27 0.34 1 1 4.52 0.13 0.19 0.25 0.19 0.27 7 5 2.31 0.16 0.24 -0.85 0.21 0.29 1 1 3.27 0.12 0.20 0.22 0.18 0.27 9 4 -0.20 0.17 0.22 -0.06 0.23 0.31 5 4 1.90 0.16 0.21 0.18 0.21 0.29 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.83 0.16 0.22 -0.53 0.21 0.27 3 3 1.13 0.16 0.21 -0.95 0.22 0.29 5 3 4.19 0.11 0.19 0.00 0.14 0.22 55 42 1.74 0.16 0.22 0.12 0.22 0.30 6 5 3.07 0.18 0.26 0.13 0.22 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.93 0.20 0.30 -0.60 0.24 0.32 3 2 -1.32 0.18 0.23 -0.25 0.23 0.31 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.70 0.19 0.23 -1.52 0.25 0.33 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0105-6141 66 5218 100 2.83 0.24 0.34 -2.55 0.13 0.18 1.66 0.13 0.23 6.04 0.20 0.25 0.20 0.17 0.26 1 1 5.36 0.12 0.18 0.33 0.15 0.23 7 7 3.26 0.14 0.24 -0.67 0.16 0.26 1 1 4.14 0.12 0.20 0.33 0.14 0.24 9 8 0.83 0.18 0.23 0.20 0.16 0.25 5 4 2.78 0.16 0.22 0.31 0.15 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.91 0.17 0.25 -0.22 0.16 0.25 3 3 2.34 0.16 0.22 -0.50 0.16 0.23 5 3 4.95 0.13 0.18 0.00 0.14 0.22 55 52 2.55 0.16 0.22 0.18 0.15 0.24 6 6 3.62 0.17 0.26 -0.08 0.17 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.40 0.18 0.27 -0.03 0.17 0.28 3 2 -0.49 0.19 0.24 -0.18 0.16 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.24 0.21 0.27 0.17 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.36 0.18 0.23 0.68 0.16 0.26 4 3
HE 0109-0742 44 5315 100 1.85 0.26 0.36 -2.53 0.12 0.18 2.19 0.13 0.23 5.72 0.19 0.26 -0.14 0.20 0.30 1 1 5.36 0.12 0.18 0.30 0.15 0.23 7 5 3.01 0.17 0.25 -0.94 0.18 0.27 1 1 4.07 0.12 0.20 0.23 0.15 0.25 9 8 0.68 0.18 0.23 0.03 0.16 0.24 5 4 2.71 0.29 0.37 0.21 0.25 0.35 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.90 0.17 0.24 -0.24 0.16 0.24 3 3 2.23 0.15 0.20 -0.64 0.15 0.23 5 3 4.98 0.12 0.18 0.00 0.14 0.22 55 47 2.52 0.15 0.21 0.12 0.15 0.25 6 5 3.58 0.18 0.24 -0.15 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.42 0.23 0.32 -0.03 0.21 0.30 3 2 -0.67 0.18 0.23 -0.39 0.17 0.25 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.56 0.22 0.28 -0.16 0.20 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0109-3711 17 6156 100 3.91 0.30 0.40 -1.91 0.13 0.18 1.60 0.18 0.28 6.79 0.18 0.26 0.31 0.20 0.29 1 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 4.87 0.12 0.20 0.42 0.15 0.25 9 1 1.38 0.18 0.23 0.12 0.17 0.26 5 1 3.49 0.16 0.22 0.38 0.16 0.24 17 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.70 0.20 0.26 -0.06 0.19 0.26 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 5.59 0.13 0.18 0.00 0.14 0.22 55 14 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0111-1454 82 4632 100 1.05 0.24 0.34 -2.99 0.13 0.18 2.36 0.11 0.21 5.18 0.20 0.27 -0.22 0.19 0.28 1 1 4.94 0.12 0.18 0.35 0.15 0.23 7 6 2.94 0.13 0.24 -0.54 0.17 0.27 1 1 3.53 0.12 0.20 0.16 0.15 0.25 9 8 0.21 0.16 0.21 0.04 0.15 0.23 5 5 2.26 0.14 0.19 0.24 0.14 0.22 17 17 1.03 0.15 0.19 0.02 0.15 0.23 3 2 2.40 0.12 0.22 -0.27 0.14 0.24 3 3 2.19 0.13 0.20 -0.21 0.14 0.23 5 5 4.51 0.13 0.18 0.00 0.14 0.22 55 54 2.06 0.14 0.22 0.14 0.15 0.24 6 6 3.40 0.14 0.26 0.14 0.15 0.26 4 4 2.29 0.13 0.20 0.68 0.14 0.24 2 2 -0.15 0.20 0.31 -0.13 0.19 0.30 3 1 -1.07 0.18 0.22 -0.31 0.15 0.24 6 4 -0.22 0.18 0.22 0.17 0.15 0.24 3 1 -1.56 0.18 0.23 -0.69 0.16 0.23 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.54 0.18 0.23 -0.06 0.15 0.24 4 1
HE 0121-2826 46 4955 100 1.99 0.26 0.36 -2.97 0.12 0.18 1.68 0.12 0.22 5.97 0.20 0.27 0.54 0.19 0.28 1 1 5.04 0.11 0.19 0.43 0.15 0.24 7 6 2.64 0.16 0.25 -0.87 0.18 0.27 1 1 3.75 0.12 0.20 0.36 0.15 0.25 9 8 0.24 0.18 0.23 0.04 0.16 0.25 5 4 2.31 0.16 0.21 0.25 0.15 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.44 0.16 0.24 -0.26 0.16 0.24 3 3 1.73 0.16 0.22 -0.70 0.16 0.23 5 3 4.53 0.12 0.18 0.00 0.14 0.22 55 45 2.15 0.16 0.22 0.19 0.15 0.25 6 6 3.13 0.17 0.25 -0.16 0.17 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.27 0.18 0.27 0.27 0.17 0.27 3 2 -0.66 0.19 0.23 0.06 0.17 0.25 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.39 0.20 0.24 -0.56 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0131-2740 28 5351 100 3.03 0.28 0.38 -3.08 0.13 0.18 1.62 0.15 0.25 5.66 0.19 0.26 0.35 0.18 0.27 1 1 4.87 0.12 0.19 0.37 0.16 0.25 7 3 2.70 0.18 0.24 -0.69 0.18 0.27 1 1 3.61 0.12 0.20 0.33 0.15 0.25 9 1 0.26 0.18 0.23 0.16 0.17 0.25 5 1 2.21 0.15 0.21 0.27 0.15 0.24 17 4 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.31 0.17 0.22 -0.28 0.15 0.23 3 3 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.42 0.13 0.18 0.00 0.14 0.22 55 19 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.27 0.19 0.24 0.10 0.18 0.25 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0131-3953 52 5928 100 3.83 0.29 0.39 -2.71 0.11 0.17 1.06 0.15 0.25 8.16 0.16 0.24 2.45 0.18 0.27 1 1 5.21 0.12 0.18 0.30 0.15 0.24 5 2 2.84 0.14 0.21 -0.96 0.16 0.26 1 1 4.05 0.12 0.20 0.37 0.15 0.25 5 3 1.08 0.19 0.24 0.59 0.19 0.27 3 1 2.47 0.16 0.22 0.13 0.17 0.26 11 5 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 2.78 0.16 0.21 -0.21 0.17 0.24 1 1 2.18 0.16 0.20 -0.53 0.17 0.25 4 2 4.82 0.11 0.17 0.00 0.14 0.22 35 22 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 3.29 0.16 0.20 -0.28 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 0.75 0.18 0.27 0.46 0.18 0.28 2 2 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.66 0.13 0.18 2.20 0.16 0.23 2 2 0.43 0.18 0.23 1.94 0.19 0.27 3 2 0.83 0.19 0.26 1.93 0.19 0.29 7 1 0.58 0.19 0.24 1.76 0.20 0.28 5 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -0.55 0.19 0.24 1.62 0.19 0.28 3 2
HE 0143-1135 43 5629 100 4.53 0.24 0.34 -2.13 0.12 0.18 1.42 0.16 0.26 6.49 0.19 0.24 0.23 0.17 0.26 1 1 5.78 0.12 0.18 0.33 0.14 0.24 7 4 3.70 0.12 0.23 -0.64 0.15 0.25 1 1 4.49 0.13 0.21 0.26 0.14 0.25 9 8 1.21 0.17 0.22 0.17 0.17 0.28 5 4 3.12 0.16 0.21 0.24 0.16 0.26 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.51 0.13 0.21 -0.02 0.15 0.23 3 3 3.07 0.15 0.20 -0.19 0.16 0.24 5 3 5.37 0.12 0.18 0.00 0.14 0.22 55 46 2.92 0.16 0.22 0.13 0.16 0.26 6 4 4.03 0.15 0.22 -0.09 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.64 0.15 0.22 -0.20 0.16 0.26 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.08 0.20 0.24 -0.07 0.19 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0143-4108 70 5121 100 2.41 0.24 0.34 -2.62 0.12 0.18 1.51 0.12 0.22 5.93 0.18 0.25 0.16 0.18 0.27 1 1 4.98 0.10 0.18 0.02 0.15 0.24 7 7 2.75 0.15 0.23 -1.10 0.16 0.26 1 1 3.75 0.12 0.20 0.00 0.14 0.25 9 8 0.45 0.17 0.22 -0.10 0.15 0.25 5 3 2.69 0.16 0.21 0.28 0.15 0.23 17 15 1.52 0.15 0.20 0.14 0.15 0.24 3 2 2.95 0.17 0.27 -0.10 0.16 0.26 3 3 2.83 0.13 0.19 0.06 0.14 0.23 5 4 4.88 0.12 0.18 0.00 0.14 0.22 55 54 2.51 0.16 0.22 0.21 0.15 0.24 6 6 3.87 0.16 0.28 0.23 0.17 0.27 4 4 2.72 0.13 0.20 0.74 0.14 0.25 2 2 -0.59 0.22 0.31 -0.94 0.20 0.30 3 2 -1.30 0.18 0.23 -0.92 0.16 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -1.67 0.19 0.23 -1.18 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0143-4146 45 4799 100 1.50 0.26 0.36 -2.94 0.13 0.18 2.03 0.13 0.23 5.55 0.20 0.27 0.11 0.19 0.28 1 1 5.04 0.12 0.19 0.41 0.15 0.23 7 7 2.92 0.19 0.29 -0.61 0.21 0.30 1 1 3.67 0.12 0.20 0.25 0.15 0.25 9 7 0.60 0.18 0.23 0.38 0.16 0.25 5 5 2.43 0.16 0.21 0.36 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.52 0.17 0.26 -0.20 0.16 0.26 3 3 2.31 0.14 0.22 -0.13 0.15 0.24 5 3 4.55 0.13 0.18 0.00 0.14 0.22 55 49 2.26 0.16 0.22 0.28 0.15 0.24 6 6 3.34 0.20 0.29 0.03 0.19 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.60 0.23 0.34 -0.62 0.22 0.32 3 2 -1.37 0.19 0.23 -0.66 0.17 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.61 0.19 0.24 -0.79 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0157-3335 81 4775 100 1.62 0.24 0.34 -3.08 0.14 0.19 1.86 0.12 0.22 5.09 0.20 0.27 -0.22 0.18 0.29 1 1 4.90 0.11 0.18 0.40 0.16 0.24 7 7 2.85 0.14 0.25 -0.54 0.16 0.27 1 1 3.50 0.12 0.20 0.22 0.15 0.25 9 8 0.17 0.17 0.22 0.08 0.14 0.23 5 3 2.21 0.16 0.21 0.27 0.14 0.22 17 16 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.15 0.15 0.23 -0.44 0.14 0.23 3 3 1.40 0.16 0.21 -0.91 0.15 0.23 5 3 4.42 0.14 0.19 0.00 0.14 0.22 55 52 2.00 0.15 0.22 0.17 0.15 0.24 6 6 3.21 0.15 0.26 0.04 0.16 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.06 0.19 0.30 0.06 0.18 0.29 3 2 -0.96 0.17 0.21 -0.12 0.15 0.23 6 3 -0.16 0.18 0.22 0.33 0.15 0.24 3 1 -1.36 0.20 0.25 -0.41 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0200-0955 39 5216 100 2.57 0.26 0.36 -2.46 0.13 0.19 1.79 0.14 0.24 6.34 0.19 0.26 0.41 0.18 0.27 1 1 5.45 0.11 0.18 0.34 0.16 0.24 7 6 3.07 0.17 0.26 -0.93 0.18 0.27 1 1 4.19 0.12 0.20 0.30 0.15 0.25 9 8 0.75 0.14 0.20 0.04 0.15 0.23 5 4 2.73 0.16 0.21 0.17 0.15 0.23 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.02 0.19 0.27 -0.19 0.17 0.26 3 3 2.56 0.16 0.22 -0.36 0.16 0.23 5 3 5.03 0.13 0.19 0.00 0.14 0.22 55 48 2.62 0.16 0.23 0.16 0.15 0.24 6 5 3.58 0.20 0.27 -0.20 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.14 0.24 0.33 -0.36 0.22 0.31 3 2 -0.54 0.19 0.24 -0.32 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.02 0.21 0.25 -0.68 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0202-2204 82 5280 100 1.65 0.22 0.32 -1.98 0.14 0.19 2.47 0.12 0.22 7.57 0.17 0.24 1.16 0.17 0.28 1 1 5.59 0.13 0.19 -0.01 0.15 0.23 5 3 3.94 0.14 0.25 -0.55 0.16 0.27 1 1 4.64 0.12 0.20 0.26 0.15 0.25 5 5 1.15 0.16 0.22 -0.04 0.14 0.23 3 3 2.98 0.16 0.21 -0.06 0.14 0.22 11 10 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.29 0.18 0.27 -0.40 0.16 0.25 1 1 3.08 0.13 0.19 -0.33 0.15 0.23 4 4 5.52 0.14 0.19 0.00 0.14 0.22 35 34 2.97 0.14 0.21 0.03 0.15 0.24 4 4 4.31 0.19 0.28 0.04 0.16 0.25 4 4 2.65 0.17 0.23 0.03 0.16 0.26 1 1 1.56 0.16 0.23 0.57 0.15 0.24 2 1 0.67 0.18 0.24 0.41 0.15 0.23 4 4 1.09 0.17 0.22 0.47 0.15 0.23 2 1 1.55 0.16 0.20 1.41 0.14 0.22 2 2 0.55 0.18 0.30 1.36 0.25 0.34 3 3 0.90 0.20 0.27 1.30 0.16 0.26 7 7 0.54 0.18 0.23 1.02 0.15 0.23 5 5 0.06 0.18 0.23 1.03 0.15 0.24 6 4 -0.98 0.18 0.22 0.49 0.15 0.24 3 3
HE 0231-4016 39 5972 100 3.59 0.28 0.38 -2.08 0.13 0.18 1.67 0.15 0.25 7.67 0.16 0.23 1.36 0.17 0.27 1 1 5.72 0.11 0.17 0.22 0.15 0.24 7 4 3.30 0.17 0.24 -1.09 0.18 0.26 1 1 4.64 0.12 0.20 0.36 0.15 0.25 9 8 1.08 0.18 0.23 -0.01 0.17 0.25 5 3 3.19 0.16 0.22 0.25 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.48 0.17 0.24 -0.11 0.16 0.24 3 3 3.03 0.16 0.20 -0.28 0.16 0.23 5 3 5.42 0.13 0.18 0.00 0.14 0.22 55 42 2.72 0.16 0.22 -0.12 0.16 0.25 6 2 4.03 0.16 0.22 -0.14 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.56 0.15 0.23 0.67 0.16 0.25 3 2 0.88 0.16 0.22 0.72 0.16 0.23 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.52 0.16 0.21 1.47 0.16 0.23 2 2 0.31 0.23 0.27 1.22 0.20 0.28 6 3 1.03 0.18 0.25 1.53 0.17 0.27 10 1 0.77 0.19 0.24 1.35 0.17 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0240-0807 50 4729 100 1.54 0.24 0.34 -2.68 0.11 0.18 1.96 0.12 0.22 5.37 0.20 0.26 -0.35 0.20 0.29 1 1 5.20 0.12 0.18 0.30 0.15 0.23 7 6 3.05 0.16 0.26 -0.75 0.18 0.27 1 1 3.83 0.12 0.20 0.15 0.14 0.25 9 8 0.62 0.18 0.23 0.13 0.16 0.26 5 5 2.71 0.22 0.35 0.36 0.29 0.37 17 17 1.27 0.16 0.20 -0.06 0.16 0.24 3 2 2.64 0.18 0.28 -0.35 0.18 0.26 3 3 2.20 0.15 0.21 -0.51 0.16 0.24 5 3 4.82 0.11 0.18 0.00 0.14 0.22 55 51 2.27 0.15 0.23 0.03 0.16 0.25 6 5 3.92 0.20 0.32 0.35 0.20 0.29 4 4 2.17 0.14 0.21 0.24 0.15 0.26 2 1 0.20 0.21 0.30 -0.10 0.20 0.29 3 1 -0.56 0.17 0.22 -0.13 0.16 0.25 6 5 0.25 0.17 0.22 0.33 0.16 0.26 3 2 -0.34 0.29 0.34 0.21 0.25 0.33 2 1 -1.28 0.18 0.22 0.23 0.16 0.26 6 4 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.72 0.18 0.23 0.45 0.17 0.26 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.43 0.18 0.22 0.73 0.16 0.26 4 4
HE 0240-6105 73 4720 100 1.26 0.25 0.35 -3.23 0.12 0.18 2.15 0.12 0.22 4.91 0.19 0.27 -0.25 0.18 0.29 1 1 4.65 0.12 0.18 0.30 0.14 0.23 7 5 2.57 0.15 0.24 -0.67 0.16 0.27 1 1 3.29 0.11 0.19 0.17 0.15 0.25 9 7 0.05 0.17 0.22 0.11 0.15 0.24 5 4 2.12 0.15 0.20 0.33 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.00 0.15 0.21 -0.44 0.15 0.23 3 3 1.76 0.15 0.21 -0.40 0.15 0.23 5 3 4.27 0.12 0.18 0.00 0.14 0.22 55 52 1.97 0.15 0.22 0.28 0.15 0.24 6 6 3.23 0.17 0.27 0.21 0.16 0.27 4 3 2.16 0.14 0.20 0.80 0.15 0.25 2 1 0.10 0.20 0.29 0.36 0.18 0.29 3 2 -0.85 0.17 0.22 0.14 0.16 0.24 6 4 -0.05 0.17 0.22 0.58 0.16 0.24 3 2 -1.78 0.20 0.24 -0.68 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0243-0753 71 5066 100 2.29 0.24 0.34 -2.49 0.14 0.19 1.77 0.12 0.22 6.19 0.20 0.26 0.29 0.17 0.27 1 1 5.31 0.11 0.18 0.23 0.15 0.24 7 6 3.51 0.13 0.24 -0.47 0.16 0.26 1 1 4.10 0.12 0.20 0.23 0.15 0.25 9 8 0.87 0.19 0.24 0.19 0.15 0.24 5 5 2.79 0.16 0.21 0.26 0.14 0.23 17 17 1.58 0.15 0.20 0.07 0.15 0.23 3 3 2.99 0.17 0.27 -0.19 0.16 0.26 3 3 2.66 0.14 0.19 -0.24 0.14 0.23 5 5 5.01 0.14 0.19 0.00 0.14 0.22 55 54 2.69 0.16 0.23 0.26 0.15 0.24 6 6 3.85 0.17 0.28 0.09 0.16 0.27 4 4 2.38 0.14 0.21 0.27 0.14 0.25 2 1 0.10 0.21 0.32 -0.38 0.19 0.30 3 2 -0.74 0.18 0.23 -0.48 0.15 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.38 0.18 0.22 -1.01 0.15 0.23 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0243-5238 60 5085 100 2.35 0.26 0.36 -3.04 0.12 0.18 1.64 0.13 0.23 5.75 0.19 0.26 0.40 0.18 0.28 1 1 4.87 0.11 0.18 0.33 0.15 0.24 7 6 2.40 0.14 0.22 -1.03 0.16 0.25 1 1 3.64 0.12 0.20 0.32 0.15 0.25 9 7 0.22 0.19 0.24 0.09 0.16 0.25 5 4 2.21 0.16 0.21 0.23 0.15 0.24 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.34 0.16 0.22 -0.29 0.15 0.23 3 3 1.61 0.17 0.21 -0.75 0.16 0.23 5 3 4.46 0.12 0.18 0.00 0.14 0.22 55 45 2.12 0.16 0.22 0.24 0.15 0.24 6 6 3.20 0.18 0.25 -0.01 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.11 0.22 0.33 -0.04 0.20 0.31 3 2 -0.92 0.19 0.23 -0.12 0.17 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.21 0.20 0.24 -0.31 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0244-4111 46 5624 100 3.39 0.26 0.36 -2.56 0.12 0.17 1.38 0.14 0.24 6.08 0.18 0.24 0.25 0.17 0.26 1 1 5.36 0.11 0.17 0.34 0.14 0.23 7 5 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 4.18 0.11 0.20 0.37 0.15 0.24 9 7 0.71 0.18 0.23 0.10 0.17 0.26 5 4 2.77 0.16 0.21 0.30 0.15 0.24 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.92 0.17 0.23 -0.19 0.16 0.24 3 3 2.26 0.16 0.20 -0.57 0.15 0.23 5 3 4.94 0.12 0.17 0.00 0.14 0.22 55 42 2.61 0.15 0.22 0.25 0.15 0.24 6 4 3.69 0.18 0.25 -0.00 0.18 0.26 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.26 0.22 0.31 -0.16 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.75 0.20 0.24 -0.32 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0248+0039 52 5199 100 2.57 0.25 0.35 -2.53 0.12 0.18 1.75 0.13 0.23 5.96 0.19 0.25 0.09 0.18 0.27 1 1 5.31 0.11 0.18 0.26 0.15 0.24 7 6 3.16 0.16 0.25 -0.78 0.17 0.26 1 1 4.10 0.12 0.20 0.27 0.14 0.24 9 8 0.78 0.18 0.23 0.14 0.16 0.25 5 4 2.73 0.16 0.22 0.24 0.15 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.76 0.17 0.25 -0.38 0.16 0.25 3 3 2.24 0.17 0.23 -0.62 0.16 0.24 5 3 4.97 0.12 0.18 0.00 0.14 0.22 55 53 2.52 0.16 0.22 0.13 0.15 0.25 6 6 3.51 0.19 0.26 -0.21 0.18 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.19 0.21 0.31 -0.25 0.20 0.30 3 2 -0.58 0.19 0.23 -0.29 0.17 0.25 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.66 0.21 0.26 -0.26 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0256-1109 16 5891 100 4.04 0.34 0.44 -2.73 0.13 0.18 1.69 0.24 0.34 6.33 0.19 0.26 0.67 0.19 0.28 1 1 5.32 0.13 0.19 0.47 0.16 0.24 7 1 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.89 0.13 0.20 0.25 0.16 0.25 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 17 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.77 0.13 0.18 0.00 0.15 0.22 54 5 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0300-0751 33 5280 100 2.97 0.26 0.36 -2.27 0.13 0.19 1.61 0.15 0.25 6.22 0.20 0.25 0.10 0.17 0.26 1 1 5.51 0.12 0.18 0.19 0.15 0.23 7 6 3.58 0.19 0.27 -0.62 0.20 0.29 1 1 4.40 0.13 0.21 0.30 0.15 0.24 9 8 1.07 0.18 0.23 0.17 0.17 0.26 5 4 3.06 0.17 0.22 0.30 0.16 0.25 17 13 1.90 0.17 0.21 0.17 0.16 0.25 3 1 3.12 0.19 0.28 -0.28 0.19 0.27 3 3 2.75 0.16 0.22 -0.37 0.16 0.24 5 3 5.23 0.13 0.19 0.00 0.14 0.22 55 47 2.85 0.17 0.23 0.20 0.16 0.25 6 5 3.95 0.20 0.30 -0.03 0.20 0.29 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.83 0.17 0.25 0.13 0.17 0.26 3 2 0.03 0.19 0.24 0.06 0.17 0.27 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.11 0.26 0.31 0.02 0.24 0.31 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.99 0.19 0.23 0.77 0.17 0.27 4 3
HE 0305-4520 56 4817 100 1.56 0.25 0.35 -2.91 0.13 0.18 2.02 0.13 0.23 5.80 0.19 0.26 0.33 0.18 0.28 1 1 4.87 0.13 0.18 0.20 0.14 0.23 7 6 2.79 0.23 0.28 -0.77 0.21 0.29 1 1 3.67 0.12 0.20 0.23 0.15 0.25 9 8 0.49 0.18 0.23 0.23 0.16 0.24 5 5 2.30 0.16 0.21 0.19 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.29 0.14 0.24 -0.47 0.15 0.24 3 3 1.88 0.16 0.22 -0.60 0.15 0.23 5 3 4.59 0.13 0.18 0.00 0.14 0.22 55 51 2.19 0.16 0.22 0.18 0.15 0.24 6 5 3.46 0.19 0.29 0.12 0.18 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.60 0.23 0.33 -0.66 0.21 0.31 3 2 -1.05 0.13 0.20 -0.38 0.17 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.20 0.21 0.27 0.59 0.19 0.27 2 1 -1.45 0.18 0.23 0.29 0.16 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0308-1154 34 4984 100 2.05 0.27 0.37 -2.82 0.13 0.18 1.69 0.14 0.24 5.95 0.21 0.27 0.38 0.19 0.28 1 1 5.38 0.12 0.19 0.62 0.15 0.23 7 6 3.17 0.24 0.31 -0.48 0.25 0.33 1 1 4.03 0.12 0.20 0.49 0.15 0.25 9 8 0.85 0.19 0.24 0.51 0.17 0.26 5 4 2.50 0.17 0.22 0.30 0.16 0.24 17 15 1.50 0.16 0.20 0.32 0.16 0.23 3 1 2.76 0.17 0.28 -0.09 0.17 0.28 3 3 1.87 0.17 0.22 -0.70 0.16 0.24 5 3 4.68 0.13 0.18 0.00 0.14 0.22 55 44 2.18 0.16 0.23 0.08 0.15 0.24 6 5 3.62 0.23 0.33 0.20 0.22 0.32 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.78 0.20 0.27 -1.93 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0315+0000 43 5013 100 2.11 0.26 0.36 -2.73 0.13 0.19 1.72 0.13 0.23 5.84 0.19 0.26 0.18 0.18 0.28 1 1 5.11 0.12 0.18 0.26 0.15 0.24 7 7 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.91 0.12 0.20 0.28 0.15 0.25 9 7 0.57 0.18 0.23 0.13 0.16 0.24 5 4 2.56 0.16 0.21 0.26 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.71 0.19 0.28 -0.23 0.18 0.27 3 2 2.02 0.17 0.22 -0.64 0.16 0.23 5 3 4.77 0.13 0.19 0.00 0.14 0.22 55 50 2.41 0.16 0.22 0.22 0.15 0.24 6 6 3.86 0.18 0.29 0.34 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.23 0.21 0.30 -0.01 0.19 0.28 3 2 -0.52 0.19 0.24 -0.03 0.16 0.25 6 3 0.31 0.19 0.24 0.44 0.17 0.26 3 1 -0.25 0.19 0.26 0.34 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.57 0.19 0.23 0.65 0.16 0.25 4 3
HE 0316+0214 35 4639 100 1.39 0.27 0.37 -3.13 0.11 0.17 1.98 0.14 0.24 4.54 0.23 0.29 -0.71 0.22 0.30 1 1 5.11 0.12 0.19 0.67 0.15 0.23 7 7 2.84 0.26 0.33 -0.49 0.27 0.34 1 1 3.45 0.12 0.20 0.22 0.15 0.25 9 6 0.44 0.18 0.23 0.40 0.17 0.26 5 5 2.07 0.14 0.20 0.19 0.15 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.13 0.17 0.26 -0.40 0.18 0.26 3 3 1.52 0.17 0.32 -0.73 0.21 0.33 5 3 4.36 0.11 0.17 0.00 0.14 0.22 55 45 1.87 0.16 0.22 0.09 0.16 0.25 6 5 3.42 0.23 0.32 0.31 0.22 0.31 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.65 0.21 0.28 -1.48 0.21 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.39 0.19 0.23 -1.38 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0317-4640 54 5872 100 4.10 0.24 0.34 -2.33 0.11 0.17 1.49 0.13 0.23 6.29 0.17 0.23 0.22 0.17 0.26 1 1 5.57 0.11 0.17 0.31 0.14 0.23 7 4 3.24 0.13 0.22 -0.91 0.16 0.25 1 1 4.33 0.11 0.20 0.30 0.14 0.25 9 8 0.85 0.17 0.23 0.01 0.17 0.27 5 2 2.94 0.14 0.20 0.24 0.15 0.24 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.07 0.15 0.21 -0.28 0.16 0.23 3 3 2.38 0.16 0.20 -0.69 0.16 0.24 5 2 5.18 0.11 0.17 0.00 0.14 0.22 55 42 2.74 0.15 0.21 0.14 0.16 0.25 6 4 3.84 0.16 0.22 -0.09 0.16 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.56 0.18 0.27 -0.09 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.38 0.19 0.23 -0.19 0.18 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0323-4529 41 5127 100 2.51 0.27 0.37 -3.15 0.13 0.18 1.62 0.14 0.24 5.63 0.19 0.26 0.38 0.18 0.28 1 1 4.82 0.12 0.19 0.38 0.16 0.24 7 4 2.52 0.17 0.24 -0.81 0.18 0.26 1 1 3.52 0.12 0.20 0.30 0.15 0.25 9 5 0.16 0.18 0.23 0.13 0.16 0.25 5 4 2.20 0.16 0.21 0.32 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.16 0.17 0.22 -0.37 0.16 0.23 3 3 1.47 0.17 0.21 -0.78 0.16 0.24 5 3 4.36 0.13 0.18 0.00 0.14 0.22 55 36 2.01 0.16 0.22 0.23 0.15 0.25 6 5 3.17 0.18 0.24 0.07 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.11 0.21 0.31 0.28 0.20 0.30 3 2 -0.72 0.19 0.24 0.18 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.71 0.23 0.28 0.30 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0328-1047 52 5301 100 3.03 0.24 0.34 -2.25 0.11 0.18 1.21 0.13 0.23 6.29 0.20 0.25 0.15 0.18 0.27 1 1 5.55 0.11 0.18 0.21 0.14 0.23 7 6 3.47 0.13 0.24 -0.76 0.17 0.26 1 1 4.34 0.12 0.20 0.23 0.14 0.24 9 8 1.02 0.19 0.24 0.09 0.17 0.27 5 4 3.03 0.16 0.21 0.26 0.16 0.25 17 15 1.79 0.16 0.20 0.03 0.16 0.25 3 1 3.28 0.16 0.26 -0.14 0.17 0.26 3 3 2.70 0.16 0.21 -0.45 0.16 0.24 5 3 5.26 0.11 0.18 0.00 0.14 0.22 55 52 2.88 0.16 0.23 0.21 0.16 0.25 6 6 4.03 0.14 0.27 0.02 0.17 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.74 0.14 0.23 0.01 0.16 0.25 3 2 -0.10 0.18 0.23 -0.09 0.17 0.27 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.18 0.23 0.29 -0.07 0.22 0.30 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.31 0.18 0.23 0.42 0.17 0.28 4 1
HE 0330-4004 42 5946 100 3.78 0.27 0.37 -2.20 0.12 0.17 1.53 0.14 0.24 6.28 0.18 0.24 0.08 0.19 0.28 1 1 5.63 0.12 0.18 0.25 0.15 0.23 7 4 3.29 0.16 0.23 -0.99 0.17 0.26 1 1 4.54 0.11 0.20 0.38 0.15 0.25 9 8 1.18 0.18 0.23 0.20 0.17 0.26 5 4 3.19 0.16 0.21 0.36 0.16 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.34 0.16 0.23 -0.14 0.16 0.24 3 3 2.47 0.15 0.20 -0.72 0.16 0.24 5 3 5.31 0.12 0.17 0.00 0.14 0.22 55 43 2.82 0.15 0.21 0.09 0.16 0.25 6 3 4.02 0.16 0.22 -0.03 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.72 0.21 0.30 -0.06 0.20 0.29 3 2 0.15 0.31 0.34 0.11 0.28 0.34 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.09 0.22 0.26 -0.03 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0330-4144 46 5961 100 4.20 0.24 0.34 -1.90 0.10 0.17 1.52 0.14 0.24 6.69 0.16 0.23 0.19 0.17 0.26 1 1 5.96 0.11 0.17 0.28 0.14 0.23 7 5 3.71 0.13 0.23 -0.87 0.17 0.26 1 1 4.68 0.11 0.20 0.22 0.14 0.24 9 7 1.44 0.15 0.21 0.16 0.16 0.27 5 3 3.42 0.15 0.20 0.30 0.16 0.25 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.61 0.15 0.22 -0.16 0.17 0.24 3 3 3.11 0.15 0.20 -0.39 0.16 0.24 5 3 5.61 0.10 0.17 0.00 0.14 0.22 55 50 3.09 0.16 0.22 0.06 0.17 0.26 6 4 4.20 0.14 0.22 -0.15 0.17 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.18 0.15 0.24 0.10 0.17 0.26 3 2 0.38 0.18 0.23 0.03 0.18 0.28 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.21 0.20 0.24 -0.03 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0331-4939 40 5206 100 2.60 0.28 0.38 -2.90 0.12 0.18 1.55 0.14 0.24 5.86 0.19 0.26 0.34 0.20 0.30 1 1 5.04 0.12 0.19 0.33 0.16 0.25 7 5 2.60 0.18 0.25 -1.00 0.19 0.27 1 1 3.66 0.12 0.20 0.18 0.15 0.25 9 6 0.43 0.18 0.23 0.14 0.17 0.26 5 4 2.38 0.16 0.21 0.24 0.16 0.24 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.33 0.17 0.23 -0.47 0.17 0.24 3 3 1.84 0.16 0.21 -0.68 0.16 0.24 5 3 4.63 0.12 0.18 0.00 0.14 0.22 55 41 2.31 0.16 0.22 0.27 0.17 0.26 6 5 3.36 0.19 0.25 -0.02 0.18 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.03 0.23 0.33 -0.07 0.21 0.30 3 2 -0.67 0.19 0.24 -0.04 0.18 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.67 0.20 0.24 -0.93 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0333-4001 46 5892 100 4.31 0.26 0.36 -2.64 0.12 0.17 1.30 0.14 0.24 6.06 0.17 0.24 0.32 0.17 0.26 1 1 5.31 0.11 0.17 0.37 0.15 0.23 7 3 2.94 0.11 0.20 -0.89 0.15 0.24 1 1 4.00 0.11 0.20 0.28 0.15 0.24 9 5 0.66 0.18 0.23 0.13 0.17 0.27 5 2 2.63 0.16 0.21 0.26 0.16 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.77 0.15 0.20 -0.26 0.15 0.23 3 3 2.07 0.16 0.20 -0.68 0.16 0.24 5 3 4.86 0.12 0.17 0.00 0.14 0.22 55 36 2.50 0.15 0.21 0.23 0.15 0.25 6 2 3.64 0.16 0.21 0.03 0.16 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.18 0.18 0.26 -0.14 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.67 0.19 0.23 -0.16 0.17 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0336-3829 41 5740 100 3.22 0.25 0.35 -2.75 0.13 0.18 1.48 0.15 0.25 5.87 0.16 0.27 0.23 0.22 0.32 1 1 5.17 0.12 0.18 0.35 0.15 0.24 7 3 2.60 0.15 0.22 -1.12 0.16 0.25 1 1 4.06 0.12 0.20 0.45 0.15 0.25 9 6 0.48 0.18 0.23 0.06 0.16 0.24 5 2 2.67 0.16 0.21 0.40 0.15 0.23 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.67 0.15 0.20 -0.25 0.15 0.23 3 3 2.03 0.16 0.20 -0.61 0.15 0.23 5 3 4.75 0.13 0.18 0.00 0.14 0.22 55 34 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.37 0.17 0.21 -0.13 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.07 0.25 0.33 -0.29 0.22 0.31 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.70 0.20 0.24 -0.08 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0337-5127 46 5247 100 2.86 0.25 0.35 -2.62 0.13 0.18 1.55 0.14 0.24 5.94 0.19 0.25 0.16 0.18 0.27 1 1 5.30 0.11 0.19 0.33 0.16 0.25 7 5 3.63 0.14 0.25 -0.23 0.17 0.27 1 1 4.08 0.13 0.21 0.33 0.14 0.25 9 8 0.67 0.18 0.23 0.11 0.16 0.26 5 4 2.67 0.17 0.22 0.26 0.15 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.83 0.17 0.25 -0.23 0.17 0.25 3 3 2.13 0.17 0.22 -0.65 0.16 0.24 5 3 4.89 0.13 0.18 0.00 0.14 0.22 55 46 2.54 0.17 0.23 0.23 0.16 0.25 6 6 3.55 0.18 0.26 -0.09 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.35 0.20 0.29 -0.01 0.19 0.29 3 2 -0.51 0.19 0.23 -0.14 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.50 0.21 0.27 -0.02 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.50 0.19 0.24 0.60 0.17 0.27 4 1
HE 0338-3945 47 6162 100 4.09 0.25 0.35 -2.41 0.13 0.18 1.33 0.14 0.24 8.05 0.15 0.23 2.07 0.16 0.27 1 1 5.56 0.11 0.17 0.39 0.15 0.24 5 1 3.37 0.15 0.22 -0.69 0.16 0.26 1 1 4.32 0.11 0.20 0.37 0.15 0.25 5 3 1.24 0.18 0.23 0.48 0.16 0.25 3 2 3.02 0.13 0.19 0.41 0.15 0.23 11 7 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.22 0.16 0.22 -0.04 0.16 0.24 1 1 2.50 0.15 0.20 -0.48 0.15 0.23 4 2 5.09 0.13 0.18 0.00 0.14 0.22 35 23 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 3.76 0.16 0.21 -0.08 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 1.29 0.16 0.24 0.73 0.16 0.26 2 2 0.56 0.19 0.24 0.73 0.17 0.25 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 2.13 0.12 0.18 2.41 0.15 0.22 2 2 1.01 0.18 0.22 2.26 0.16 0.24 3 3 1.38 0.18 0.24 2.21 0.16 0.26 7 4 1.18 0.18 0.23 2.09 0.16 0.24 5 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -0.01 0.18 0.23 1.89 0.16 0.25 3 2
HE 0339-4027 55 5896 100 4.11 0.24 0.34 -1.81 0.11 0.18 1.48 0.14 0.24 6.76 0.17 0.23 0.18 0.16 0.25 1 1 6.07 0.11 0.17 0.31 0.14 0.23 7 4 3.97 0.11 0.22 -0.69 0.16 0.26 1 1 4.90 0.11 0.20 0.35 0.14 0.24 9 9 1.45 0.17 0.22 0.09 0.16 0.27 5 4 3.46 0.15 0.20 0.25 0.15 0.24 17 13 2.27 0.15 0.19 0.08 0.15 0.24 3 1 3.79 0.14 0.23 -0.06 0.16 0.24 3 3 3.24 0.15 0.20 -0.34 0.15 0.24 5 3 5.69 0.11 0.18 0.00 0.14 0.22 55 52 3.19 0.15 0.22 0.08 0.15 0.25 6 4 4.35 0.15 0.24 -0.08 0.17 0.26 4 3 2.92 0.14 0.21 0.13 0.15 0.26 2 1 1.33 0.13 0.22 0.18 0.15 0.25 3 2 0.44 0.18 0.22 0.01 0.16 0.27 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.22 0.20 0.25 -0.09 0.19 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0340-3430 49 5914 100 3.81 0.25 0.35 -1.95 0.12 0.18 1.59 0.14 0.24 6.50 0.17 0.23 0.06 0.17 0.26 1 1 5.82 0.11 0.18 0.19 0.15 0.23 7 4 3.52 0.15 0.24 -1.00 0.17 0.26 1 1 4.77 0.11 0.20 0.36 0.15 0.25 9 8 1.32 0.17 0.23 0.10 0.16 0.25 5 3 3.32 0.16 0.21 0.25 0.15 0.24 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.56 0.16 0.23 -0.16 0.16 0.24 3 3 2.94 0.16 0.21 -0.50 0.15 0.23 5 3 5.55 0.12 0.18 0.00 0.14 0.22 55 48 2.92 0.14 0.20 -0.05 0.15 0.24 6 4 4.04 0.25 0.29 -0.26 0.22 0.28 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.89 0.17 0.28 -0.13 0.17 0.28 3 2 -0.02 0.25 0.28 -0.31 0.21 0.29 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.04 0.20 0.25 -0.22 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0340-5355 59 4862 100 1.81 0.25 0.35 -2.89 0.13 0.18 1.87 0.12 0.22 5.40 0.20 0.26 -0.11 0.18 0.28 1 1 4.66 0.10 0.18 -0.04 0.15 0.24 7 4 2.33 0.15 0.23 -1.26 0.16 0.25 1 1 3.58 0.12 0.20 0.10 0.15 0.25 9 8 0.21 0.18 0.23 -0.08 0.16 0.25 5 4 2.07 0.16 0.21 -0.07 0.15 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.28 0.16 0.24 -0.51 0.15 0.24 3 3 1.63 0.16 0.22 -0.88 0.15 0.23 5 3 4.62 0.13 0.18 0.00 0.14 0.22 55 53 1.88 0.16 0.22 -0.16 0.15 0.24 6 6 2.55 0.18 0.22 -0.82 0.16 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.44 0.23 0.33 -0.53 0.20 0.31 3 2 -1.20 0.18 0.23 -0.56 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.16 0.19 0.23 -1.41 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0341-4024 79 6108 100 4.20 0.24 0.34 -1.82 0.12 0.17 1.41 0.13 0.23 6.83 0.15 0.22 0.27 0.16 0.25 1 1 5.95 0.11 0.17 0.19 0.14 0.23 7 4 -9.99 0.00 0.00 -9.99 0.00 0.00 1 1 4.79 0.11 0.20 0.26 0.14 0.24 9 9 1.41 0.17 0.22 0.07 0.16 0.25 5 4 3.45 0.15 0.20 0.26 0.15 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.80 0.14 0.22 -0.05 0.15 0.24 3 3 3.10 0.14 0.20 -0.47 0.15 0.23 5 3 5.68 0.12 0.17 0.00 0.14 0.22 55 53 3.11 0.14 0.21 0.02 0.15 0.24 6 4 4.24 0.15 0.22 -0.18 0.16 0.24 4 2 2.88 0.14 0.21 0.10 0.15 0.25 2 1 1.05 0.16 0.25 -0.09 0.16 0.26 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.23 0.19 0.24 -0.08 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.62 0.18 0.23 0.69 0.16 0.26 4 1
HE 0344+0139 42 6291 100 4.18 0.26 0.36 -1.81 0.12 0.18 1.45 0.15 0.25 7.00 0.16 0.23 0.41 0.17 0.26 1 1 5.90 0.11 0.17 0.12 0.15 0.23 7 3 3.41 0.15 0.22 -1.26 0.16 0.26 1 1 4.85 0.10 0.19 0.29 0.15 0.25 9 8 1.48 0.16 0.22 0.11 0.16 0.26 5 3 3.48 0.15 0.21 0.26 0.15 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.86 0.16 0.23 -0.01 0.16 0.24 3 3 3.20 0.14 0.20 -0.39 0.15 0.23 5 3 5.70 0.12 0.18 0.00 0.14 0.22 55 47 3.12 0.15 0.21 -0.00 0.15 0.25 6 2 4.41 0.19 0.25 -0.04 0.18 0.26 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.03 0.20 0.29 -0.14 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.19 0.19 0.24 -0.14 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0347-1819 59 5198 100 4.23 0.24 0.34 -2.78 0.14 0.19 1.61 0.15 0.25 5.65 0.23 0.28 0.03 0.18 0.26 1 1 5.23 0.14 0.19 0.42 0.14 0.24 7 3 3.26 0.12 0.22 -0.44 0.15 0.25 1 1 3.94 0.13 0.20 0.35 0.14 0.24 9 8 0.46 0.18 0.24 0.07 0.16 0.26 5 2 2.41 0.17 0.22 0.16 0.15 0.24 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.84 0.15 0.21 -0.06 0.15 0.23 3 3 2.10 0.18 0.22 -0.52 0.15 0.23 5 2 4.73 0.14 0.19 0.00 0.14 0.22 55 43 2.20 0.18 0.23 0.06 0.15 0.25 6 5 3.27 0.16 0.21 -0.21 0.15 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.02 0.19 0.25 -0.18 0.17 0.26 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.15 0.20 0.25 -0.51 0.16 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0353-6024 53 5320 100 3.15 0.27 0.37 -3.17 0.13 0.18 1.49 0.14 0.24 5.51 0.19 0.25 0.29 0.17 0.27 1 1 4.62 0.12 0.21 0.21 0.17 0.26 7 4 2.49 0.12 0.21 -0.81 0.16 0.26 1 1 3.30 0.12 0.20 0.11 0.15 0.25 9 3 0.28 0.18 0.23 0.27 0.16 0.25 5 2 2.11 0.16 0.22 0.25 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.07 0.16 0.21 -0.43 0.15 0.23 3 2 1.46 0.16 0.21 -0.76 0.15 0.23 5 3 4.33 0.13 0.18 0.00 0.14 0.22 55 37 2.24 0.15 0.21 0.49 0.15 0.24 6 5 3.25 0.17 0.23 0.17 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.48 0.19 0.26 -1.28 0.17 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0400-2917 61 5065 100 2.39 0.25 0.35 -2.88 0.12 0.18 1.67 0.13 0.23 5.66 0.19 0.26 0.15 0.18 0.27 1 1 4.68 0.11 0.18 -0.02 0.15 0.24 7 5 2.21 0.15 0.22 -1.38 0.16 0.25 1 1 3.50 0.12 0.20 0.02 0.14 0.25 9 7 0.18 0.18 0.23 -0.11 0.16 0.25 5 4 2.12 0.16 0.21 -0.02 0.15 0.24 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.34 0.16 0.23 -0.45 0.16 0.23 3 3 1.83 0.17 0.22 -0.68 0.15 0.23 5 3 4.62 0.12 0.18 0.00 0.14 0.22 55 49 2.03 0.16 0.22 -0.01 0.15 0.25 6 5 3.23 0.18 0.26 -0.14 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.78 0.22 0.30 -0.87 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.84 0.19 0.23 -1.10 0.16 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0401-0138 56 4866 100 1.76 0.27 0.37 -3.34 0.13 0.18 1.45 0.13 0.23 5.30 0.20 0.27 0.24 0.18 0.28 1 1 4.67 0.12 0.19 0.42 0.15 0.23 7 5 2.07 0.11 0.21 -1.06 0.15 0.25 1 1 3.37 0.12 0.20 0.35 0.15 0.25 9 6 -0.06 0.18 0.23 0.11 0.16 0.25 5 4 1.97 0.16 0.21 0.28 0.15 0.23 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.87 0.16 0.22 -0.46 0.15 0.23 3 3 1.25 0.15 0.20 -0.80 0.15 0.23 5 3 4.16 0.13 0.18 0.00 0.14 0.22 55 41 1.82 0.16 0.22 0.24 0.15 0.24 6 5 2.94 0.18 0.26 0.02 0.17 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.26 0.23 0.35 0.11 0.21 0.33 3 2 -1.05 0.19 0.23 0.05 0.17 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.41 0.20 0.25 -0.21 0.18 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0417-0821 62 5811 100 4.83 0.24 0.34 -2.33 0.12 0.17 1.40 0.14 0.24 6.31 0.18 0.23 0.25 0.16 0.25 1 1 5.49 0.12 0.18 0.24 0.14 0.24 7 3 3.39 0.11 0.21 -0.75 0.15 0.25 1 1 4.26 0.12 0.20 0.23 0.14 0.24 9 8 0.97 0.17 0.22 0.13 0.16 0.26 5 2 2.95 0.15 0.21 0.26 0.15 0.25 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.24 0.13 0.20 -0.10 0.15 0.23 3 3 2.69 0.16 0.20 -0.37 0.15 0.24 5 3 5.17 0.12 0.17 0.00 0.14 0.22 55 41 2.78 0.16 0.22 0.19 0.15 0.25 6 4 3.92 0.15 0.21 0.00 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.48 0.16 0.24 -0.16 0.17 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.56 0.18 0.23 -0.36 0.17 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0430-4404 49 6214 100 4.27 0.25 0.35 -2.07 0.11 0.17 1.41 0.14 0.24 7.75 0.15 0.22 1.44 0.16 0.26 1 1 5.79 0.11 0.17 0.29 0.15 0.23 7 3 3.42 0.14 0.22 -0.97 0.16 0.25 1 1 4.61 0.11 0.20 0.33 0.15 0.25 9 7 1.28 0.17 0.23 0.19 0.17 0.26 5 3 3.26 0.16 0.21 0.32 0.16 0.25 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.57 0.15 0.21 -0.02 0.16 0.23 3 3 2.84 0.15 0.20 -0.47 0.15 0.24 5 3 5.42 0.11 0.17 0.00 0.14 0.22 55 41 2.94 0.15 0.21 0.10 0.15 0.25 6 3 4.18 0.15 0.21 0.01 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.45 0.14 0.23 0.56 0.16 0.25 3 2 0.76 0.18 0.23 0.60 0.17 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.67 0.14 0.18 1.62 0.15 0.23 2 2 0.50 0.17 0.22 1.41 0.17 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0430-4901 50 5296 100 3.12 0.25 0.35 -2.72 0.12 0.18 1.32 0.13 0.23 5.76 0.19 0.25 0.09 0.18 0.27 1 1 5.03 0.11 0.19 0.17 0.16 0.24 7 5 2.57 0.15 0.22 -1.18 0.16 0.25 1 1 3.76 0.12 0.20 0.12 0.14 0.25 9 7 0.42 0.18 0.23 -0.03 0.16 0.26 5 4 2.43 0.16 0.21 0.13 0.16 0.25 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.62 0.17 0.24 -0.33 0.16 0.24 3 3 1.96 0.17 0.21 -0.71 0.16 0.24 5 3 4.78 0.12 0.18 0.00 0.14 0.22 55 46 2.25 0.16 0.22 0.04 0.15 0.25 6 5 3.50 0.17 0.22 -0.03 0.17 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.25 0.18 0.27 -0.01 0.18 0.28 3 2 -0.45 0.19 0.24 0.02 0.17 0.27 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.08 0.22 0.27 0.50 0.20 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.05 0.18 0.23 1.16 0.17 0.27 4 3
HE 0432-0923 74 5131 100 2.64 0.23 0.33 -3.19 0.13 0.18 1.54 0.12 0.22 5.44 0.18 0.25 0.24 0.17 0.27 1 1 4.73 0.11 0.18 0.34 0.16 0.24 7 5 2.32 0.14 0.22 -0.96 0.15 0.25 1 1 3.49 0.11 0.20 0.32 0.15 0.25 9 6 0.07 0.17 0.22 0.09 0.15 0.24 5 4 2.16 0.15 0.21 0.33 0.14 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.97 0.16 0.21 -0.51 0.15 0.23 3 3 1.47 0.21 0.24 -0.73 0.17 0.25 5 3 4.31 0.13 0.18 0.00 0.14 0.22 55 41 2.03 0.16 0.22 0.29 0.15 0.24 6 5 3.17 0.18 0.24 0.11 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.26 0.17 0.26 0.47 0.16 0.27 3 2 -0.44 0.18 0.22 0.51 0.15 0.24 6 3 0.29 0.18 0.22 0.88 0.15 0.25 3 1 -0.34 0.20 0.26 0.72 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.43 0.18 0.23 1.25 0.15 0.24 4 2
HE 0436-4008 40 5431 100 3.34 0.24 0.34 -2.35 0.12 0.18 1.30 0.14 0.24 6.53 0.19 0.25 0.49 0.17 0.26 1 1 5.45 0.15 0.20 0.22 0.15 0.24 7 5 2.94 0.18 0.25 -1.18 0.19 0.28 1 1 4.26 0.12 0.20 0.25 0.14 0.24 9 8 0.86 0.18 0.23 0.05 0.16 0.26 5 4 2.97 0.16 0.21 0.30 0.15 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.17 0.17 0.25 -0.15 0.17 0.25 3 3 2.63 0.16 0.21 -0.41 0.16 0.24 5 3 5.15 0.12 0.18 0.00 0.14 0.22 55 49 2.75 0.15 0.22 0.18 0.15 0.25 6 5 3.97 0.19 0.27 0.07 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.95 0.14 0.22 0.33 0.15 0.24 3 2 0.01 0.18 0.23 0.12 0.17 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.48 0.22 0.27 -0.26 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0441-4343 44 5629 100 3.59 0.25 0.35 -2.52 0.12 0.18 1.29 0.15 0.25 6.20 0.18 0.24 0.33 0.17 0.26 1 1 5.37 0.12 0.18 0.32 0.15 0.23 7 4 2.86 0.15 0.23 -1.09 0.17 0.26 1 1 4.02 0.11 0.20 0.18 0.15 0.24 9 7 0.78 0.18 0.24 0.13 0.17 0.26 5 4 2.77 0.16 0.21 0.27 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.78 0.16 0.22 -0.36 0.15 0.23 3 3 2.23 0.16 0.21 -0.63 0.16 0.24 5 3 4.98 0.12 0.18 0.00 0.14 0.22 55 40 2.74 0.16 0.22 0.34 0.15 0.25 6 3 3.79 0.18 0.25 0.07 0.17 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.34 0.21 0.30 -0.10 0.20 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.99 0.19 0.24 -0.59 0.17 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0442-1234 77 4604 100 1.34 0.24 0.34 -2.41 0.14 0.20 2.21 0.12 0.22 5.37 0.22 0.27 -0.61 0.18 0.27 1 1 5.48 0.11 0.18 0.32 0.15 0.24 7 5 3.72 0.14 0.24 -0.34 0.15 0.25 1 1 4.14 0.12 0.20 0.20 0.15 0.25 9 9 0.91 0.18 0.23 0.16 0.15 0.24 5 5 2.76 0.16 0.21 0.15 0.14 0.23 17 17 1.49 0.17 0.21 -0.09 0.15 0.23 3 3 2.74 0.21 0.30 -0.52 0.17 0.26 3 3 2.59 0.15 0.20 -0.39 0.14 0.23 5 5 5.09 0.14 0.20 0.00 0.14 0.22 55 54 2.54 0.17 0.24 0.03 0.15 0.24 6 6 3.82 0.25 0.34 -0.02 0.20 0.29 4 4 2.26 0.13 0.20 0.07 0.14 0.25 2 2 0.24 0.19 0.26 -0.32 0.16 0.25 3 1 -0.42 0.18 0.22 -0.24 0.14 0.24 6 6 0.27 0.17 0.22 0.08 0.14 0.24 3 2 -0.42 0.23 0.34 -0.13 0.20 0.30 2 1 -1.21 0.18 0.22 0.03 0.14 0.25 6 5 -0.85 0.18 0.24 -0.01 0.14 0.27 10 3 -0.80 0.18 0.23 0.11 0.14 0.25 9 6 -1.00 0.18 0.23 0.40 0.14 0.25 8 2 -1.38 0.17 0.22 0.52 0.14 0.25 4 4
HE 0447-4858 18 5995 100 3.86 0.27 0.37 -1.69 0.12 0.18 1.35 0.19 0.29 6.74 0.17 0.24 0.04 0.18 0.27 1 1 6.14 0.12 0.18 0.24 0.15 0.24 7 2 3.97 0.24 0.31 -0.81 0.25 0.32 1 1 4.91 0.12 0.20 0.24 0.15 0.25 9 2 1.67 0.18 0.23 0.19 0.18 0.28 5 2 3.62 0.17 0.22 0.28 0.17 0.26 17 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 4.07 0.21 0.28 0.09 0.22 0.28 3 2 3.39 0.14 0.20 -0.31 0.16 0.24 5 1 5.81 0.12 0.18 0.00 0.14 0.22 55 18 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 4.90 0.37 0.43 0.33 0.41 0.45 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.95 0.14 0.22 0.67 0.16 0.25 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.89 0.22 0.28 0.45 0.23 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0450-4705 48 5429 100 3.34 0.28 0.38 -3.10 0.13 0.18 1.49 0.15 0.25 6.14 0.18 0.25 0.84 0.17 0.27 1 1 4.70 0.12 0.21 0.22 0.17 0.26 7 4 2.51 0.14 0.26 -0.86 0.21 0.30 1 1 3.48 0.12 0.20 0.21 0.15 0.25 9 3 0.06 0.18 0.23 -0.01 0.17 0.26 5 1 2.16 0.15 0.20 0.24 0.15 0.24 17 7 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.34 0.16 0.21 -0.24 0.15 0.23 3 3 2.04 0.17 0.21 -0.25 0.16 0.23 5 2 4.40 0.13 0.18 0.00 0.14 0.22 55 34 2.13 0.16 0.22 0.31 0.15 0.25 6 4 3.52 0.16 0.23 0.36 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.61 0.21 0.29 -0.48 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0
HE 0454-4758 77 5388 100 3.33 0.25 0.35 -3.10 0.13 0.18 1.49 0.13 0.23 5.72 0.18 0.25 0.44 0.17 0.27 1 1 4.77 0.11 0.20 0.29 0.17 0.26 7 4 2.43 0.18 0.24 -0.94 0.16 0.26 1 1 3.54 0.11 0.20 0.28 0.15 0.25 9 6 0.18 0.18 0.23 0.11 0.16 0.25 5 2 2.24 0.16 0.21 0.32 0.15 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.22 0.17 0.21 -0.35 0.16 0.23 3 2 1.59 0.16 0.21 -0.70 0.15 0.23 5 3 4.40 0.13 0.18 0.00 0.14 0.22 55 39 2.15 0.15 0.21 0.33 0.15 0.24 6 5 3.22 0.16 0.21 0.07 0.15 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.49 0.20 0.28 -0.36 0.18 0.28 3 2 -0.97 0.19 0.24 -0.11 0.17 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.66 0.19 0.23 -0.69 0.16 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0501-5139 21 5861 100 3.54 0.26 0.36 -2.38 0.14 0.19 1.49 0.16 0.26 6.41 0.18 0.24 0.40 0.18 0.28 1 1 5.39 0.12 0.18 0.19 0.16 0.24 7 1 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 4.32 0.12 0.20 0.34 0.15 0.25 9 1 0.88 0.18 0.23 0.09 0.15 0.24 5 1 3.03 0.16 0.21 0.39 0.15 0.23 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.05 0.17 0.23 -0.24 0.16 0.24 3 2 2.44 0.16 0.21 -0.57 0.15 0.23 5 1 5.12 0.14 0.19 0.00 0.14 0.22 55 18 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.74 0.20 0.25 -0.13 0.19 0.26 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.46 0.26 0.35 -0.13 0.23 0.33 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0501-5644 41 5033 100 2.30 0.25 0.35 -2.41 0.12 0.19 1.76 0.13 0.23 6.26 0.20 0.26 0.27 0.19 0.27 1 1 5.47 0.12 0.18 0.29 0.15 0.23 7 6 3.33 0.18 0.27 -0.74 0.20 0.28 1 1 4.24 0.13 0.21 0.28 0.14 0.25 9 8 0.91 0.17 0.23 0.15 0.16 0.25 5 5 2.78 0.16 0.21 0.16 0.15 0.24 17 16 1.54 0.16 0.20 -0.06 0.16 0.24 3 1 3.06 0.19 0.29 -0.20 0.18 0.27 3 3 2.63 0.15 0.20 -0.36 0.15 0.23 5 3 5.10 0.12 0.19 0.00 0.14 0.22 55 52 2.60 0.16 0.23 0.08 0.16 0.25 6 6 3.59 0.21 0.30 -0.25 0.20 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.41 0.20 0.29 -0.16 0.20 0.29 3 1 -0.34 0.19 0.23 -0.17 0.17 0.26 6 3 0.64 0.18 0.23 0.44 0.16 0.26 3 1 -0.72 0.23 0.29 -0.45 0.21 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.59 0.18 0.23 0.30 0.16 0.26 4 3
HE 0512-3835 41 4948 100 2.01 0.25 0.35 -2.40 0.12 0.19 1.90 0.14 0.24 5.77 0.21 0.26 -0.22 0.21 0.29 1 1 5.52 0.12 0.19 0.33 0.15 0.24 7 5 3.63 0.18 0.27 -0.44 0.19 0.27 1 1 4.28 0.12 0.21 0.31 0.15 0.25 9 8 0.96 0.18 0.23 0.19 0.17 0.26 5 5 2.94 0.17 0.22 0.31 0.16 0.24 17 17 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.03 0.18 0.29 -0.25 0.18 0.26 3 3 2.65 0.14 0.20 -0.35 0.15 0.23 5 3 5.11 0.12 0.19 0.00 0.14 0.22 55 53 2.53 0.16 0.23 -0.00 0.16 0.25 6 6 3.52 0.21 0.30 -0.34 0.20 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.61 0.18 0.25 0.03 0.17 0.26 3 2 -0.40 0.19 0.23 -0.25 0.17 0.27 6 3 0.45 0.18 0.23 0.24 0.17 0.27 3 1 -0.37 0.23 0.30 -0.11 0.21 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.51 0.18 0.23 0.37 0.17 0.28 4 3
HE 0513-4557 19 5629 100 3.62 0.28 0.38 -2.79 0.13 0.18 1.44 0.20 0.30 5.99 0.18 0.25 0.39 0.18 0.27 1 1 5.13 0.12 0.18 0.34 0.15 0.24 7 1 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 3.78 0.12 0.20 0.21 0.15 0.25 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 17 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.71 0.13 0.18 0.00 0.14 0.22 55 10 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.19 0.23 0.32 0.01 0.21 0.30 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0516-3820 51 5342 100 3.05 0.24 0.34 -2.33 0.12 0.18 1.48 0.13 0.23 6.46 0.19 0.25 0.39 0.18 0.26 1 1 5.48 0.11 0.18 0.22 0.15 0.23 7 5 3.03 0.18 0.26 -1.12 0.20 0.28 1 1 4.28 0.11 0.20 0.24 0.14 0.24 9 8 0.92 0.18 0.23 0.07 0.16 0.26 5 4 2.92 0.15 0.20 0.22 0.15 0.24 17 15 1.70 0.16 0.20 0.03 0.16 0.24 3 1 3.26 0.16 0.26 -0.08 0.17 0.26 3 3 2.82 0.15 0.20 -0.25 0.15 0.23 5 4 5.18 0.12 0.18 0.00 0.14 0.22 55 54 2.70 0.17 0.23 0.10 0.16 0.25 6 6 3.80 0.19 0.27 -0.12 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.69 0.16 0.24 0.05 0.16 0.25 3 2 -0.08 0.19 0.23 0.00 0.17 0.26 6 3 0.69 0.19 0.23 0.41 0.17 0.27 3 1 -0.30 0.23 0.29 -0.11 0.21 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.22 0.19 0.24 0.60 0.17 0.27 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.15 0.18 0.23 0.67 0.16 0.27 4 3
HE 0517-1952 69 5254 100 1.99 0.25 0.35 -2.61 0.14 0.19 2.09 0.12 0.22 5.26 0.20 0.26 -0.52 0.19 0.29 1 1 5.17 0.12 0.18 0.20 0.15 0.24 7 7 3.01 0.16 0.24 -0.84 0.16 0.26 1 1 4.01 0.11 0.19 0.27 0.15 0.25 9 8 0.66 0.18 0.23 0.10 0.15 0.23 5 5 2.65 0.17 0.22 0.24 0.15 0.23 17 15 1.39 0.15 0.20 0.00 0.15 0.23 3 1 2.66 0.18 0.23 -0.40 0.15 0.23 3 3 2.14 0.16 0.21 -0.64 0.15 0.23 5 3 4.89 0.14 0.19 0.00 0.14 0.22 55 52 2.44 0.15 0.22 0.13 0.15 0.24 6 6 3.59 0.15 0.23 -0.05 0.15 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.33 0.22 0.33 -0.03 0.19 0.30 3 2 -0.64 0.18 0.23 -0.27 0.15 0.23 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.86 0.21 0.25 -0.38 0.17 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0519-5525 26 5580 100 3.48 0.27 0.37 -2.52 0.12 0.18 1.45 0.16 0.26 6.16 0.18 0.25 0.29 0.17 0.26 1 1 5.47 0.12 0.18 0.41 0.15 0.23 7 1 3.20 0.18 0.26 -0.76 0.20 0.28 1 1 4.21 0.12 0.20 0.37 0.15 0.24 9 3 0.74 0.19 0.24 0.08 0.17 0.26 5 1 2.87 0.17 0.22 0.37 0.16 0.24 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.96 0.18 0.24 -0.19 0.17 0.25 3 3 2.34 0.17 0.22 -0.53 0.16 0.24 5 2 4.98 0.12 0.18 0.00 0.14 0.22 55 29 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.86 0.23 0.30 0.13 0.22 0.30 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.64 0.20 0.29 0.18 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.58 0.20 0.25 -0.20 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0520-1748 72 5272 100 3.06 0.24 0.34 -2.52 0.12 0.18 1.46 0.12 0.22 6.32 0.19 0.25 0.45 0.17 0.26 1 1 5.30 0.11 0.18 0.24 0.15 0.23 7 6 2.88 0.14 0.23 -1.07 0.16 0.25 1 1 4.10 0.12 0.20 0.26 0.14 0.24 9 8 0.70 0.18 0.23 0.05 0.16 0.26 5 4 2.75 0.16 0.21 0.26 0.15 0.24 17 16 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.06 0.15 0.24 -0.09 0.16 0.25 3 3 2.66 0.12 0.20 -0.21 0.15 0.23 5 4 4.98 0.12 0.18 0.00 0.14 0.22 55 52 2.53 0.16 0.22 0.13 0.15 0.25 6 5 3.66 0.16 0.25 -0.07 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.09 0.23 0.33 -0.54 0.22 0.33 3 2 -0.61 0.19 0.23 -0.33 0.16 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.98 0.19 0.24 -0.58 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0524-2055 66 4739 100 1.57 0.24 0.34 -2.58 0.12 0.19 1.95 0.12 0.22 5.56 0.21 0.26 -0.25 0.19 0.28 1 1 5.32 0.11 0.18 0.32 0.15 0.24 7 6 3.59 0.14 0.24 -0.29 0.16 0.25 1 1 4.01 0.12 0.20 0.24 0.15 0.25 9 8 0.63 0.18 0.23 0.05 0.15 0.25 5 5 2.64 0.16 0.21 0.21 0.15 0.23 17 17 1.30 0.16 0.20 -0.11 0.15 0.24 3 3 2.77 0.17 0.28 -0.32 0.16 0.26 3 3 2.36 0.15 0.20 -0.45 0.15 0.23 5 5 4.91 0.12 0.19 0.00 0.14 0.22 55 54 2.43 0.16 0.23 0.10 0.15 0.24 6 6 3.66 0.19 0.29 -0.01 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.51 0.16 0.23 0.13 0.15 0.25 3 1 -0.56 0.18 0.22 -0.21 0.15 0.25 6 6 0.28 0.17 0.22 0.27 0.15 0.25 3 2 -0.39 0.21 0.31 0.07 0.20 0.29 2 1 -1.33 0.18 0.22 0.08 0.15 0.25 6 4 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.89 0.18 0.23 0.20 0.15 0.25 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.59 0.18 0.22 0.49 0.15 0.25 4 4
HE 0534-4615 53 5506 100 3.40 0.24 0.34 -2.01 0.12 0.18 1.43 0.13 0.23 6.51 0.19 0.25 0.13 0.17 0.26 1 1 5.80 0.12 0.18 0.22 0.14 0.23 7 4 3.59 0.13 0.23 -0.87 0.16 0.25 1 1 4.64 0.11 0.20 0.28 0.14 0.24 9 8 1.21 0.18 0.23 0.05 0.16 0.27 5 4 3.20 0.16 0.21 0.19 0.15 0.25 17 15 2.04 0.16 0.20 0.04 0.15 0.24 3 2 3.48 0.15 0.24 -0.18 0.16 0.25 3 3 3.03 0.15 0.20 -0.35 0.15 0.24 5 4 5.49 0.12 0.18 0.00 0.14 0.22 55 53 2.93 0.15 0.22 0.02 0.15 0.25 6 5 4.04 0.18 0.27 -0.20 0.19 0.27 4 3 2.77 0.14 0.21 0.18 0.15 0.26 2 1 1.01 0.14 0.22 0.04 0.15 0.25 3 2 0.06 0.18 0.23 -0.17 0.16 0.27 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.11 0.22 0.27 -0.01 0.20 0.30 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.00 0.18 0.23 0.49 0.16 0.27 4 3
HE 0538-4515 41 5896 100 3.97 0.25 0.35 -1.52 0.10 0.18 1.52 0.14 0.24 7.02 0.16 0.23 0.15 0.18 0.26 1 1 6.27 0.11 0.17 0.21 0.14 0.23 7 4 4.26 0.12 0.24 -0.69 0.17 0.26 1 1 5.12 0.10 0.20 0.28 0.14 0.24 9 9 1.82 0.17 0.22 0.17 0.18 0.28 5 5 3.73 0.15 0.20 0.23 0.17 0.26 17 14 2.62 0.15 0.19 0.14 0.16 0.26 3 2 4.14 0.13 0.23 -0.01 0.17 0.25 3 3 3.72 0.13 0.18 -0.15 0.15 0.24 5 5 5.98 0.10 0.18 0.00 0.14 0.22 55 53 3.50 0.14 0.21 0.10 0.16 0.26 6 5 4.54 0.17 0.26 -0.19 0.19 0.27 4 3 3.24 0.14 0.21 0.16 0.16 0.27 2 1 1.61 0.14 0.21 0.16 0.16 0.25 3 1 0.71 0.18 0.23 -0.01 0.19 0.28 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.51 0.23 0.28 -0.10 0.24 0.31 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.50 0.18 0.23 0.51 0.18 0.29 4 1
HE 0547-4539 94 5152 100 2.59 0.24 0.34 -3.01 0.13 0.18 1.57 0.12 0.22 5.88 0.19 0.26 0.50 0.17 0.27 1 1 4.70 0.11 0.18 0.13 0.15 0.24 7 5 2.38 0.14 0.22 -1.07 0.15 0.24 1 1 3.48 0.12 0.20 0.13 0.14 0.24 9 7 0.23 0.17 0.22 0.07 0.15 0.24 5 4 2.20 0.16 0.21 0.19 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.38 0.16 0.22 -0.27 0.15 0.23 3 3 1.83 0.16 0.21 -0.55 0.15 0.23 5 3 4.49 0.13 0.18 0.00 0.14 0.22 55 49 2.10 0.16 0.22 0.19 0.15 0.24 6 6 3.27 0.16 0.23 0.03 0.16 0.24 4 4 2.22 0.14 0.21 0.63 0.14 0.25 2 1 0.14 0.19 0.29 0.18 0.18 0.29 3 2 -1.10 0.18 0.23 -0.33 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.91 0.18 0.23 -1.03 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0858-0016 39 4447 100 0.75 0.26 0.36 -2.73 0.12 0.19 2.35 0.14 0.24 4.84 0.21 0.27 -0.80 0.20 0.28 1 1 5.09 0.11 0.19 0.26 0.15 0.23 7 4 3.31 0.17 0.26 -0.41 0.18 0.27 1 1 3.80 0.12 0.20 0.19 0.15 0.25 9 7 0.38 0.15 0.21 -0.04 0.15 0.24 5 5 2.45 0.12 0.18 0.18 0.15 0.23 17 17 1.05 0.16 0.20 -0.21 0.16 0.24 3 1 2.49 0.22 0.30 -0.43 0.20 0.28 3 3 2.31 0.16 0.21 -0.33 0.16 0.23 5 4 4.75 0.12 0.19 0.00 0.14 0.22 55 47 2.13 0.16 0.24 -0.04 0.16 0.25 6 6 3.99 0.23 0.32 0.49 0.21 0.29 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.48 0.25 0.35 -0.70 0.24 0.33 3 1 -1.12 0.18 0.23 -0.61 0.16 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.16 0.24 0.30 -0.54 0.22 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.25 0.19 0.23 -0.01 0.17 0.26 4 3
HE 0926-0508 124 6249 100 4.24 0.25 0.35 -2.78 0.12 0.17 1.60 0.12 0.22 6.23 0.14 0.23 0.62 0.16 0.27 1 1 5.08 0.12 0.18 0.28 0.14 0.23 7 1 2.79 0.13 0.20 -0.90 0.14 0.24 1 1 3.96 0.11 0.19 0.37 0.14 0.24 9 3 0.67 0.17 0.22 0.28 0.15 0.25 5 1 2.73 0.15 0.21 0.49 0.15 0.24 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.75 0.14 0.19 -0.14 0.15 0.22 3 3 2.07 0.14 0.19 -0.54 0.15 0.23 5 2 4.72 0.12 0.17 0.00 0.14 0.22 55 33 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.42 0.14 0.19 -0.06 0.15 0.22 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.17 0.18 0.26 -0.02 0.17 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.92 0.18 0.22 -0.28 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0938+0114 307 6777 100 4.89 0.23 0.33 -2.51 0.12 0.17 1.76 0.11 0.21 6.54 0.14 0.22 0.65 0.16 0.27 1 1 5.29 0.11 0.17 0.22 0.14 0.23 7 1 3.18 0.12 0.20 -0.79 0.14 0.24 1 1 4.22 0.11 0.19 0.37 0.15 0.24 9 3 1.12 0.16 0.22 0.46 0.15 0.24 5 1 3.05 0.15 0.21 0.53 0.14 0.23 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.13 0.13 0.18 -0.03 0.14 0.22 3 3 2.45 0.12 0.17 -0.43 0.14 0.22 5 1 4.99 0.12 0.17 0.00 0.14 0.22 55 30 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.78 0.14 0.18 0.04 0.14 0.22 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.38 0.17 0.24 -0.08 0.16 0.26 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.48 0.17 0.21 -0.10 0.15 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 0951-1152 41 5349 100 4.75 0.25 0.35 -2.62 0.14 0.18 1.42 0.17 0.27 5.88 0.24 0.28 0.10 0.19 0.27 1 1 5.50 0.14 0.20 0.54 0.14 0.24 7 3 3.80 0.13 0.22 -0.05 0.16 0.26 1 1 3.99 0.13 0.21 0.25 0.14 0.24 9 7 0.82 0.19 0.24 0.27 0.16 0.26 5 2 2.66 0.17 0.22 0.25 0.16 0.25 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.07 0.14 0.20 0.02 0.15 0.23 3 3 2.58 0.15 0.20 -0.19 0.15 0.23 5 3 4.88 0.14 0.18 0.00 0.14 0.22 55 37 2.47 0.17 0.23 0.17 0.15 0.25 6 5 3.53 0.15 0.20 -0.10 0.15 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.15 0.19 0.25 -0.51 0.17 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.40 0.20 0.26 0.09 0.17 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1006-2218 65 6638 100 4.62 0.30 0.40 -2.69 0.13 0.18 1.79 0.16 0.26 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 2.99 0.13 0.20 -0.79 0.15 0.25 1 1 3.99 0.12 0.20 0.32 0.15 0.25 9 2 0.83 0.18 0.23 0.35 0.16 0.25 5 1 2.81 0.17 0.22 0.48 0.16 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.87 0.13 0.18 -0.11 0.15 0.23 3 3 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.81 0.13 0.18 0.00 0.14 0.22 55 22 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.13 0.19 0.26 -0.15 0.17 0.26 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1015-0027 47 6315 100 4.40 0.27 0.37 -2.66 0.12 0.17 1.43 0.15 0.25 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 5.27 0.12 0.18 0.35 0.15 0.24 7 1 2.81 0.14 0.21 -1.00 0.16 0.25 1 1 4.11 0.11 0.19 0.41 0.15 0.25 9 3 0.79 0.18 0.23 0.28 0.17 0.26 5 1 2.91 0.16 0.21 0.55 0.16 0.25 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.78 0.14 0.19 -0.24 0.15 0.23 3 3 2.29 0.15 0.20 -0.45 0.16 0.24 5 1 4.85 0.12 0.17 0.00 0.14 0.22 55 27 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.50 0.15 0.19 -0.10 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.75 0.20 0.28 0.44 0.19 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1044-2509 51 5227 100 2.78 0.26 0.36 -2.89 0.12 0.18 1.84 0.14 0.24 6.03 0.19 0.26 0.52 0.18 0.28 1 1 4.99 0.11 0.19 0.29 0.16 0.25 7 6 3.00 0.13 0.24 -0.59 0.16 0.26 1 1 3.85 0.12 0.20 0.37 0.15 0.25 9 7 0.54 0.18 0.23 0.25 0.16 0.26 5 4 2.37 0.16 0.22 0.24 0.15 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.63 0.17 0.24 -0.16 0.16 0.24 3 3 1.99 0.17 0.22 -0.52 0.16 0.24 5 3 4.62 0.12 0.18 0.00 0.14 0.22 55 40 2.28 0.16 0.22 0.25 0.15 0.25 6 5 3.42 0.18 0.25 0.05 0.17 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.32 0.20 0.29 0.23 0.18 0.28 3 2 -0.46 0.19 0.24 0.18 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.52 0.21 0.26 0.24 0.19 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.44 0.18 0.23 0.94 0.17 0.26 4 1
HE 1052-2548 93 6534 100 4.52 0.25 0.35 -2.29 0.12 0.17 1.57 0.13 0.23 6.61 0.14 0.22 0.51 0.17 0.26 1 1 5.45 0.11 0.17 0.16 0.14 0.23 7 1 3.70 0.12 0.21 -0.48 0.15 0.25 1 1 4.34 0.11 0.19 0.27 0.14 0.24 9 7 1.14 0.17 0.22 0.27 0.16 0.25 5 2 3.17 0.15 0.20 0.45 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.26 0.13 0.18 -0.12 0.15 0.22 3 3 2.62 0.14 0.19 -0.48 0.15 0.23 5 3 5.21 0.12 0.17 0.00 0.14 0.22 55 35 2.88 0.14 0.21 0.25 0.16 0.25 6 1 3.99 0.15 0.19 0.03 0.15 0.22 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.93 0.18 0.27 0.26 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.71 0.18 0.23 0.88 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1054-0059 38 4601 100 1.19 0.27 0.37 -3.34 0.13 0.18 2.21 0.14 0.24 4.32 0.22 0.29 -0.73 0.20 0.29 1 1 4.51 0.13 0.19 0.27 0.15 0.23 7 4 2.36 0.21 0.29 -0.77 0.23 0.31 1 1 3.26 0.12 0.20 0.24 0.15 0.24 9 3 -0.04 0.17 0.22 0.12 0.16 0.25 5 3 1.88 0.16 0.21 0.20 0.15 0.23 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.69 0.16 0.22 -0.64 0.16 0.24 3 3 1.43 0.16 0.22 -0.62 0.16 0.24 5 3 4.16 0.13 0.18 0.00 0.14 0.22 55 40 1.80 0.16 0.22 0.22 0.15 0.24 6 5 2.93 0.19 0.27 0.01 0.19 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.08 0.23 0.32 -0.71 0.22 0.32 3 2 -1.43 0.20 0.24 -0.33 0.18 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.42 0.19 0.23 -1.21 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1059-0118 49 5560 100 4.30 0.25 0.35 -2.81 0.12 0.18 1.28 0.18 0.28 5.95 0.19 0.25 0.37 0.17 0.26 1 1 5.24 0.12 0.18 0.46 0.15 0.24 7 3 2.93 0.14 0.22 -0.73 0.16 0.25 1 1 3.86 0.12 0.20 0.31 0.14 0.24 9 7 0.50 0.18 0.23 0.14 0.18 0.28 5 2 2.42 0.16 0.21 0.21 0.16 0.27 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.51 0.14 0.20 -0.36 0.15 0.23 3 3 2.14 0.17 0.22 -0.45 0.17 0.25 5 2 4.70 0.12 0.18 0.00 0.14 0.22 55 35 2.44 0.15 0.22 0.32 0.16 0.25 6 3 3.55 0.15 0.21 0.11 0.16 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.34 0.19 0.26 -0.50 0.19 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1100-0137 50 6101 100 4.25 0.32 0.42 -2.92 0.13 0.18 1.29 0.17 0.27 5.96 0.21 0.28 0.47 0.22 0.30 1 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 2.39 0.14 0.21 -1.17 0.16 0.26 1 1 3.67 0.12 0.20 0.22 0.15 0.25 9 2 0.49 0.18 0.23 0.22 0.18 0.27 5 1 2.37 0.17 0.23 0.25 0.17 0.27 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.38 0.15 0.19 -0.39 0.15 0.23 3 3 2.19 0.15 0.20 -0.30 0.16 0.24 5 2 4.60 0.13 0.18 0.00 0.14 0.22 55 23 2.57 0.15 0.21 0.55 0.16 0.25 6 1 3.27 0.16 0.20 -0.07 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 0.65 0.20 0.25 2.05 0.19 0.28 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1105+0027 43 6132 100 3.45 0.25 0.35 -2.42 0.13 0.19 1.52 0.14 0.24 7.97 0.15 0.23 2.00 0.17 0.28 1 1 5.63 0.11 0.17 0.47 0.16 0.24 7 2 3.16 0.15 0.22 -0.89 0.17 0.26 1 1 4.41 0.12 0.20 0.47 0.15 0.25 9 6 1.03 0.17 0.22 0.28 0.15 0.23 5 2 2.92 0.15 0.21 0.32 0.15 0.23 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.30 0.16 0.22 0.05 0.15 0.23 3 3 2.46 0.15 0.20 -0.51 0.15 0.24 5 3 5.08 0.13 0.19 0.00 0.14 0.22 55 34 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.54 0.16 0.20 -0.29 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.28 0.20 0.29 0.73 0.18 0.28 3 2 0.57 0.18 0.23 0.75 0.16 0.24 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.16 0.11 0.18 2.45 0.16 0.23 2 2 0.85 0.17 0.22 2.10 0.15 0.24 6 4 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 1.14 0.18 0.23 2.06 0.16 0.24 9 4 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.10 0.18 0.23 1.81 0.16 0.24 4 4
HE 1120-0153 194 6191 100 4.09 0.24 0.34 -2.77 0.11 0.17 0.68 0.12 0.22 6.26 0.16 0.23 0.63 0.17 0.26 1 1 4.86 0.11 0.17 0.04 0.14 0.23 7 1 2.64 0.13 0.20 -1.07 0.14 0.25 1 1 3.80 0.11 0.19 0.20 0.15 0.24 9 2 0.61 0.16 0.22 0.20 0.15 0.25 5 1 2.56 0.15 0.21 0.30 0.15 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.69 0.14 0.19 -0.22 0.15 0.22 3 3 1.94 0.14 0.19 -0.69 0.15 0.23 5 1 4.74 0.11 0.17 0.00 0.14 0.22 55 34 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.30 0.14 0.19 -0.19 0.15 0.22 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.03 0.18 0.25 -0.18 0.17 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.76 0.15 0.20 -0.13 0.15 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1122-1429 44 5787 100 3.29 0.27 0.37 -2.65 0.13 0.18 1.54 0.15 0.25 6.18 0.18 0.25 0.44 0.18 0.28 1 1 5.26 0.11 0.17 0.34 0.16 0.24 7 2 2.89 0.15 0.22 -0.92 0.16 0.26 1 1 4.21 0.11 0.20 0.50 0.15 0.25 9 7 0.55 0.18 0.23 0.04 0.16 0.25 5 2 2.67 0.17 0.23 0.30 0.16 0.24 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.74 0.15 0.20 -0.27 0.15 0.23 3 3 2.00 0.15 0.20 -0.74 0.15 0.23 5 2 4.85 0.13 0.18 0.00 0.14 0.22 55 32 2.41 0.16 0.22 0.14 0.15 0.25 6 1 3.27 0.19 0.22 -0.32 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.26 0.23 0.33 -0.05 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.87 0.19 0.23 -0.34 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1124-2335 48 5226 100 2.68 0.26 0.36 -2.95 0.14 0.19 1.65 0.13 0.23 6.31 0.19 0.26 0.86 0.18 0.28 1 1 5.00 0.11 0.19 0.35 0.19 0.27 7 6 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.62 0.12 0.20 0.19 0.15 0.25 9 7 0.41 0.16 0.21 0.18 0.15 0.23 5 4 2.43 0.16 0.21 0.34 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.69 0.17 0.24 -0.05 0.16 0.24 3 3 2.18 0.16 0.21 -0.28 0.15 0.23 5 3 4.57 0.14 0.19 0.00 0.14 0.22 55 42 2.34 0.16 0.22 0.35 0.15 0.24 6 6 3.56 0.18 0.27 0.25 0.17 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.12 0.22 0.32 0.09 0.19 0.30 3 2 -0.68 0.19 0.23 0.01 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.86 0.19 0.23 -1.06 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1126-1735 46 5689 100 3.31 0.28 0.38 -2.69 0.13 0.18 1.55 0.15 0.25 5.93 0.18 0.25 0.23 0.18 0.28 1 1 5.20 0.11 0.17 0.31 0.16 0.24 7 3 2.72 0.13 0.21 -1.06 0.15 0.24 1 1 4.00 0.12 0.20 0.32 0.15 0.25 9 5 0.55 0.18 0.23 0.07 0.16 0.25 5 2 2.66 0.16 0.22 0.33 0.15 0.24 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.69 0.18 0.22 -0.29 0.16 0.23 3 3 1.99 0.16 0.20 -0.71 0.15 0.23 5 3 4.81 0.13 0.18 0.00 0.14 0.22 55 34 2.35 0.15 0.22 0.12 0.15 0.25 6 2 3.53 0.13 0.24 -0.04 0.17 0.26 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.11 0.22 0.32 -0.17 0.20 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.02 0.19 0.24 -0.46 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1127-1143 49 5224 100 2.64 0.25 0.35 -2.73 0.14 0.19 1.59 0.14 0.24 6.21 0.19 0.25 0.54 0.17 0.27 1 1 5.08 0.11 0.18 0.22 0.16 0.25 7 6 2.87 0.16 0.25 -0.87 0.17 0.26 1 1 3.89 0.12 0.20 0.26 0.15 0.25 9 8 0.57 0.18 0.23 0.13 0.15 0.24 5 4 2.48 0.16 0.21 0.19 0.14 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.65 0.17 0.24 -0.29 0.15 0.24 3 3 1.92 0.17 0.22 -0.75 0.15 0.23 5 2 4.78 0.14 0.19 0.00 0.14 0.22 55 46 2.48 0.16 0.22 0.28 0.15 0.24 6 6 3.71 0.20 0.28 0.19 0.17 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.49 0.22 0.30 0.24 0.19 0.28 3 1 -0.27 0.19 0.24 0.22 0.16 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.03 0.22 0.29 0.63 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.37 0.19 0.23 0.86 0.16 0.24 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.14 0.18 0.23 1.08 0.15 0.24 4 3
HE 1128-0823 65 5909 100 3.71 0.25 0.35 -2.71 0.13 0.18 1.49 0.13 0.23 6.15 0.17 0.24 0.47 0.17 0.27 1 1 5.10 0.12 0.18 0.23 0.15 0.23 7 2 2.79 0.14 0.21 -0.97 0.15 0.25 1 1 3.99 0.11 0.20 0.34 0.15 0.25 9 7 0.71 0.17 0.23 0.25 0.16 0.24 5 2 2.73 0.15 0.20 0.42 0.15 0.23 17 7 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.66 0.15 0.19 -0.30 0.15 0.22 3 3 1.96 0.15 0.20 -0.72 0.15 0.23 5 3 4.79 0.13 0.18 0.00 0.14 0.22 55 37 2.40 0.14 0.21 0.20 0.15 0.24 6 2 3.55 0.22 0.26 0.01 0.19 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.28 0.17 0.28 0.02 0.17 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.74 0.18 0.23 -0.16 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1131+0141 45 5236 100 2.98 0.25 0.35 -2.48 0.13 0.18 1.63 0.14 0.24 6.02 0.20 0.25 0.12 0.17 0.26 1 1 5.33 0.12 0.18 0.23 0.15 0.23 7 5 3.15 0.18 0.26 -0.84 0.21 0.29 1 1 4.15 0.12 0.20 0.28 0.15 0.24 9 8 0.67 0.18 0.24 -0.01 0.16 0.26 5 3 2.71 0.17 0.22 0.18 0.16 0.25 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.94 0.16 0.25 -0.25 0.16 0.25 3 3 2.44 0.17 0.22 -0.47 0.16 0.24 5 3 5.01 0.13 0.18 0.00 0.14 0.22 55 49 2.38 0.16 0.22 -0.05 0.15 0.25 6 5 3.72 0.18 0.27 -0.04 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.63 0.17 0.25 0.15 0.17 0.26 3 2 -0.18 0.18 0.23 0.07 0.16 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.17 0.19 0.25 0.52 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.10 0.18 0.23 0.87 0.16 0.26 4 3
HE 1132+0125 50 5732 100 3.54 0.26 0.36 -2.42 0.11 0.18 1.41 0.13 0.23 6.25 0.18 0.24 0.24 0.20 0.28 1 1 5.58 0.11 0.18 0.38 0.15 0.24 7 5 3.09 0.15 0.23 -1.00 0.17 0.26 1 1 4.29 0.11 0.20 0.31 0.15 0.25 9 7 0.83 0.18 0.23 0.04 0.18 0.28 5 3 2.83 0.16 0.21 0.19 0.17 0.26 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.07 0.17 0.23 -0.22 0.17 0.25 3 3 2.15 0.16 0.21 -0.86 0.18 0.26 5 2 5.12 0.11 0.18 0.00 0.14 0.22 55 44 2.58 0.15 0.21 0.04 0.17 0.26 6 3 3.62 0.18 0.23 -0.25 0.18 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.56 0.19 0.29 -0.03 0.19 0.29 3 2 -0.19 0.18 0.23 -0.05 0.19 0.28 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.41 0.19 0.24 -0.16 0.19 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1132+0204 42 5046 100 2.25 0.25 0.35 -2.55 0.11 0.18 1.68 0.13 0.23 5.99 0.20 0.26 0.13 0.20 0.29 1 1 5.25 0.12 0.18 0.20 0.15 0.24 7 6 2.90 0.19 0.27 -1.04 0.20 0.28 1 1 4.01 0.11 0.20 0.18 0.14 0.25 9 8 0.59 0.15 0.21 -0.05 0.15 0.25 5 4 2.56 0.16 0.21 0.07 0.16 0.25 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.93 0.19 0.28 -0.21 0.19 0.27 3 3 2.32 0.17 0.23 -0.54 0.17 0.25 5 3 4.97 0.11 0.18 0.00 0.14 0.22 54 52 2.54 0.16 0.22 0.15 0.16 0.26 6 6 3.73 0.19 0.30 0.01 0.19 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.22 0.21 0.32 -0.22 0.21 0.31 3 2 -0.70 0.19 0.24 -0.41 0.18 0.27 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.09 0.21 0.26 -0.69 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.77 0.19 0.23 0.25 0.18 0.28 4 1
HE 1135+0139 47 5487 100 1.80 0.26 0.36 -2.33 0.13 0.18 2.66 0.12 0.22 7.28 0.17 0.25 1.19 0.19 0.29 1 1 5.60 0.11 0.17 0.33 0.15 0.24 7 7 3.28 0.17 0.24 -0.89 0.17 0.26 1 1 4.44 0.12 0.20 0.38 0.15 0.25 9 8 1.02 0.18 0.23 0.15 0.16 0.24 5 5 2.86 0.18 0.23 0.14 0.16 0.25 17 15 1.72 0.16 0.21 0.03 0.16 0.24 3 1 3.13 0.14 0.21 -0.24 0.14 0.22 3 3 2.64 0.16 0.21 -0.44 0.16 0.23 5 2 5.19 0.13 0.18 0.00 0.14 0.22 55 47 2.76 0.17 0.23 0.14 0.17 0.26 6 5 3.95 0.14 0.21 0.01 0.15 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.32 0.18 0.25 0.66 0.17 0.26 3 1 0.29 0.18 0.23 0.36 0.16 0.24 6 6 0.75 0.16 0.21 0.46 0.15 0.24 3 1 0.95 0.18 0.23 1.13 0.16 0.24 2 2 -0.21 0.18 0.23 0.93 0.16 0.25 6 4 0.45 0.18 0.25 1.17 0.16 0.27 10 6 -0.03 0.18 0.23 0.77 0.16 0.25 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.46 0.18 0.23 0.33 0.16 0.25 4 1
HE 1135-0344 45 6154 100 4.03 0.31 0.41 -2.63 0.12 0.18 1.17 0.17 0.27 6.80 0.16 0.24 1.03 0.17 0.27 1 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 2.58 0.15 0.22 -1.26 0.17 0.26 1 1 4.00 0.12 0.20 0.27 0.15 0.25 9 3 0.72 0.18 0.24 0.18 0.18 0.26 5 1 2.84 0.16 0.21 0.45 0.16 0.25 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.82 0.15 0.20 -0.22 0.15 0.23 3 3 2.09 0.15 0.20 -0.67 0.16 0.24 5 1 4.87 0.12 0.18 0.00 0.14 0.22 55 29 2.60 0.16 0.22 0.30 0.16 0.26 6 1 3.48 0.16 0.20 -0.14 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.72 0.22 0.31 0.38 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1148-0037 76 5964 100 4.16 0.35 0.45 -3.47 0.13 0.18 0.81 0.20 0.30 5.76 0.20 0.27 0.84 0.19 0.29 1 1 4.03 0.41 0.44 -0.09 0.35 0.40 7 1 1.98 0.14 0.21 -1.02 0.16 0.26 1 1 2.95 0.17 0.23 0.06 0.16 0.26 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 1.97 0.18 0.23 0.41 0.18 0.27 17 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.03 0.13 0.18 0.00 0.14 0.22 55 18 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 2.52 0.20 0.23 -0.26 0.18 0.25 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.92 0.19 0.26 -0.42 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1207-2031 50 6281 100 4.40 0.30 0.40 -2.82 0.12 0.17 1.42 0.16 0.26 6.21 0.19 0.26 0.64 0.19 0.28 1 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 2.70 0.14 0.21 -0.96 0.15 0.25 1 1 4.05 0.11 0.20 0.50 0.15 0.25 9 3 0.78 0.18 0.23 0.43 0.17 0.26 5 1 2.75 0.16 0.22 0.54 0.16 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.65 0.14 0.19 -0.20 0.15 0.23 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.68 0.12 0.17 0.00 0.14 0.22 55 24 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.29 0.15 0.19 -0.14 0.15 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.01 0.19 0.26 -0.16 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1210+0048 49 6028 100 3.73 0.27 0.37 -2.28 0.11 0.18 1.56 0.14 0.24 6.70 0.16 0.23 0.57 0.18 0.28 1 1 5.57 0.12 0.18 0.25 0.15 0.25 7 3 3.06 0.15 0.22 -1.15 0.17 0.26 1 1 4.42 0.11 0.20 0.32 0.15 0.25 9 7 0.98 0.18 0.23 0.07 0.18 0.27 5 1 3.08 0.16 0.21 0.32 0.16 0.25 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.27 0.16 0.22 -0.14 0.16 0.24 3 3 2.46 0.15 0.20 -0.67 0.17 0.25 5 2 5.24 0.11 0.18 0.00 0.14 0.22 55 41 2.80 0.15 0.21 0.14 0.16 0.26 6 2 3.75 0.17 0.21 -0.24 0.17 0.24 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.64 0.22 0.32 -0.07 0.21 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.18 0.19 0.24 -0.05 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 0.61 0.18 0.23 1.37 0.18 0.28 9 1 1.06 0.19 0.24 2.31 0.19 0.28 8 1 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1210-1956 50 5790 100 3.30 0.27 0.37 -2.57 0.13 0.18 1.52 0.14 0.24 6.04 0.21 0.26 0.22 0.19 0.28 1 1 5.42 0.12 0.18 0.41 0.15 0.23 7 4 2.94 0.14 0.22 -0.96 0.16 0.25 1 1 4.32 0.11 0.20 0.53 0.15 0.25 9 7 0.56 0.18 0.23 -0.04 0.16 0.24 5 2 2.78 0.16 0.22 0.33 0.15 0.23 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.92 0.16 0.21 -0.18 0.15 0.23 3 3 2.15 0.16 0.20 -0.68 0.15 0.23 5 2 4.93 0.13 0.18 0.00 0.14 0.22 55 41 2.40 0.15 0.21 0.05 0.15 0.25 6 3 3.43 0.16 0.21 -0.25 0.15 0.22 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.44 0.23 0.32 0.04 0.20 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.86 0.19 0.23 -0.43 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1212-0127 30 4915 100 1.85 0.26 0.36 -2.15 0.13 0.19 1.87 0.14 0.24 5.85 0.20 0.26 -0.39 0.18 0.27 1 1 5.55 0.12 0.19 0.13 0.15 0.24 7 5 3.77 0.23 0.30 -0.54 0.24 0.31 1 1 4.35 0.12 0.21 0.15 0.15 0.25 9 8 0.95 0.15 0.22 -0.07 0.16 0.24 5 5 2.91 0.18 0.24 0.05 0.16 0.25 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.19 0.20 0.33 -0.33 0.21 0.31 3 3 2.82 0.15 0.20 -0.42 0.15 0.24 5 3 5.34 0.13 0.19 0.00 0.14 0.22 55 54 2.65 0.17 0.24 -0.11 0.16 0.25 6 6 3.53 0.26 0.34 -0.56 0.24 0.32 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.62 0.19 0.26 -0.20 0.18 0.26 3 2 -0.23 0.17 0.22 -0.31 0.16 0.26 6 3 0.56 0.19 0.23 0.11 0.17 0.27 3 1 -0.34 0.27 0.35 -0.32 0.27 0.34 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.30 0.18 0.23 0.35 0.16 0.27 4 3
HE 1214-1819 53 4916 100 1.88 0.26 0.36 -3.01 0.12 0.18 1.74 0.13 0.23 5.74 0.20 0.26 0.35 0.19 0.28 1 1 4.96 0.12 0.19 0.39 0.15 0.24 7 5 2.73 0.19 0.27 -0.74 0.20 0.29 1 1 3.70 0.12 0.20 0.34 0.15 0.25 9 8 0.33 0.18 0.23 0.16 0.16 0.25 5 4 2.30 0.16 0.21 0.28 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.35 0.17 0.24 -0.32 0.16 0.24 3 3 1.71 0.17 0.21 -0.68 0.16 0.23 5 3 4.50 0.12 0.18 0.00 0.14 0.22 55 47 2.13 0.16 0.22 0.22 0.15 0.24 6 5 3.46 0.19 0.28 0.21 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.23 0.17 0.29 0.27 0.18 0.29 3 2 -0.65 0.19 0.23 0.11 0.16 0.25 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.92 0.22 0.28 -0.04 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.00 0.19 0.23 0.49 0.16 0.26 4 1
HE 1215+0149 35 5098 100 2.37 0.27 0.37 -2.90 0.13 0.19 1.48 0.14 0.24 5.65 0.20 0.26 0.15 0.19 0.28 1 1 5.03 0.12 0.19 0.35 0.16 0.24 7 6 3.10 0.20 0.28 -0.47 0.21 0.29 1 1 3.74 0.12 0.20 0.27 0.15 0.25 9 5 0.33 0.18 0.23 0.06 0.16 0.26 5 4 2.48 0.17 0.22 0.36 0.16 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.27 0.18 0.24 -0.51 0.17 0.24 3 2 1.77 0.17 0.22 -0.72 0.16 0.24 5 3 4.60 0.13 0.19 0.00 0.14 0.22 55 42 2.25 0.16 0.22 0.23 0.16 0.25 6 5 3.50 0.22 0.30 0.15 0.20 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.36 0.20 0.30 0.29 0.19 0.29 3 2 -0.71 0.20 0.24 -0.05 0.18 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.53 0.20 0.24 -0.76 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1217-0540 45 5700 100 4.20 0.27 0.37 -2.95 0.12 0.18 1.41 0.17 0.27 6.26 0.17 0.24 0.81 0.17 0.26 1 1 5.06 0.12 0.18 0.42 0.15 0.24 7 1 2.82 0.14 0.22 -0.71 0.16 0.25 1 1 3.67 0.12 0.20 0.25 0.15 0.25 9 3 0.24 0.18 0.23 0.01 0.18 0.28 5 1 2.34 0.16 0.22 0.27 0.17 0.27 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.55 0.16 0.20 -0.18 0.16 0.23 3 3 1.82 0.16 0.21 -0.62 0.16 0.25 5 3 4.56 0.12 0.18 0.00 0.14 0.22 54 30 2.27 0.16 0.22 0.30 0.16 0.26 6 2 3.21 0.16 0.20 -0.09 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.16 0.20 0.28 0.13 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1219-0312 46 5140 100 2.40 0.26 0.36 -2.81 0.12 0.18 1.54 0.13 0.23 5.51 0.19 0.26 -0.08 0.19 0.28 1 1 4.82 0.11 0.19 0.04 0.16 0.24 7 4 2.56 0.17 0.24 -1.11 0.17 0.26 1 1 3.53 0.11 0.20 -0.03 0.15 0.25 9 6 0.31 0.18 0.23 -0.07 0.17 0.25 5 4 2.21 0.16 0.21 -0.01 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.35 0.16 0.23 -0.52 0.16 0.24 3 3 2.10 0.25 0.42 -0.49 0.32 0.44 5 3 4.70 0.12 0.18 0.00 0.14 0.22 55 44 2.14 0.16 0.22 0.02 0.16 0.25 6 4 3.41 0.19 0.26 -0.05 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.38 0.18 0.27 0.20 0.18 0.27 3 2 -0.27 0.19 0.24 0.29 0.17 0.26 6 4 0.45 0.19 0.23 0.65 0.17 0.26 3 1 -0.16 0.29 0.35 0.51 0.25 0.33 2 1 -0.72 0.18 0.23 0.91 0.17 0.26 6 4 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.31 0.19 0.23 0.98 0.17 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.87 0.19 0.23 1.41 0.17 0.26 4 3
HE 1221-0522 44 5789 100 4.04 0.28 0.38 -2.84 0.12 0.17 1.29 0.17 0.27 6.08 0.18 0.24 0.53 0.17 0.26 1 1 5.19 0.11 0.18 0.45 0.15 0.23 7 2 2.96 0.15 0.23 -0.67 0.16 0.26 1 1 3.99 0.11 0.20 0.47 0.15 0.25 9 5 0.47 0.18 0.24 0.14 0.18 0.27 5 1 2.49 0.16 0.21 0.31 0.16 0.25 17 4 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.61 0.15 0.20 -0.22 0.15 0.23 3 3 1.98 0.16 0.20 -0.57 0.16 0.24 5 3 4.66 0.12 0.17 0.00 0.14 0.22 55 32 2.41 0.16 0.22 0.32 0.16 0.25 6 2 3.45 0.16 0.21 0.04 0.16 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.32 0.20 0.27 -0.46 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1221-1948 57 6083 100 3.81 0.28 0.38 -3.36 0.13 0.18 1.65 0.15 0.25 6.46 0.22 0.28 1.42 0.22 0.31 1 1 5.02 0.13 0.19 0.80 0.15 0.24 7 1 2.39 0.14 0.21 -0.72 0.16 0.25 1 1 3.81 0.12 0.20 0.81 0.15 0.25 9 3 0.10 0.18 0.23 0.29 0.17 0.26 5 1 2.19 0.16 0.22 0.52 0.16 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.12 0.14 0.19 -0.19 0.15 0.23 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.14 0.13 0.18 0.00 0.14 0.22 55 18 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 2.79 0.15 0.19 -0.10 0.16 0.23 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1222-0200 45 5288 100 2.72 0.26 0.36 -2.45 0.13 0.19 1.50 0.14 0.24 6.18 0.19 0.25 0.23 0.18 0.27 1 1 5.31 0.12 0.18 0.17 0.15 0.24 7 5 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 4.20 0.12 0.20 0.29 0.14 0.24 9 8 0.68 0.18 0.24 -0.04 0.16 0.26 5 4 2.71 0.17 0.22 0.14 0.15 0.24 17 14 1.99 0.16 0.20 0.43 0.15 0.24 3 3 3.36 0.18 0.28 0.13 0.17 0.26 3 3 2.54 0.14 0.26 -0.41 0.19 0.28 5 3 5.06 0.13 0.19 0.00 0.14 0.22 55 47 2.78 0.16 0.22 0.31 0.15 0.24 6 6 3.92 0.19 0.29 0.12 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.40 0.20 0.31 -0.13 0.19 0.30 3 2 -0.42 0.19 0.24 -0.22 0.17 0.26 6 2 0.79 0.18 0.23 0.64 0.17 0.26 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.34 0.19 0.23 0.60 0.16 0.26 4 1
HE 1222-0336 46 6052 100 3.96 0.25 0.35 -2.04 0.11 0.17 1.30 0.14 0.24 6.57 0.15 0.23 0.22 0.16 0.26 1 1 5.63 0.11 0.17 0.09 0.15 0.23 7 3 3.14 0.15 0.22 -1.28 0.16 0.25 1 1 4.58 0.11 0.20 0.26 0.15 0.25 9 8 1.15 0.17 0.23 0.02 0.17 0.26 5 2 3.27 0.16 0.21 0.29 0.16 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.48 0.16 0.23 -0.14 0.16 0.24 3 3 2.84 0.16 0.20 -0.51 0.16 0.24 5 3 5.46 0.11 0.17 0.00 0.14 0.22 55 45 2.79 0.15 0.21 -0.09 0.16 0.25 6 2 4.11 0.18 0.25 -0.10 0.19 0.26 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.60 0.20 0.29 -0.33 0.20 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.11 0.19 0.24 -0.20 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1225+0155 100 4842 100 1.80 0.23 0.33 -2.75 0.12 0.18 1.85 0.11 0.21 5.90 0.20 0.26 0.26 0.19 0.28 1 1 5.30 0.12 0.18 0.46 0.15 0.23 7 6 3.18 0.12 0.24 -0.54 0.15 0.25 1 1 3.98 0.13 0.21 0.37 0.14 0.25 9 9 0.56 0.17 0.22 0.14 0.15 0.24 5 5 2.58 0.16 0.21 0.30 0.15 0.23 17 17 1.26 0.15 0.19 0.00 0.15 0.23 3 2 2.67 0.15 0.26 -0.25 0.15 0.25 3 3 2.17 0.14 0.21 -0.48 0.15 0.23 5 4 4.75 0.12 0.18 0.00 0.14 0.22 55 54 2.32 0.16 0.23 0.15 0.15 0.24 6 6 3.33 0.14 0.26 -0.18 0.15 0.26 4 4 2.11 0.13 0.20 0.26 0.14 0.25 2 2 0.30 0.17 0.26 0.07 0.16 0.26 3 2 -0.67 0.17 0.22 -0.17 0.15 0.24 6 6 0.16 0.17 0.22 0.30 0.15 0.24 3 2 -1.07 0.20 0.26 -0.45 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.99 0.18 0.23 0.25 0.15 0.25 4 3
HE 1225-0515 41 6210 100 3.81 0.27 0.37 -1.96 0.13 0.18 1.35 0.15 0.25 6.94 0.16 0.23 0.52 0.17 0.27 1 1 5.80 0.12 0.18 0.18 0.15 0.24 7 3 3.51 0.16 0.24 -1.00 0.18 0.26 1 1 4.67 0.11 0.20 0.27 0.15 0.25 9 8 1.22 0.17 0.23 0.02 0.16 0.25 5 3 3.40 0.15 0.21 0.34 0.15 0.23 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.62 0.17 0.23 -0.08 0.16 0.24 3 3 2.93 0.15 0.20 -0.50 0.15 0.23 5 3 5.54 0.13 0.18 0.00 0.14 0.22 55 44 3.01 0.15 0.21 0.05 0.15 0.25 6 3 4.12 0.18 0.24 -0.16 0.17 0.24 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.82 0.23 0.32 -0.18 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.12 0.19 0.24 -0.29 0.17 0.25 2 1 0.44 0.18 0.23 1.24 0.17 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1230-1724 54 5952 100 3.98 0.24 0.34 -2.30 0.12 0.17 1.39 0.15 0.25 6.22 0.17 0.23 0.13 0.17 0.26 1 1 5.50 0.12 0.18 0.22 0.15 0.23 7 4 3.17 0.14 0.22 -1.00 0.16 0.25 1 1 4.36 0.11 0.20 0.30 0.14 0.24 9 8 0.86 0.18 0.23 -0.01 0.16 0.26 5 2 2.91 0.16 0.21 0.18 0.15 0.24 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.19 0.15 0.21 -0.19 0.16 0.23 3 3 2.42 0.16 0.20 -0.67 0.15 0.23 5 3 5.20 0.12 0.17 0.00 0.14 0.22 55 44 2.57 0.15 0.21 -0.05 0.15 0.25 6 2 3.72 0.20 0.24 -0.23 0.18 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 0.61 0.20 0.29 -0.07 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.34 0.18 0.23 -0.18 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1237-3103 48 4851 100 1.72 0.26 0.36 -2.91 0.13 0.18 2.04 0.13 0.23 5.42 0.20 0.27 -0.06 0.18 0.28 1 1 4.88 0.12 0.18 0.21 0.15 0.23 7 6 2.72 0.16 0.26 -0.84 0.18 0.28 1 1 3.69 0.12 0.20 0.24 0.15 0.25 9 8 0.31 0.18 0.23 0.05 0.16 0.24 5 4 2.30 0.15 0.20 0.19 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.22 0.17 0.23 -0.54 0.16 0.24 3 3 2.13 0.19 0.26 -0.35 0.17 0.25 5 3 4.59 0.13 0.18 0.00 0.14 0.22 55 50 2.25 0.16 0.22 0.24 0.15 0.24 6 6 3.29 0.17 0.26 -0.05 0.17 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.13 0.23 0.33 -0.19 0.21 0.32 3 2 -1.01 0.18 0.23 -0.34 0.16 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.38 0.22 0.27 -0.60 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1243-1425 50 5507 100 3.19 0.26 0.36 -2.67 0.12 0.18 1.11 0.15 0.25 6.23 0.18 0.25 0.51 0.18 0.27 1 1 5.13 0.12 0.18 0.22 0.15 0.24 7 2 2.74 0.16 0.23 -1.06 0.17 0.26 1 1 3.89 0.11 0.20 0.20 0.15 0.25 9 7 0.76 0.18 0.23 0.26 0.17 0.26 5 4 2.60 0.16 0.21 0.25 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.76 0.16 0.23 -0.25 0.16 0.24 3 3 1.83 0.16 0.20 -0.89 0.16 0.24 5 3 4.83 0.12 0.18 0.00 0.14 0.22 55 38 2.58 0.16 0.22 0.33 0.16 0.25 6 4 4.01 0.17 0.27 0.43 0.17 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.54 0.18 0.28 0.23 0.18 0.27 3 1 -0.14 0.19 0.24 0.28 0.18 0.27 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.94 0.20 0.24 -0.41 0.18 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1245-1616 47 6191 100 4.04 0.32 0.42 -2.98 0.13 0.18 1.53 0.17 0.27 6.19 0.21 0.28 0.77 0.26 0.34 1 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.88 0.12 0.20 0.50 0.15 0.25 9 3 0.39 0.19 0.24 0.19 0.17 0.26 5 1 2.61 0.17 0.23 0.57 0.16 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.56 0.15 0.19 -0.13 0.15 0.23 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.53 0.13 0.18 0.00 0.14 0.22 55 20 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.12 0.15 0.19 -0.15 0.16 0.23 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.26 0.22 0.30 0.26 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.56 0.19 0.24 0.28 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1246-1344 49 4853 100 1.65 0.27 0.37 -3.40 0.14 0.19 1.84 0.13 0.23 4.93 0.20 0.27 -0.06 0.19 0.29 1 1 4.68 0.12 0.19 0.50 0.15 0.24 7 5 2.33 0.17 0.25 -0.74 0.18 0.27 1 1 3.35 0.12 0.20 0.39 0.15 0.25 9 6 0.12 0.18 0.22 0.35 0.15 0.23 5 4 1.87 0.16 0.21 0.25 0.15 0.23 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.82 0.16 0.21 -0.45 0.15 0.23 3 3 1.08 0.17 0.21 -0.91 0.16 0.23 5 3 4.10 0.14 0.19 0.00 0.14 0.22 55 39 1.64 0.15 0.22 0.12 0.15 0.24 6 3 2.84 0.17 0.23 -0.01 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.68 0.19 0.26 -1.25 0.17 0.26 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1247-2114 54 5012 100 2.08 0.25 0.35 -2.61 0.12 0.18 1.67 0.12 0.22 6.10 0.19 0.26 0.32 0.18 0.28 1 1 5.21 0.11 0.19 0.25 0.15 0.24 7 7 2.89 0.16 0.25 -0.96 0.18 0.27 1 1 3.94 0.11 0.20 0.20 0.15 0.24 9 8 0.56 0.19 0.24 0.00 0.16 0.25 5 4 2.57 0.16 0.21 0.17 0.15 0.23 17 15 1.41 0.15 0.20 0.02 0.15 0.23 3 1 2.74 0.17 0.27 -0.32 0.17 0.26 3 3 2.36 0.15 0.21 -0.42 0.15 0.23 5 3 4.89 0.12 0.18 0.00 0.14 0.22 55 53 2.39 0.16 0.22 0.08 0.15 0.24 6 6 3.60 0.18 0.29 -0.04 0.18 0.29 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.72 0.14 0.22 0.37 0.15 0.24 3 2 -0.34 0.18 0.23 0.04 0.16 0.25 6 6 0.41 0.18 0.22 0.42 0.16 0.25 3 1 -0.91 0.22 0.28 -0.43 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.88 0.18 0.23 0.22 0.16 0.25 4 1
HE 1248-1800 43 5288 100 2.92 0.27 0.37 -2.89 0.14 0.19 1.47 0.14 0.24 6.02 0.19 0.25 0.53 0.17 0.27 1 1 4.95 0.11 0.20 0.27 0.16 0.25 7 4 2.87 0.18 0.26 -0.71 0.19 0.27 1 1 3.71 0.12 0.20 0.24 0.15 0.25 9 6 0.33 0.18 0.23 0.05 0.16 0.25 5 3 2.45 0.16 0.21 0.32 0.15 0.23 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.28 0.16 0.21 -0.50 0.15 0.22 3 3 1.83 0.17 0.21 -0.67 0.15 0.23 5 3 4.61 0.14 0.19 0.00 0.14 0.22 55 39 2.22 0.16 0.22 0.20 0.15 0.24 6 5 3.27 0.18 0.24 -0.09 0.16 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.18 0.23 0.33 -0.25 0.21 0.32 3 2 -0.85 0.19 0.24 -0.20 0.17 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.89 0.20 0.25 -0.12 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1249-2932 56 4718 100 1.52 0.24 0.34 -2.65 0.13 0.18 2.09 0.12 0.22 5.32 0.20 0.26 -0.41 0.18 0.27 1 1 5.03 0.12 0.18 0.11 0.15 0.23 7 6 3.07 0.17 0.26 -0.75 0.18 0.27 1 1 3.73 0.12 0.20 0.03 0.15 0.25 9 8 0.48 0.18 0.23 -0.03 0.16 0.24 5 5 2.44 0.16 0.21 0.07 0.15 0.23 17 16 1.31 0.15 0.19 -0.04 0.15 0.23 3 3 2.76 0.13 0.28 -0.26 0.15 0.27 3 3 2.57 0.14 0.19 -0.17 0.15 0.23 5 5 4.85 0.13 0.18 0.00 0.14 0.22 55 55 2.26 0.15 0.22 -0.00 0.15 0.24 6 6 3.93 0.16 0.28 0.33 0.16 0.27 4 4 2.42 0.13 0.20 0.47 0.14 0.25 2 2 -0.56 0.23 0.33 -0.88 0.21 0.31 3 1 -1.52 0.19 0.23 -1.11 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.73 0.18 0.23 -1.20 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1249-3121 47 5373 100 3.40 0.30 0.40 -3.23 0.14 0.19 1.58 0.18 0.28 7.01 0.18 0.26 1.86 0.17 0.27 1 1 4.61 0.14 0.23 0.26 0.20 0.29 5 3 2.43 0.31 0.36 -0.81 0.25 0.35 1 1 3.51 0.14 0.26 0.38 0.22 0.32 5 2 0.53 0.21 0.26 0.59 0.18 0.26 3 1 2.22 0.17 0.22 0.43 0.15 0.24 11 5 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 2.16 0.17 0.22 -0.28 0.16 0.23 1 1 1.67 0.19 0.23 -0.49 0.17 0.25 4 2 4.27 0.14 0.19 0.00 0.14 0.22 35 17 2.03 0.16 0.22 0.34 0.15 0.25 4 3 2.98 0.17 0.21 -0.03 0.15 0.22 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 -1.24 0.20 0.26 -0.98 0.17 0.27 2 2 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0
HE 1251-0104 53 5084 100 2.32 0.24 0.34 -2.73 0.13 0.18 1.58 0.13 0.23 5.91 0.19 0.25 0.25 0.18 0.27 1 1 4.91 0.11 0.18 0.06 0.15 0.24 7 6 2.62 0.16 0.24 -1.12 0.17 0.26 1 1 3.79 0.12 0.20 0.16 0.15 0.25 9 7 0.35 0.17 0.22 -0.09 0.15 0.24 5 4 2.46 0.16 0.21 0.17 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.55 0.17 0.25 -0.39 0.16 0.24 3 3 2.05 0.17 0.22 -0.61 0.15 0.23 5 3 4.77 0.13 0.18 0.00 0.14 0.22 55 50 2.28 0.16 0.22 0.09 0.15 0.24 6 5 3.55 0.18 0.28 0.03 0.17 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.02 0.21 0.31 -0.22 0.20 0.30 3 2 -0.85 0.19 0.24 -0.36 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.97 0.20 0.25 -0.37 0.18 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1252+0044 44 5296 100 2.98 0.29 0.39 -3.28 0.14 0.19 1.57 0.15 0.25 5.70 0.19 0.26 0.60 0.18 0.28 1 1 4.81 0.12 0.20 0.51 0.18 0.26 7 4 2.51 0.15 0.23 -0.68 0.16 0.25 1 1 3.56 0.12 0.20 0.48 0.15 0.25 9 3 -0.05 0.19 0.24 0.06 0.17 0.25 5 1 2.10 0.17 0.22 0.36 0.15 0.24 17 7 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.11 0.15 0.20 -0.28 0.15 0.23 3 3 1.36 0.17 0.21 -0.75 0.16 0.24 5 3 4.22 0.14 0.19 0.00 0.14 0.22 55 31 1.88 0.16 0.22 0.24 0.15 0.25 6 2 3.08 0.16 0.21 0.11 0.15 0.22 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.39 0.19 0.28 0.70 0.18 0.28 3 2 -0.41 0.19 0.24 0.64 0.17 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.68 0.20 0.24 -0.53 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1252-0117 53 4847 100 1.67 0.26 0.36 -2.89 0.11 0.18 1.88 0.13 0.23 5.38 0.20 0.27 -0.16 0.22 0.31 1 1 4.86 0.12 0.18 0.14 0.16 0.25 7 6 2.79 0.20 0.29 -0.82 0.22 0.29 1 1 3.44 0.12 0.20 -0.06 0.15 0.26 9 7 0.05 0.18 0.23 -0.26 0.18 0.28 5 4 2.17 0.16 0.21 0.01 0.17 0.25 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.22 0.16 0.23 -0.59 0.17 0.24 3 3 2.56 0.14 0.19 0.03 0.16 0.24 5 4 4.64 0.11 0.18 0.00 0.14 0.22 55 52 2.66 0.15 0.22 0.59 0.17 0.25 6 6 4.10 0.17 0.30 0.71 0.18 0.27 4 4 2.30 0.14 0.21 0.55 0.16 0.27 2 1 -0.88 0.22 0.32 -0.99 0.22 0.31 3 2 -1.51 0.19 0.23 -0.89 0.19 0.29 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.38 0.19 0.23 -1.65 0.19 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1254+0009 54 4865 100 1.86 0.25 0.35 -2.94 0.14 0.19 1.78 0.13 0.23 5.34 0.20 0.26 -0.11 0.18 0.28 1 1 4.89 0.12 0.19 0.26 0.15 0.24 7 5 2.78 0.19 0.28 -0.74 0.20 0.29 1 1 3.63 0.12 0.20 0.21 0.15 0.25 9 8 0.33 0.17 0.22 0.11 0.15 0.23 5 4 2.32 0.16 0.21 0.25 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.23 0.16 0.23 -0.49 0.15 0.24 3 3 1.62 0.16 0.21 -0.82 0.15 0.23 5 3 4.55 0.14 0.19 0.00 0.14 0.22 55 51 2.09 0.16 0.22 0.11 0.15 0.24 6 6 3.32 0.18 0.28 0.02 0.17 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.32 0.23 0.34 -0.35 0.21 0.32 3 2 -1.30 0.19 0.24 -0.59 0.16 0.24 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.67 0.19 0.23 -0.86 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1256-0228 48 4860 100 1.83 0.25 0.35 -2.07 0.12 0.20 1.69 0.13 0.23 6.27 0.21 0.26 -0.04 0.19 0.28 1 1 5.77 0.11 0.19 0.27 0.15 0.24 7 6 3.61 0.16 0.24 -0.77 0.18 0.27 1 1 4.57 0.12 0.21 0.29 0.15 0.25 9 8 1.38 0.17 0.24 0.30 0.16 0.25 5 5 3.10 0.17 0.23 0.16 0.16 0.25 17 16 1.77 0.16 0.20 -0.15 0.15 0.24 3 3 3.33 0.17 0.30 -0.26 0.17 0.27 3 3 2.93 0.14 0.19 -0.38 0.15 0.24 5 5 5.42 0.12 0.20 0.00 0.14 0.22 55 51 2.81 0.21 0.27 -0.02 0.18 0.26 6 6 4.59 0.15 0.25 0.42 0.16 0.23 4 3 2.83 0.14 0.21 0.31 0.15 0.26 2 2 0.89 0.14 0.21 0.00 0.15 0.25 3 1 0.11 0.19 0.25 -0.05 0.17 0.27 6 5 0.79 0.18 0.23 0.27 0.16 0.27 3 2 0.17 0.22 0.28 0.12 0.20 0.28 2 1 -0.64 0.18 0.23 0.28 0.16 0.27 6 4 -0.15 0.18 0.25 0.35 0.16 0.28 10 5 -0.15 0.18 0.23 0.43 0.16 0.27 9 8 -0.25 0.18 0.23 0.82 0.16 0.27 8 2 -1.07 0.18 0.23 0.51 0.16 0.27 4 3
HE 1256-0651 44 6137 100 4.05 0.28 0.38 -2.36 0.13 0.18 1.50 0.16 0.26 6.65 0.20 0.26 0.62 0.23 0.31 1 1 5.44 0.12 0.18 0.22 0.15 0.24 7 2 3.06 0.15 0.22 -1.06 0.16 0.25 1 1 4.33 0.11 0.20 0.32 0.15 0.25 9 7 0.88 0.18 0.23 0.06 0.17 0.26 5 2 2.96 0.16 0.21 0.30 0.15 0.24 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.15 0.15 0.20 -0.17 0.15 0.23 3 3 2.48 0.15 0.20 -0.56 0.15 0.23 5 3 5.15 0.13 0.18 0.00 0.14 0.22 55 34 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.95 0.17 0.22 0.06 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.27 0.20 0.28 -0.35 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.49 0.19 0.23 -0.26 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1259-0621 44 5787 100 3.68 0.25 0.35 -2.64 0.13 0.18 1.60 0.14 0.24 6.16 0.17 0.24 0.41 0.17 0.27 1 1 5.26 0.10 0.17 0.32 0.16 0.24 7 2 2.92 0.15 0.22 -0.91 0.16 0.25 1 1 3.99 0.12 0.20 0.28 0.15 0.25 9 7 0.61 0.18 0.23 0.08 0.16 0.25 5 2 2.77 0.15 0.21 0.40 0.15 0.23 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.71 0.15 0.20 -0.31 0.15 0.22 3 3 2.16 0.16 0.20 -0.59 0.15 0.23 5 3 4.86 0.13 0.18 0.00 0.14 0.22 55 36 2.62 0.15 0.21 0.35 0.15 0.25 6 3 3.52 0.17 0.21 -0.09 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.40 0.21 0.30 0.08 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.48 0.19 0.24 0.04 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1300+0157 56 5411 100 3.38 0.34 0.44 -3.76 0.13 0.19 1.43 0.17 0.27 5.82 0.20 0.27 1.17 0.20 0.29 1 1 4.25 0.15 0.24 0.40 0.19 0.27 7 3 1.90 0.15 0.22 -0.83 0.17 0.27 1 1 3.10 0.13 0.22 0.47 0.15 0.25 9 1 -0.30 0.19 0.24 0.26 0.20 0.29 5 1 1.62 0.16 0.22 0.34 0.18 0.28 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.56 0.16 0.20 -0.37 0.17 0.25 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 3.76 0.13 0.19 0.00 0.14 0.22 55 18 1.69 0.19 0.25 0.50 0.20 0.30 6 1 2.48 0.12 0.17 -0.04 0.15 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.94 0.16 0.22 0.56 0.22 0.31 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1300-0641 44 5308 100 2.96 0.29 0.39 -3.14 0.13 0.18 1.59 0.15 0.25 6.54 0.18 0.26 1.29 0.17 0.27 1 1 4.48 0.12 0.21 0.04 0.17 0.26 7 3 2.12 0.15 0.22 -1.21 0.16 0.25 1 1 3.23 0.11 0.20 0.01 0.17 0.26 9 2 -0.01 0.19 0.24 -0.04 0.17 0.25 5 2 1.87 0.17 0.22 -0.01 0.15 0.25 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.36 0.16 0.22 -0.17 0.15 0.23 3 3 1.80 0.17 0.22 -0.44 0.16 0.23 5 2 4.36 0.13 0.18 0.00 0.14 0.22 55 34 1.90 0.16 0.22 0.12 0.15 0.25 6 3 3.41 0.18 0.25 0.30 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.77 0.22 0.29 -0.59 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -1.78 0.20 0.24 -0.77 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1300-0642 43 5173 100 2.68 0.27 0.37 -3.03 0.12 0.18 1.57 0.14 0.24 5.71 0.19 0.26 0.34 0.19 0.28 1 1 4.82 0.11 0.19 0.26 0.16 0.25 7 3 2.31 0.16 0.23 -1.14 0.17 0.26 1 1 3.65 0.12 0.20 0.31 0.15 0.25 9 4 0.32 0.18 0.23 0.17 0.17 0.26 5 4 2.30 0.16 0.21 0.30 0.16 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.25 0.17 0.22 -0.40 0.16 0.23 3 3 1.63 0.17 0.21 -0.74 0.16 0.24 5 3 4.48 0.12 0.18 0.00 0.14 0.22 55 40 2.12 0.16 0.22 0.22 0.16 0.25 6 4 3.25 0.17 0.24 0.02 0.17 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.27 0.25 0.34 -0.22 0.22 0.33 3 2 -0.80 0.19 0.24 -0.02 0.18 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.27 0.19 0.24 -0.38 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1300-2201 52 6332 100 4.64 0.28 0.38 -2.61 0.11 0.17 1.34 0.15 0.25 6.80 0.16 0.23 1.01 0.17 0.27 1 1 5.27 0.12 0.18 0.29 0.15 0.24 7 1 2.95 0.13 0.21 -0.92 0.15 0.25 1 1 4.05 0.11 0.20 0.29 0.15 0.25 9 3 0.76 0.18 0.23 0.19 0.18 0.27 5 1 2.80 0.16 0.22 0.38 0.17 0.26 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.97 0.14 0.19 -0.11 0.16 0.23 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.90 0.11 0.17 0.00 0.14 0.22 55 30 2.72 0.14 0.21 0.39 0.16 0.25 6 1 3.58 0.15 0.19 -0.07 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.65 0.19 0.27 0.28 0.19 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.51 0.18 0.23 -0.04 0.18 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0
HE 1300-2431 47 5029 100 1.96 0.27 0.37 -3.25 0.14 0.19 1.92 0.13 0.23 4.98 0.24 0.30 -0.16 0.21 0.31 1 1 4.73 0.12 0.18 0.40 0.16 0.24 7 5 2.49 0.17 0.25 -0.73 0.18 0.27 1 1 3.39 0.12 0.20 0.28 0.15 0.25 9 3 0.15 0.18 0.23 0.23 0.15 0.23 5 4 2.44 0.15 0.20 0.67 0.14 0.22 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.09 0.16 0.21 -0.33 0.15 0.23 3 3 1.29 0.16 0.21 -0.84 0.15 0.23 5 3 4.25 0.14 0.19 0.00 0.14 0.22 55 41 2.11 0.15 0.22 0.44 0.15 0.24 6 5 3.22 0.19 0.25 0.22 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.67 0.24 0.33 -0.39 0.21 0.31 3 2 -1.05 0.19 0.23 -0.04 0.16 0.24 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.57 0.18 0.23 -0.45 0.15 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1305-0331 46 6081 100 4.22 0.38 0.48 -3.26 0.13 0.18 1.58 0.19 0.29 6.26 0.19 0.26 1.13 0.20 0.29 1 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 2.49 0.14 0.21 -0.72 0.16 0.25 1 1 3.50 0.13 0.21 0.40 0.15 0.25 9 1 0.32 0.20 0.25 0.41 0.20 0.28 5 1 2.29 0.19 0.25 0.53 0.19 0.28 17 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.24 0.15 0.19 -0.17 0.15 0.23 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.24 0.13 0.18 0.00 0.14 0.22 55 17 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 2.99 0.16 0.20 -0.01 0.16 0.23 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.46 0.20 0.26 -0.17 0.19 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1311-1412 56 4796 100 1.50 0.25 0.35 -2.91 0.13 0.18 1.92 0.12 0.22 5.35 0.20 0.27 -0.15 0.18 0.28 1 1 4.96 0.12 0.18 0.26 0.15 0.23 7 7 2.97 0.18 0.27 -0.62 0.18 0.28 1 1 3.62 0.13 0.20 0.14 0.14 0.25 9 8 0.22 0.17 0.22 -0.07 0.15 0.24 5 4 2.26 0.15 0.20 0.13 0.14 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.42 0.16 0.25 -0.37 0.15 0.25 3 3 1.91 0.16 0.22 -0.60 0.15 0.23 5 3 4.62 0.13 0.18 0.00 0.14 0.22 55 52 2.10 0.16 0.22 0.06 0.15 0.24 6 5 3.26 0.18 0.28 -0.10 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.03 0.22 0.33 -0.06 0.20 0.32 3 1 -0.96 0.18 0.22 -0.32 0.15 0.24 6 3 -0.01 0.18 0.22 0.27 0.15 0.24 3 1 -0.81 0.24 0.31 -0.06 0.21 0.29 2 1 -1.48 0.18 0.23 0.23 0.16 0.24 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -1.13 0.18 0.23 0.25 0.16 0.24 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.84 0.18 0.23 0.53 0.15 0.24 4 4
HE 1314-3036 82 4757 100 1.54 0.23 0.33 -2.99 0.12 0.18 1.88 0.11 0.21 5.27 0.20 0.27 -0.13 0.19 0.28 1 1 4.92 0.11 0.18 0.32 0.15 0.23 7 7 2.61 0.14 0.24 -0.87 0.15 0.26 1 1 3.60 0.12 0.20 0.23 0.14 0.25 9 8 0.23 0.17 0.22 0.04 0.15 0.24 5 5 2.24 0.14 0.19 0.21 0.14 0.22 17 16 0.99 0.15 0.20 -0.02 0.15 0.23 3 2 2.34 0.15 0.24 -0.35 0.15 0.24 3 3 1.77 0.14 0.21 -0.64 0.15 0.23 5 3 4.52 0.12 0.18 0.00 0.14 0.22 55 53 2.09 0.15 0.22 0.16 0.15 0.24 6 6 3.03 0.16 0.25 -0.23 0.16 0.24 4 4 2.01 0.13 0.20 0.39 0.14 0.25 2 1 -0.13 0.20 0.31 -0.12 0.19 0.29 3 2 -1.02 0.18 0.22 -0.27 0.16 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.90 0.19 0.27 -0.05 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.30 0.18 0.22 0.17 0.16 0.25 4 1
HE 1320-1339 291 4935 100 1.69 0.22 0.32 -2.78 0.13 0.18 1.97 0.10 0.20 5.10 0.19 0.26 -0.51 0.18 0.28 1 1 5.05 0.11 0.18 0.25 0.15 0.23 7 7 2.89 0.12 0.23 -0.80 0.14 0.25 1 1 3.84 0.11 0.20 0.26 0.15 0.25 9 8 0.66 0.16 0.22 0.27 0.15 0.23 5 5 2.49 0.15 0.21 0.25 0.14 0.23 17 17 1.23 0.15 0.19 0.01 0.15 0.23 3 2 2.56 0.15 0.23 -0.33 0.14 0.24 3 3 2.04 0.15 0.22 -0.56 0.14 0.23 5 3 4.72 0.13 0.18 0.00 0.14 0.22 55 54 2.29 0.16 0.22 0.16 0.15 0.24 6 6 3.89 0.16 0.28 0.43 0.15 0.27 4 4 2.25 0.13 0.20 0.43 0.14 0.24 2 2 0.42 0.17 0.27 0.23 0.16 0.26 3 2 -0.67 0.18 0.22 -0.13 0.15 0.23 6 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.08 0.19 0.24 -0.42 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.11 0.18 0.22 0.16 0.15 0.24 4 1
HE 1330-0354 47 6257 100 4.13 0.27 0.37 -2.29 0.12 0.18 1.49 0.15 0.25 7.15 0.16 0.24 1.05 0.18 0.27 1 1 5.61 0.11 0.17 0.32 0.15 0.23 7 2 3.25 0.14 0.22 -0.93 0.16 0.25 1 1 4.47 0.11 0.19 0.40 0.15 0.25 9 8 1.24 0.18 0.23 0.36 0.17 0.25 5 2 3.27 0.16 0.21 0.54 0.15 0.24 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.33 0.15 0.20 -0.05 0.15 0.23 3 3 2.55 0.15 0.19 -0.55 0.15 0.23 5 3 5.21 0.12 0.18 0.00 0.14 0.22 55 36 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.88 0.16 0.20 -0.08 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.69 0.21 0.30 0.01 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.63 0.18 0.23 -0.47 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1330-0607 41 5094 100 2.30 0.24 0.34 -2.33 0.13 0.19 1.90 0.14 0.24 6.27 0.19 0.25 0.21 0.17 0.26 1 1 5.35 0.12 0.18 0.10 0.15 0.23 7 5 3.31 0.18 0.26 -0.83 0.19 0.28 1 1 4.26 0.12 0.20 0.23 0.15 0.25 9 7 0.82 0.18 0.23 -0.02 0.16 0.25 5 4 2.87 0.17 0.23 0.18 0.15 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.35 0.20 0.29 0.01 0.19 0.27 3 2 2.84 0.15 0.20 -0.22 0.15 0.23 5 4 5.17 0.13 0.19 0.00 0.14 0.22 55 52 2.78 0.16 0.23 0.19 0.15 0.24 6 6 3.74 0.20 0.27 -0.18 0.19 0.26 4 4 2.64 0.14 0.21 0.37 0.15 0.25 2 1 0.19 0.23 0.34 -0.45 0.22 0.32 3 2 -0.40 0.19 0.24 -0.31 0.16 0.25 6 3 0.51 0.18 0.23 0.24 0.16 0.25 3 1 -0.96 0.23 0.27 -0.76 0.20 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.57 0.19 0.23 0.25 0.16 0.25 4 1
HE 1332-0309 38 5125 100 2.40 0.26 0.36 -2.46 0.13 0.18 1.64 0.14 0.24 6.14 0.19 0.26 0.21 0.18 0.27 1 1 5.25 0.12 0.19 0.13 0.15 0.24 7 5 3.05 0.16 0.25 -0.96 0.19 0.28 1 1 4.11 0.12 0.20 0.21 0.14 0.24 9 8 0.82 0.18 0.23 0.11 0.16 0.25 5 4 2.88 0.16 0.22 0.32 0.15 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.17 0.19 0.29 -0.03 0.18 0.27 3 3 2.49 0.16 0.22 -0.44 0.16 0.24 5 3 5.04 0.13 0.18 0.00 0.14 0.22 55 51 2.60 0.17 0.23 0.14 0.15 0.25 6 6 3.78 0.21 0.31 -0.01 0.20 0.29 4 4 2.71 0.14 0.21 0.57 0.15 0.26 2 1 0.81 0.15 0.24 0.30 0.16 0.25 3 2 -0.19 0.19 0.24 0.03 0.17 0.26 6 3 0.69 0.18 0.23 0.55 0.17 0.26 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.30 0.19 0.24 0.66 0.17 0.26 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.47 0.19 0.23 0.48 0.16 0.26 4 1
HE 1333-0340 41 6053 100 4.18 0.31 0.41 -2.64 0.12 0.18 1.37 0.19 0.29 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 5.18 0.12 0.18 0.24 0.16 0.25 7 1 3.01 0.17 0.24 -0.82 0.17 0.27 1 1 4.02 0.11 0.20 0.30 0.15 0.25 9 3 0.76 0.19 0.24 0.23 0.18 0.27 5 1 2.64 0.17 0.23 0.27 0.17 0.26 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.76 0.15 0.20 -0.27 0.15 0.23 3 3 2.19 0.15 0.19 -0.55 0.16 0.24 5 2 4.86 0.12 0.18 0.00 0.14 0.22 55 31 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.62 0.16 0.21 0.01 0.17 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.60 0.22 0.31 0.27 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1335+0135 50 5246 100 2.94 0.25 0.35 -2.47 0.12 0.18 1.34 0.13 0.23 6.06 0.20 0.26 0.13 0.18 0.26 1 1 5.39 0.12 0.18 0.28 0.14 0.23 7 5 3.07 0.16 0.24 -0.93 0.18 0.26 1 1 4.13 0.11 0.20 0.24 0.14 0.24 9 8 0.72 0.18 0.23 0.01 0.16 0.26 5 4 2.74 0.15 0.20 0.18 0.15 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.21 0.17 0.27 0.01 0.17 0.26 3 3 2.63 0.15 0.21 -0.29 0.16 0.24 5 3 5.03 0.12 0.18 0.00 0.14 0.22 55 49 2.56 0.17 0.23 0.11 0.16 0.25 6 6 3.95 0.17 0.27 0.17 0.17 0.26 4 4 2.68 0.14 0.21 0.55 0.15 0.26 2 1 0.54 0.16 0.25 0.04 0.17 0.26 3 2 -0.38 0.19 0.24 -0.15 0.17 0.27 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.11 0.19 0.24 -0.78 0.17 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1337+0012 229 6141 100 4.25 0.27 0.37 -3.44 0.13 0.18 1.49 0.12 0.22 5.66 0.19 0.25 0.71 0.18 0.27 1 1 4.69 0.12 0.18 0.55 0.15 0.23 7 1 2.38 0.13 0.20 -0.65 0.14 0.24 1 1 3.40 0.11 0.20 0.48 0.14 0.25 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 2.09 0.15 0.21 0.51 0.15 0.24 17 4 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.06 0.13 0.18 0.00 0.14 0.22 55 20 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 2.98 0.14 0.19 0.17 0.14 0.22 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.42 0.18 0.25 0.06 0.16 0.26 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.24 0.18 0.23 0.07 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1337-0453 50 5938 100 3.56 0.27 0.37 -2.34 0.13 0.18 1.62 0.13 0.23 6.17 0.19 0.26 0.12 0.19 0.28 1 1 5.62 0.12 0.18 0.38 0.15 0.24 7 3 3.06 0.14 0.22 -1.07 0.16 0.25 1 1 4.46 0.11 0.20 0.44 0.15 0.25 9 8 0.98 0.18 0.23 0.15 0.16 0.25 5 3 3.07 0.16 0.21 0.39 0.15 0.23 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.19 0.16 0.22 -0.14 0.15 0.23 3 3 2.50 0.15 0.20 -0.56 0.15 0.23 5 3 5.16 0.13 0.18 0.00 0.14 0.22 55 42 2.65 0.14 0.21 0.06 0.15 0.25 6 3 3.78 0.12 0.18 -0.14 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.78 0.18 0.29 0.15 0.17 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.45 0.19 0.24 -0.24 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1343-0640 43 5942 100 3.97 0.25 0.35 -1.90 0.11 0.17 1.48 0.14 0.24 7.26 0.17 0.23 0.77 0.17 0.26 1 1 6.05 0.11 0.18 0.37 0.14 0.23 7 5 3.72 0.15 0.24 -0.85 0.18 0.26 1 1 4.87 0.10 0.20 0.41 0.15 0.25 9 8 1.34 0.16 0.21 0.06 0.16 0.26 5 4 3.44 0.15 0.21 0.32 0.16 0.25 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.74 0.16 0.24 -0.04 0.17 0.25 3 3 3.06 0.16 0.21 -0.43 0.16 0.24 5 3 5.60 0.11 0.17 0.00 0.14 0.22 55 50 2.94 0.16 0.22 -0.08 0.16 0.26 6 2 4.14 0.26 0.31 -0.21 0.24 0.30 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.75 0.13 0.21 0.68 0.15 0.24 3 1 0.85 0.20 0.24 0.51 0.18 0.27 6 2 1.68 0.18 0.23 0.98 0.18 0.27 3 1 0.94 0.19 0.25 0.70 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1345-0206 34 5006 100 2.22 0.27 0.37 -2.82 0.14 0.19 1.65 0.14 0.24 5.91 0.20 0.26 0.34 0.18 0.28 1 1 4.87 0.13 0.19 0.11 0.16 0.24 7 4 2.53 0.17 0.24 -1.12 0.18 0.27 1 1 3.59 0.12 0.20 0.05 0.15 0.25 9 4 0.19 0.18 0.23 -0.16 0.16 0.24 5 3 2.16 0.17 0.22 -0.04 0.15 0.23 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.55 0.18 0.28 -0.30 0.18 0.28 3 3 1.79 0.17 0.23 -0.78 0.16 0.23 5 3 4.68 0.14 0.19 0.00 0.14 0.22 55 44 2.07 0.15 0.22 -0.03 0.15 0.24 6 4 3.03 0.21 0.26 -0.40 0.18 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.28 0.20 0.31 -0.43 0.18 0.30 3 2 -1.08 0.20 0.24 -0.50 0.17 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.79 0.20 0.24 -1.10 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1351-1049 45 5204 100 2.85 0.26 0.36 -3.46 0.13 0.18 1.48 0.16 0.26 6.49 0.18 0.26 1.55 0.18 0.28 1 1 4.43 0.12 0.21 0.30 0.17 0.27 5 3 2.25 0.15 0.22 -0.77 0.16 0.25 1 1 3.23 0.12 0.21 0.32 0.16 0.25 5 2 0.00 0.19 0.24 0.28 0.17 0.25 3 1 1.87 0.17 0.22 0.30 0.16 0.25 11 4 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 1.94 0.17 0.22 -0.28 0.16 0.24 1 1 1.32 0.17 0.21 -0.63 0.16 0.24 4 2 4.05 0.13 0.18 0.00 0.14 0.22 35 17 1.95 0.16 0.22 0.48 0.16 0.25 4 3 3.10 0.18 0.23 0.30 0.16 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 -0.45 0.23 0.32 0.03 0.21 0.30 2 2 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.18 0.20 0.24 0.13 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0
HE 1413-1954 48 6533 100 4.59 0.43 0.53 -3.22 0.12 0.17 1.40 0.16 0.26 6.65 0.22 0.30 1.45 0.24 0.32 1 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 3.50 0.13 0.22 0.33 0.15 0.25 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 17 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.31 0.12 0.17 0.00 0.14 0.22 54 14 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.69 0.21 0.28 -0.47 0.21 0.31 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1419-1759 45 4809 100 1.63 0.25 0.35 -3.18 0.13 0.18 1.83 0.13 0.23 5.02 0.20 0.27 -0.20 0.19 0.29 1 1 4.68 0.11 0.18 0.27 0.15 0.23 7 5 2.34 0.18 0.26 -0.95 0.19 0.28 1 1 3.47 0.12 0.20 0.29 0.15 0.25 9 7 0.07 0.17 0.22 0.07 0.16 0.24 5 4 1.98 0.16 0.21 0.13 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.02 0.16 0.23 -0.48 0.16 0.23 3 3 1.30 0.16 0.21 -0.92 0.15 0.23 5 3 4.33 0.13 0.18 0.00 0.14 0.22 55 46 1.89 0.16 0.22 0.15 0.15 0.25 6 6 3.07 0.18 0.27 -0.00 0.17 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.47 0.25 0.36 -0.26 0.23 0.34 3 2 -1.48 0.19 0.24 -0.54 0.17 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.85 0.19 0.23 -0.81 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1421-2006 49 5687 100 3.73 0.25 0.35 -2.65 0.12 0.18 1.33 0.14 0.24 6.04 0.17 0.24 0.30 0.17 0.26 1 1 5.31 0.10 0.17 0.37 0.15 0.23 7 3 2.86 0.15 0.22 -0.97 0.16 0.25 1 1 4.09 0.11 0.20 0.37 0.15 0.24 9 7 0.52 0.18 0.23 -0.01 0.17 0.26 5 2 2.62 0.15 0.20 0.25 0.15 0.24 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.74 0.14 0.20 -0.29 0.15 0.23 3 3 2.03 0.16 0.21 -0.72 0.16 0.24 5 3 4.85 0.12 0.18 0.00 0.14 0.22 55 37 2.29 0.16 0.22 0.02 0.16 0.25 6 2 3.37 0.16 0.21 -0.24 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.22 0.20 0.29 -0.10 0.20 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.65 0.19 0.23 -0.14 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1430+0053 71 5201 100 2.74 0.24 0.34 -3.03 0.13 0.18 1.55 0.13 0.23 5.65 0.18 0.25 0.29 0.17 0.27 1 1 4.77 0.11 0.19 0.21 0.16 0.25 7 6 2.47 0.14 0.22 -0.98 0.15 0.25 1 1 3.56 0.11 0.19 0.23 0.15 0.25 9 7 0.19 0.18 0.23 0.04 0.15 0.24 5 4 2.25 0.16 0.21 0.26 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.21 0.16 0.21 -0.43 0.15 0.23 3 3 1.59 0.16 0.21 -0.77 0.15 0.23 5 3 4.47 0.13 0.18 0.00 0.14 0.22 55 45 2.17 0.16 0.22 0.27 0.15 0.24 6 6 3.23 0.17 0.23 0.01 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.84 0.21 0.28 -0.78 0.18 0.28 3 2 -1.35 0.19 0.23 -0.57 0.16 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.99 0.21 0.25 -0.10 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.80 0.18 0.23 0.72 0.15 0.24 4 1
HE 1430-0026 53 5855 100 4.12 0.26 0.36 -2.79 0.11 0.17 1.38 0.14 0.24 6.13 0.17 0.24 0.52 0.17 0.26 1 1 5.09 0.11 0.17 0.29 0.15 0.23 7 2 2.79 0.14 0.21 -0.89 0.15 0.25 1 1 3.89 0.11 0.20 0.31 0.14 0.24 9 6 0.49 0.18 0.23 0.10 0.17 0.27 5 1 2.52 0.16 0.22 0.28 0.16 0.26 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.60 0.15 0.20 -0.29 0.15 0.23 3 3 2.02 0.16 0.20 -0.59 0.16 0.24 5 3 4.72 0.11 0.17 0.00 0.14 0.22 55 37 2.49 0.15 0.21 0.35 0.16 0.25 6 3 3.38 0.16 0.20 -0.09 0.16 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.03 0.19 0.27 -0.22 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.91 0.18 0.23 -0.26 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1430-1123 43 5915 100 3.75 0.29 0.39 -2.71 0.13 0.18 1.40 0.16 0.26 7.53 0.16 0.24 1.84 0.18 0.28 1 1 5.23 0.13 0.19 0.35 0.16 0.24 7 2 2.86 0.15 0.22 -0.91 0.16 0.26 1 1 4.13 0.11 0.20 0.47 0.15 0.25 9 5 0.84 0.18 0.23 0.37 0.17 0.26 5 2 2.57 0.17 0.22 0.25 0.16 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.97 0.16 0.21 -0.00 0.16 0.23 3 2 2.12 0.16 0.20 -0.57 0.16 0.24 5 3 4.80 0.13 0.18 0.00 0.14 0.22 55 31 2.61 0.14 0.20 0.39 0.15 0.25 6 2 3.34 0.17 0.21 -0.21 0.17 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.51 0.21 0.30 0.24 0.19 0.29 3 2 0.05 0.30 0.33 0.50 0.26 0.32 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.25 0.14 0.21 1.82 0.16 0.23 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 0.53 0.23 0.27 1.72 0.20 0.28 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1431-2142 53 6137 100 4.10 0.25 0.35 -2.60 0.13 0.18 1.55 0.14 0.24 6.28 0.17 0.24 0.48 0.18 0.28 1 1 5.34 0.12 0.18 0.35 0.15 0.23 7 2 2.85 0.14 0.21 -1.02 0.15 0.25 1 1 4.13 0.10 0.20 0.37 0.16 0.26 9 7 0.82 0.17 0.23 0.24 0.16 0.25 5 2 2.79 0.15 0.21 0.36 0.15 0.23 17 6 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.95 0.14 0.19 -0.13 0.15 0.22 3 3 2.30 0.15 0.19 -0.50 0.15 0.23 5 3 4.90 0.13 0.18 0.00 0.14 0.22 55 33 2.56 0.15 0.21 0.23 0.15 0.25 6 1 3.69 0.15 0.20 0.04 0.15 0.22 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.34 0.20 0.28 -0.03 0.18 0.28 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.34 0.18 0.23 0.13 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 1500-1628 45 4994 100 2.10 0.25 0.35 -2.31 0.12 0.18 1.85 0.13 0.23 6.21 0.20 0.26 0.13 0.18 0.27 1 1 5.45 0.11 0.18 0.18 0.15 0.23 7 6 3.15 0.20 0.28 -1.01 0.21 0.29 1 1 3.87 0.12 0.20 -0.18 0.14 0.24 9 7 0.90 0.18 0.23 0.04 0.17 0.26 5 5 2.48 0.16 0.21 -0.23 0.15 0.24 17 15 1.52 0.16 0.20 -0.18 0.16 0.24 3 2 3.05 0.18 0.28 -0.31 0.18 0.27 3 3 2.80 0.15 0.20 -0.29 0.15 0.23 5 5 5.19 0.12 0.18 0.00 0.14 0.22 55 54 2.77 0.17 0.24 0.15 0.16 0.25 6 5 3.95 0.18 0.32 0.01 0.19 0.31 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.10 0.24 0.30 -1.76 0.20 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.85 0.19 0.23 -1.68 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2133-1432 46 5716 100 3.46 0.24 0.34 -2.02 0.12 0.18 1.46 0.13 0.23 6.49 0.17 0.24 0.12 0.17 0.26 1 1 5.90 0.12 0.18 0.33 0.15 0.23 7 4 3.67 0.12 0.23 -0.78 0.17 0.26 1 1 4.72 0.11 0.20 0.38 0.15 0.25 9 8 1.21 0.18 0.23 0.06 0.16 0.25 5 4 3.27 0.15 0.21 0.27 0.15 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.59 0.16 0.24 -0.06 0.16 0.24 3 3 2.89 0.16 0.22 -0.49 0.16 0.23 5 3 5.48 0.12 0.18 0.00 0.14 0.22 55 50 2.89 0.15 0.22 -0.01 0.15 0.25 6 4 4.03 0.15 0.24 -0.20 0.16 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.06 0.17 0.25 0.10 0.16 0.26 3 2 0.12 0.18 0.23 -0.10 0.16 0.26 6 2 1.10 0.18 0.23 0.52 0.17 0.26 3 1 0.06 0.22 0.27 -0.05 0.20 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2134+0001 37 5257 100 3.00 0.25 0.35 -2.22 0.12 0.19 1.55 0.14 0.24 6.38 0.21 0.26 0.20 0.18 0.27 1 1 5.75 0.12 0.18 0.38 0.14 0.23 7 4 3.42 0.16 0.25 -0.83 0.18 0.27 1 1 4.54 0.12 0.21 0.40 0.14 0.24 9 8 1.00 0.18 0.23 0.05 0.16 0.26 5 3 3.04 0.17 0.22 0.24 0.16 0.25 17 14 1.78 0.16 0.20 0.00 0.15 0.24 3 1 3.48 0.16 0.26 0.03 0.17 0.26 3 3 2.89 0.11 0.22 -0.28 0.19 0.26 5 3 5.28 0.12 0.19 0.00 0.14 0.22 55 52 2.85 0.17 0.23 0.14 0.16 0.25 6 5 3.87 0.20 0.29 -0.16 0.20 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.67 0.17 0.25 -0.08 0.17 0.27 3 2 -0.22 0.19 0.24 -0.24 0.17 0.27 6 2 0.76 0.18 0.23 0.38 0.16 0.27 3 1 -0.51 0.25 0.29 -0.42 0.23 0.31 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -1.24 0.19 0.24 0.47 0.16 0.27 4 1
HE 2139-1851 83 4925 100 1.86 0.25 0.35 -3.25 0.13 0.18 1.78 0.12 0.22 5.64 0.19 0.26 0.49 0.18 0.28 1 1 4.70 0.11 0.18 0.36 0.15 0.24 7 6 2.31 0.14 0.22 -0.92 0.15 0.25 1 1 3.44 0.12 0.20 0.33 0.15 0.25 9 7 -0.02 0.17 0.22 0.06 0.15 0.24 5 4 2.04 0.16 0.21 0.26 0.15 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.01 0.15 0.21 -0.41 0.15 0.23 3 3 1.23 0.16 0.21 -0.91 0.15 0.23 5 3 4.26 0.13 0.18 0.00 0.14 0.22 55 47 1.92 0.15 0.22 0.25 0.15 0.24 6 6 2.95 0.16 0.23 -0.05 0.15 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.02 0.20 0.32 0.29 0.19 0.31 3 2 -1.06 0.18 0.23 -0.05 0.16 0.24 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.01 0.18 0.23 -0.90 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2143+0030 43 4688 100 1.50 0.25 0.35 -2.43 0.12 0.19 1.91 0.12 0.22 5.60 0.21 0.26 -0.36 0.18 0.27 1 1 5.37 0.11 0.19 0.22 0.15 0.23 7 7 3.33 0.17 0.26 -0.71 0.19 0.27 1 1 4.04 0.12 0.20 0.11 0.14 0.25 9 8 0.66 0.16 0.21 -0.08 0.15 0.25 5 5 2.70 0.16 0.21 0.11 0.15 0.24 17 17 1.38 0.15 0.20 -0.19 0.15 0.23 3 3 2.99 0.17 0.30 -0.24 0.16 0.26 3 3 2.62 0.14 0.19 -0.34 0.15 0.23 5 4 5.07 0.12 0.19 0.00 0.14 0.22 55 52 2.41 0.17 0.24 -0.08 0.16 0.25 6 6 3.98 0.19 0.30 0.17 0.19 0.27 4 4 2.45 0.14 0.21 0.28 0.15 0.27 2 1 0.45 0.18 0.25 -0.09 0.17 0.26 3 2 -0.57 0.18 0.23 -0.37 0.15 0.26 6 5 0.21 0.17 0.22 0.04 0.15 0.26 3 2 -0.68 0.28 0.35 -0.38 0.25 0.33 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.93 0.18 0.23 -0.01 0.15 0.27 4 3
HE 2145-3025 26 5608 100 2.22 0.29 0.39 -2.69 0.14 0.19 2.47 0.15 0.25 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 5.25 0.12 0.18 0.36 0.16 0.24 7 1 3.04 0.17 0.23 -0.73 0.17 0.26 1 1 4.02 0.12 0.20 0.35 0.15 0.25 9 1 0.65 0.18 0.23 0.17 0.16 0.24 5 2 2.67 0.17 0.22 0.35 0.15 0.23 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.80 0.16 0.21 -0.18 0.15 0.23 3 3 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.81 0.14 0.19 0.00 0.14 0.22 55 25 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 3.49 0.17 0.22 -0.07 0.16 0.23 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.74 0.27 0.37 0.46 0.25 0.36 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.87 0.20 0.25 -0.31 0.17 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2150-0825 39 5960 100 3.67 0.26 0.36 -1.98 0.12 0.18 1.57 0.15 0.25 7.76 0.16 0.23 1.35 0.17 0.27 1 1 5.95 0.12 0.18 0.36 0.15 0.24 7 5 3.40 0.17 0.24 -1.09 0.18 0.26 1 1 4.83 0.11 0.20 0.46 0.15 0.25 9 8 1.41 0.18 0.23 0.22 0.16 0.26 5 4 3.35 0.16 0.21 0.31 0.15 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.76 0.17 0.25 0.07 0.17 0.25 3 3 3.03 0.15 0.20 -0.37 0.15 0.23 5 3 5.52 0.12 0.18 0.00 0.14 0.22 55 47 2.95 0.15 0.22 0.02 0.16 0.25 6 3 3.99 0.17 0.23 -0.27 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.64 0.15 0.23 0.66 0.16 0.25 3 1 1.10 0.18 0.23 0.85 0.17 0.25 6 5 1.59 0.18 0.23 0.97 0.17 0.26 3 1 1.85 0.14 0.19 1.70 0.15 0.22 2 2 0.60 0.16 0.22 1.41 0.16 0.25 6 5 1.08 0.18 0.25 1.48 0.17 0.28 10 1 0.93 0.18 0.23 1.42 0.17 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2151-2858 42 5598 100 4.14 0.25 0.35 -2.38 0.11 0.18 1.39 0.15 0.25 6.11 0.19 0.24 0.10 0.18 0.26 1 1 5.57 0.12 0.18 0.37 0.14 0.24 7 4 3.48 0.12 0.25 -0.61 0.17 0.27 1 1 4.28 0.12 0.20 0.30 0.14 0.24 9 8 0.85 0.18 0.23 0.06 0.18 0.28 5 3 2.91 0.13 0.19 0.27 0.15 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.17 0.15 0.22 -0.12 0.16 0.24 3 3 2.48 0.16 0.21 -0.53 0.17 0.25 5 2 5.12 0.11 0.18 0.00 0.14 0.22 55 41 2.64 0.16 0.22 0.10 0.16 0.26 6 4 3.75 0.16 0.24 -0.12 0.18 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.31 0.18 0.26 -0.29 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 -0.50 0.20 0.24 -0.26 0.19 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2153-2719 73 4898 100 2.01 0.23 0.33 -2.49 0.12 0.18 1.80 0.12 0.22 6.02 0.21 0.27 0.12 0.19 0.27 1 1 5.46 0.11 0.18 0.36 0.15 0.23 7 6 3.47 0.13 0.24 -0.51 0.15 0.25 1 1 4.20 0.12 0.20 0.33 0.14 0.24 9 9 0.82 0.18 0.23 0.14 0.15 0.25 5 4 2.77 0.16 0.21 0.24 0.15 0.23 17 17 1.52 0.16 0.20 0.01 0.15 0.23 3 3 3.10 0.15 0.28 -0.08 0.16 0.27 3 3 2.50 0.14 0.20 -0.41 0.15 0.23 5 5 5.01 0.12 0.18 0.00 0.14 0.22 55 54 2.44 0.16 0.23 0.01 0.15 0.24 6 6 3.62 0.16 0.28 -0.15 0.17 0.27 4 4 2.31 0.13 0.20 0.19 0.14 0.25 2 2 0.48 0.15 0.24 -0.00 0.15 0.25 3 2 -0.46 0.19 0.24 -0.22 0.16 0.26 6 6 0.30 0.17 0.22 0.19 0.15 0.25 3 2 -1.05 0.19 0.25 -0.69 0.18 0.26 2 1 -1.42 0.18 0.23 -0.11 0.15 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -1.01 0.19 0.23 -0.03 0.16 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.77 0.18 0.22 0.21 0.15 0.25 4 3
HE 2154-2838 44 5303 100 3.18 0.25 0.35 -1.85 0.12 0.19 1.46 0.14 0.24 6.58 0.20 0.25 0.05 0.17 0.27 1 1 5.91 0.11 0.18 0.18 0.14 0.23 7 5 3.96 0.14 0.23 -0.66 0.17 0.26 1 1 4.78 0.12 0.21 0.28 0.14 0.24 9 9 1.51 0.17 0.22 0.20 0.16 0.27 5 5 3.39 0.16 0.21 0.23 0.16 0.25 17 17 2.13 0.16 0.20 -0.01 0.15 0.25 3 3 3.83 0.14 0.24 0.02 0.16 0.24 3 3 3.26 0.15 0.20 -0.28 0.15 0.24 5 5 5.65 0.12 0.19 0.00 0.14 0.22 55 53 3.18 0.18 0.24 0.11 0.17 0.26 6 5 4.19 0.17 0.27 -0.20 0.18 0.26 4 4 2.78 0.14 0.21 0.03 0.15 0.27 2 1 1.15 0.14 0.22 0.03 0.15 0.25 3 2 0.30 0.18 0.23 -0.08 0.17 0.28 6 5 1.15 0.18 0.23 0.40 0.17 0.28 3 2 0.24 0.21 0.29 -0.03 0.22 0.30 2 1 -0.55 0.19 0.23 0.14 0.16 0.29 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.89 0.19 0.24 0.45 0.16 0.29 4 3
HE 2155+0136 37 5331 100 3.22 0.25 0.35 -2.07 0.12 0.19 1.23 0.15 0.25 6.32 0.20 0.25 -0.00 0.18 0.27 1 1 5.73 0.11 0.18 0.22 0.15 0.23 7 5 3.44 0.17 0.25 -0.96 0.18 0.27 1 1 4.66 0.12 0.21 0.37 0.14 0.24 9 8 1.07 0.18 0.23 -0.03 0.17 0.28 5 4 3.16 0.15 0.21 0.21 0.16 0.26 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.52 0.15 0.26 -0.08 0.17 0.25 3 3 3.01 0.15 0.20 -0.32 0.16 0.24 5 3 5.43 0.12 0.19 0.00 0.14 0.22 55 52 3.00 0.16 0.24 0.15 0.16 0.26 6 6 4.22 0.19 0.28 0.04 0.19 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.78 0.16 0.24 -0.13 0.17 0.26 3 2 -0.05 0.19 0.24 -0.22 0.18 0.29 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.20 0.21 0.28 0.13 0.21 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.87 0.18 0.23 0.68 0.17 0.29 4 3
HE 2156-3130 60 4692 100 1.28 0.26 0.36 -3.13 0.13 0.18 1.93 0.13 0.23 6.00 0.20 0.27 0.74 0.19 0.29 1 1 5.22 0.11 0.19 0.77 0.15 0.24 5 5 3.27 0.15 0.25 -0.07 0.17 0.27 1 1 3.53 0.11 0.20 0.31 0.15 0.25 5 4 0.42 0.19 0.24 0.39 0.16 0.25 3 3 2.05 0.15 0.20 0.16 0.15 0.22 11 10 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 2.17 0.17 0.26 -0.37 0.17 0.26 1 1 1.71 0.11 0.23 -0.55 0.16 0.26 4 2 4.37 0.13 0.18 0.00 0.14 0.22 35 34 2.04 0.15 0.22 0.26 0.15 0.24 4 3 2.91 0.17 0.26 -0.21 0.16 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 -1.06 0.20 0.30 -0.89 0.19 0.29 2 2 -1.79 0.19 0.24 -0.90 0.17 0.25 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.48 0.22 0.31 0.52 0.20 0.29 2 1 -1.64 0.18 0.22 0.32 0.16 0.24 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0
HE 2158-3112 85 4843 100 1.85 0.23 0.33 -2.75 0.12 0.18 1.85 0.11 0.21 5.61 0.20 0.26 -0.04 0.18 0.27 1 1 5.13 0.11 0.18 0.29 0.15 0.23 7 6 3.02 0.14 0.24 -0.71 0.16 0.26 1 1 3.80 0.11 0.20 0.18 0.15 0.24 9 8 0.57 0.17 0.22 0.14 0.15 0.24 5 5 2.44 0.16 0.21 0.16 0.15 0.23 17 17 1.21 0.15 0.20 -0.05 0.15 0.23 3 2 2.59 0.16 0.25 -0.34 0.16 0.25 3 3 2.28 0.14 0.21 -0.37 0.15 0.23 5 4 4.76 0.12 0.18 0.00 0.14 0.22 55 53 2.33 0.15 0.22 0.14 0.15 0.24 6 6 3.46 0.17 0.27 -0.05 0.17 0.26 4 4 2.07 0.13 0.20 0.21 0.14 0.25 2 1 0.03 0.18 0.29 -0.20 0.18 0.28 3 2 -0.79 0.18 0.23 -0.29 0.16 0.25 6 4 -0.10 0.18 0.22 0.04 0.15 0.25 3 1 -1.45 0.19 0.23 -0.84 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.21 0.18 0.23 0.02 0.16 0.25 4 1
HE 2200-2030 40 5870 100 3.42 0.27 0.37 -2.00 0.12 0.18 1.64 0.15 0.25 6.49 0.17 0.24 0.10 0.18 0.28 1 1 5.82 0.12 0.18 0.24 0.15 0.24 7 4 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 4.67 0.11 0.20 0.32 0.15 0.25 9 8 1.20 0.18 0.23 0.03 0.17 0.26 5 3 3.26 0.16 0.22 0.25 0.16 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.58 0.18 0.25 -0.09 0.17 0.25 3 3 2.96 0.18 0.23 -0.43 0.17 0.24 5 3 5.50 0.12 0.18 0.00 0.14 0.22 55 48 2.89 0.15 0.21 -0.03 0.16 0.25 6 3 4.08 0.19 0.26 -0.16 0.18 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.90 0.21 0.31 -0.07 0.19 0.29 3 2 -0.06 0.19 0.24 -0.30 0.18 0.27 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.09 0.23 0.28 -0.03 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2201-0637 43 4976 100 2.21 0.25 0.35 -2.61 0.11 0.18 1.69 0.13 0.23 5.93 0.20 0.26 0.14 0.21 0.29 1 1 5.18 0.12 0.19 0.19 0.15 0.24 7 5 2.91 0.21 0.28 -0.96 0.22 0.29 1 1 4.00 0.12 0.20 0.24 0.15 0.25 9 8 0.56 0.18 0.23 -0.01 0.18 0.27 5 4 2.57 0.15 0.21 0.15 0.16 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.82 0.18 0.28 -0.26 0.18 0.26 3 3 2.11 0.18 0.25 -0.69 0.18 0.25 5 3 4.91 0.11 0.18 0.00 0.14 0.22 55 52 2.35 0.23 0.29 0.02 0.22 0.31 6 5 3.64 0.21 0.31 -0.02 0.20 0.29 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.28 0.20 0.28 -0.10 0.19 0.28 3 2 -0.64 0.19 0.23 -0.28 0.18 0.28 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.13 0.20 0.24 -0.66 0.20 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2204-1703 36 4932 100 1.87 0.27 0.37 -2.79 0.12 0.18 1.84 0.13 0.23 5.81 0.20 0.26 0.21 0.20 0.29 1 1 5.16 0.12 0.19 0.36 0.15 0.24 7 6 3.27 0.20 0.29 -0.41 0.21 0.30 1 1 3.77 0.12 0.20 0.20 0.15 0.25 9 6 0.61 0.18 0.23 0.23 0.17 0.25 5 4 2.44 0.17 0.22 0.21 0.16 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.59 0.18 0.27 -0.29 0.18 0.26 3 3 1.87 0.17 0.23 -0.73 0.17 0.24 5 3 4.71 0.12 0.18 0.00 0.14 0.22 55 45 2.41 0.15 0.22 0.27 0.16 0.25 6 4 3.49 0.21 0.30 0.03 0.20 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.35 0.26 0.36 -0.53 0.24 0.34 3 2 -0.95 0.19 0.24 -0.40 0.18 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.41 0.22 0.26 -0.75 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2206-2245 45 5100 100 2.45 0.25 0.35 -2.73 0.12 0.18 1.70 0.13 0.23 5.87 0.19 0.26 0.21 0.18 0.27 1 1 5.17 0.11 0.19 0.32 0.15 0.24 7 6 2.82 0.17 0.25 -0.92 0.18 0.27 1 1 3.99 0.12 0.20 0.36 0.15 0.25 9 8 0.58 0.18 0.23 0.14 0.16 0.25 5 3 2.55 0.16 0.21 0.26 0.15 0.24 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.67 0.18 0.25 -0.27 0.17 0.25 3 3 2.11 0.18 0.24 -0.55 0.17 0.24 5 2 4.77 0.12 0.18 0.00 0.14 0.22 55 48 2.38 0.16 0.23 0.20 0.15 0.25 6 6 3.52 0.19 0.28 0.00 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.19 0.19 0.30 -0.05 0.19 0.29 3 2 -0.70 0.19 0.24 -0.21 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.71 0.23 0.28 -0.11 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.61 0.19 0.23 0.62 0.16 0.26 4 1
HE 2216-0621 42 4671 100 1.27 0.27 0.37 -3.23 0.13 0.18 2.02 0.12 0.22 4.50 0.21 0.28 -0.66 0.20 0.30 1 1 4.57 0.12 0.19 0.22 0.15 0.23 7 5 2.40 0.18 0.27 -0.84 0.21 0.30 1 1 3.27 0.12 0.20 0.14 0.15 0.25 9 5 0.05 0.16 0.21 0.11 0.15 0.24 5 4 1.87 0.15 0.20 0.08 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.93 0.15 0.22 -0.51 0.15 0.23 3 3 1.61 0.13 0.21 -0.55 0.15 0.24 5 3 4.27 0.13 0.18 0.00 0.14 0.22 55 43 1.94 0.14 0.21 0.24 0.15 0.24 6 5 3.37 0.19 0.30 0.35 0.19 0.30 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.75 0.24 0.34 -0.49 0.22 0.33 3 2 -1.48 0.19 0.24 -0.49 0.17 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.36 0.19 0.23 -1.27 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2216-1548 75 5154 100 1.73 0.24 0.34 -1.70 0.14 0.20 2.69 0.12 0.22 6.31 0.19 0.25 -0.38 0.18 0.27 1 1 6.05 0.11 0.18 0.17 0.15 0.24 7 5 3.88 0.15 0.26 -0.89 0.17 0.26 1 1 4.85 0.13 0.21 0.19 0.15 0.25 9 9 1.41 0.16 0.22 -0.06 0.14 0.23 5 5 3.44 0.16 0.22 0.11 0.14 0.23 17 17 2.17 0.15 0.20 -0.13 0.15 0.23 3 3 3.56 0.18 0.27 -0.41 0.16 0.25 3 2 3.39 0.14 0.19 -0.30 0.15 0.23 5 5 5.80 0.14 0.20 0.00 0.14 0.22 55 52 3.30 0.16 0.23 0.08 0.15 0.24 6 6 4.53 0.20 0.29 -0.02 0.17 0.25 4 4 2.96 0.13 0.20 0.06 0.14 0.25 2 2 1.32 0.16 0.22 0.05 0.15 0.24 3 2 0.40 0.18 0.23 -0.14 0.15 0.24 6 6 1.20 0.18 0.23 0.30 0.14 0.24 3 3 0.72 0.16 0.22 0.29 0.14 0.23 2 2 -0.34 0.18 0.22 0.19 0.14 0.24 6 5 0.03 0.18 0.25 0.15 0.15 0.27 10 5 0.00 0.18 0.23 0.20 0.15 0.24 9 8 -0.29 0.18 0.23 0.40 0.15 0.25 8 3 -0.61 0.18 0.23 0.58 0.15 0.25 4 4
HE 2217-0706 45 4497 100 1.01 0.24 0.34 -2.56 0.12 0.19 2.13 0.12 0.22 5.27 0.21 0.27 -0.55 0.19 0.28 1 1 5.34 0.11 0.18 0.33 0.15 0.24 7 5 3.37 0.17 0.27 -0.52 0.18 0.27 1 1 4.02 0.11 0.20 0.23 0.15 0.25 9 8 0.65 0.17 0.22 0.05 0.15 0.24 5 5 2.54 0.15 0.20 0.09 0.15 0.23 17 17 1.31 0.16 0.20 -0.11 0.16 0.24 3 3 2.53 0.18 0.28 -0.56 0.17 0.25 3 3 2.42 0.15 0.20 -0.39 0.16 0.24 5 5 4.92 0.12 0.19 0.00 0.14 0.22 55 52 2.39 0.16 0.23 0.05 0.15 0.24 6 6 3.71 0.22 0.33 0.03 0.21 0.29 4 4 2.20 0.13 0.20 0.17 0.14 0.26 2 2 0.20 0.18 0.27 -0.20 0.18 0.27 3 1 -0.68 0.18 0.22 -0.34 0.15 0.25 6 6 0.03 0.17 0.22 0.01 0.15 0.25 3 2 -1.01 0.24 0.30 -0.57 0.21 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -1.34 0.19 0.23 -0.26 0.16 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.21 0.18 0.23 -0.15 0.16 0.26 4 3
HE 2217-1523 48 4847 100 1.82 0.25 0.35 -2.62 0.13 0.19 1.81 0.13 0.23 5.80 0.20 0.26 0.04 0.18 0.27 1 1 5.28 0.10 0.18 0.32 0.16 0.24 7 6 3.19 0.18 0.28 -0.66 0.20 0.29 1 1 4.05 0.11 0.20 0.31 0.15 0.25 9 8 0.65 0.19 0.24 0.11 0.16 0.25 5 5 2.62 0.16 0.22 0.23 0.15 0.23 17 17 1.31 0.16 0.20 -0.07 0.16 0.24 3 1 2.64 0.17 0.27 -0.41 0.17 0.26 3 3 2.33 0.14 0.21 -0.44 0.15 0.23 5 3 4.88 0.13 0.19 0.00 0.14 0.22 55 53 2.40 0.16 0.23 0.10 0.15 0.24 6 6 3.57 0.20 0.31 -0.06 0.19 0.29 4 4 2.26 0.14 0.21 0.29 0.15 0.25 2 1 0.20 0.18 0.28 -0.14 0.18 0.27 3 2 -0.67 0.20 0.24 -0.29 0.16 0.26 6 4 0.06 0.18 0.23 0.09 0.16 0.25 3 1 -1.01 0.23 0.29 -0.52 0.20 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2219-0713 55 4789 100 1.68 0.25 0.35 -2.91 0.12 0.18 1.64 0.13 0.23 5.30 0.20 0.27 -0.17 0.19 0.28 1 1 4.91 0.12 0.18 0.25 0.15 0.23 7 7 2.52 0.16 0.25 -1.03 0.17 0.27 1 1 3.62 0.12 0.20 0.17 0.14 0.25 9 8 0.15 0.17 0.22 -0.10 0.16 0.25 5 4 2.15 0.15 0.21 0.05 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.43 0.17 0.27 -0.32 0.16 0.26 3 3 1.91 0.14 0.22 -0.56 0.15 0.23 5 3 4.58 0.12 0.18 0.00 0.14 0.22 55 52 2.00 0.16 0.22 0.00 0.15 0.25 6 5 3.23 0.18 0.29 -0.10 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.27 0.22 0.34 -0.32 0.21 0.32 3 2 -1.30 0.19 0.23 -0.62 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.15 0.19 0.23 -1.36 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2221-4150 53 5887 100 4.06 0.24 0.34 -2.03 0.11 0.17 1.41 0.14 0.24 6.59 0.16 0.23 0.23 0.17 0.25 1 1 5.87 0.11 0.17 0.32 0.14 0.23 7 4 3.43 0.14 0.22 -1.01 0.16 0.26 1 1 4.64 0.11 0.20 0.31 0.14 0.24 9 8 1.19 0.17 0.22 0.05 0.17 0.27 5 4 3.24 0.16 0.21 0.25 0.16 0.25 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.48 0.15 0.23 -0.16 0.16 0.25 3 3 2.91 0.15 0.21 -0.45 0.16 0.24 5 3 5.47 0.11 0.17 0.00 0.14 0.22 55 47 2.95 0.15 0.21 0.06 0.15 0.25 6 4 4.06 0.17 0.23 -0.16 0.17 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.96 0.16 0.25 0.02 0.17 0.27 3 2 0.13 0.18 0.23 -0.08 0.17 0.27 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.19 0.20 0.24 0.09 0.19 0.28 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2222-4156 51 5537 100 3.27 0.24 0.34 -2.73 0.12 0.18 1.44 0.14 0.24 6.08 0.17 0.24 0.42 0.17 0.27 1 1 5.28 0.12 0.21 0.42 0.20 0.27 7 2 2.82 0.15 0.23 -0.93 0.16 0.25 1 1 3.99 0.11 0.20 0.35 0.15 0.25 9 7 0.47 0.17 0.23 0.03 0.16 0.25 5 2 2.62 0.16 0.21 0.33 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.73 0.16 0.22 -0.21 0.16 0.23 3 3 1.95 0.16 0.21 -0.71 0.16 0.24 5 3 4.77 0.12 0.18 0.00 0.14 0.22 55 38 2.26 0.16 0.22 0.07 0.15 0.25 6 3 3.51 0.18 0.24 -0.02 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.30 0.21 0.31 0.06 0.19 0.30 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.76 0.19 0.23 -0.16 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2224+0143 88 5198 100 2.66 0.24 0.34 -2.58 0.12 0.18 1.67 0.12 0.22 6.16 0.19 0.25 0.35 0.17 0.26 1 1 5.32 0.11 0.18 0.32 0.15 0.23 7 6 2.90 0.14 0.23 -0.98 0.15 0.25 1 1 4.07 0.13 0.20 0.29 0.14 0.24 9 8 0.72 0.17 0.22 0.13 0.15 0.25 5 5 2.74 0.16 0.21 0.31 0.15 0.23 17 16 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.88 0.16 0.24 -0.21 0.16 0.24 3 3 2.34 0.16 0.22 -0.47 0.15 0.23 5 3 4.92 0.12 0.18 0.00 0.14 0.22 55 54 2.57 0.16 0.22 0.24 0.15 0.24 6 6 3.63 0.17 0.25 -0.04 0.16 0.25 4 4 2.29 0.14 0.21 0.27 0.14 0.25 2 1 0.62 0.15 0.24 0.23 0.15 0.25 3 2 -0.22 0.18 0.23 0.13 0.16 0.25 6 5 0.60 0.18 0.22 0.58 0.15 0.25 3 1 0.13 0.20 0.27 0.59 0.18 0.27 2 1 -0.77 0.18 0.23 0.65 0.15 0.25 6 4 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.47 0.18 0.23 0.61 0.16 0.25 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.02 0.18 0.23 1.05 0.15 0.25 4 4
HE 2224-4103 49 5074 100 2.32 0.25 0.35 -2.64 0.12 0.17 1.75 0.12 0.22 6.02 0.20 0.26 0.23 0.19 0.28 1 1 5.34 0.11 0.19 0.36 0.15 0.24 7 6 3.10 0.16 0.25 -0.77 0.17 0.26 1 1 4.12 0.12 0.20 0.36 0.15 0.25 9 8 0.74 0.18 0.23 0.18 0.17 0.25 5 4 2.68 0.16 0.21 0.27 0.15 0.24 17 15 1.47 0.16 0.20 0.07 0.16 0.24 3 1 2.78 0.17 0.26 -0.29 0.17 0.26 3 3 2.26 0.14 0.22 -0.53 0.15 0.24 5 3 4.90 0.12 0.17 0.00 0.14 0.22 55 52 2.46 0.16 0.22 0.15 0.16 0.25 6 5 3.51 0.19 0.27 -0.13 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.27 0.18 0.29 -0.10 0.18 0.29 3 2 -0.66 0.19 0.24 -0.29 0.18 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.04 0.20 0.25 -0.57 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2226-4102 49 5140 100 2.43 0.26 0.36 -2.87 0.13 0.19 1.73 0.13 0.23 5.98 0.19 0.26 0.46 0.18 0.27 1 1 4.95 0.12 0.18 0.23 0.15 0.24 7 6 2.60 0.16 0.24 -1.01 0.16 0.26 1 1 3.75 0.12 0.20 0.26 0.15 0.25 9 7 0.40 0.18 0.23 0.10 0.16 0.25 5 4 2.33 0.16 0.21 0.17 0.15 0.24 17 11 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.48 0.17 0.24 -0.32 0.16 0.24 3 3 1.98 0.17 0.22 -0.55 0.15 0.23 5 3 4.63 0.13 0.19 0.00 0.14 0.22 55 45 2.30 0.16 0.22 0.25 0.15 0.24 6 6 3.27 0.18 0.24 -0.11 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.05 0.22 0.33 -0.06 0.20 0.31 3 2 -0.77 0.19 0.23 -0.15 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.74 0.19 0.23 -1.00 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2227-4044 49 5811 100 3.85 0.25 0.35 -2.32 0.11 0.17 1.40 0.14 0.24 7.75 0.16 0.23 1.67 0.17 0.26 1 1 5.56 0.11 0.18 0.30 0.15 0.23 5 2 3.42 0.14 0.23 -0.73 0.16 0.25 1 1 4.43 0.11 0.21 0.39 0.15 0.25 5 4 1.17 0.18 0.23 0.32 0.17 0.26 3 2 2.94 0.15 0.20 0.24 0.15 0.24 11 8 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.33 0.17 0.24 -0.03 0.17 0.25 1 1 2.54 0.16 0.21 -0.54 0.16 0.24 4 2 5.18 0.11 0.17 0.00 0.14 0.22 35 26 2.65 0.16 0.22 0.05 0.16 0.25 4 2 3.79 0.16 0.22 -0.14 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 1.06 0.14 0.24 0.41 0.15 0.25 2 2 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.19 0.17 0.21 1.38 0.17 0.24 2 1 0.13 0.18 0.23 1.28 0.17 0.26 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0
HE 2228-3806 50 5175 100 2.62 0.27 0.37 -3.07 0.13 0.18 1.65 0.14 0.24 5.74 0.19 0.26 0.42 0.18 0.27 1 1 4.84 0.11 0.19 0.33 0.15 0.24 7 4 2.43 0.15 0.22 -0.97 0.16 0.25 1 1 3.64 0.12 0.20 0.35 0.15 0.25 9 7 0.23 0.18 0.23 0.12 0.16 0.25 5 4 2.25 0.16 0.22 0.30 0.15 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.17 0.16 0.21 -0.43 0.15 0.23 3 3 1.58 0.16 0.21 -0.74 0.15 0.23 5 3 4.43 0.13 0.18 0.00 0.14 0.22 55 40 2.15 0.16 0.22 0.30 0.15 0.24 6 5 3.11 0.18 0.24 -0.07 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.29 0.23 0.32 -0.19 0.21 0.31 3 2 -1.03 0.19 0.24 -0.20 0.17 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.51 0.19 0.24 -0.57 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2229-4153 74 5138 100 2.47 0.24 0.34 -2.62 0.12 0.18 1.79 0.12 0.22 6.17 0.19 0.26 0.37 0.19 0.28 1 1 5.29 0.12 0.18 0.29 0.15 0.23 7 5 3.09 0.14 0.24 -0.79 0.16 0.26 1 1 4.11 0.11 0.20 0.34 0.14 0.25 9 8 0.71 0.18 0.23 0.13 0.16 0.25 5 5 2.65 0.16 0.21 0.22 0.15 0.23 17 14 1.46 0.15 0.20 0.05 0.15 0.24 3 1 2.84 0.16 0.24 -0.25 0.16 0.24 3 3 2.33 0.16 0.22 -0.47 0.16 0.23 5 3 4.91 0.12 0.18 0.00 0.14 0.22 55 53 2.51 0.16 0.22 0.18 0.15 0.25 6 6 3.48 0.17 0.26 -0.19 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.47 0.17 0.26 0.09 0.16 0.26 3 2 -0.46 0.18 0.23 -0.12 0.16 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.74 0.21 0.26 -0.28 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.63 0.18 0.23 0.45 0.16 0.26 4 1
HE 2231-0622 22 5211 100 2.90 0.27 0.37 -2.12 0.13 0.19 1.50 0.15 0.25 6.19 0.20 0.26 -0.08 0.18 0.26 1 1 5.62 0.12 0.18 0.15 0.15 0.23 7 5 2.96 0.31 0.37 -1.39 0.33 0.39 1 1 4.43 0.11 0.21 0.19 0.15 0.25 9 8 0.91 0.19 0.24 -0.14 0.18 0.28 5 4 3.02 0.15 0.21 0.11 0.17 0.25 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.43 0.20 0.29 -0.12 0.20 0.29 3 3 2.91 0.17 0.21 -0.36 0.17 0.25 5 3 5.38 0.13 0.19 0.00 0.14 0.22 55 43 2.78 0.17 0.23 -0.03 0.17 0.26 6 5 3.53 0.29 0.35 -0.61 0.29 0.35 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.35 0.25 0.33 -0.50 0.25 0.34 3 2 -0.17 0.21 0.26 -0.29 0.20 0.30 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.45 0.30 0.35 -0.46 0.31 0.37 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2234-0521 34 5332 100 3.15 0.25 0.35 -2.78 0.13 0.18 1.39 0.15 0.25 5.97 0.19 0.25 0.36 0.17 0.26 1 1 5.13 0.11 0.19 0.32 0.16 0.25 7 5 2.60 0.17 0.24 -1.09 0.17 0.26 1 1 3.88 0.12 0.20 0.30 0.15 0.25 9 6 0.58 0.18 0.23 0.19 0.16 0.25 5 3 2.54 0.17 0.22 0.30 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.50 0.17 0.23 -0.39 0.16 0.24 3 3 1.92 0.17 0.21 -0.69 0.16 0.23 5 3 4.72 0.13 0.18 0.00 0.14 0.22 55 39 2.44 0.16 0.22 0.29 0.15 0.25 6 5 3.56 0.15 0.21 0.09 0.15 0.22 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.11 0.23 0.32 -0.30 0.22 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.49 0.20 0.24 -0.84 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2238-2152 48 5427 100 3.28 0.25 0.35 -2.40 0.12 0.18 1.46 0.13 0.23 6.12 0.19 0.25 0.13 0.17 0.26 1 1 5.37 0.11 0.18 0.19 0.15 0.23 7 6 2.89 0.16 0.24 -1.18 0.17 0.26 1 1 4.19 0.12 0.20 0.23 0.14 0.25 9 7 0.70 0.18 0.23 -0.07 0.16 0.26 5 4 2.82 0.15 0.20 0.21 0.15 0.24 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.95 0.17 0.24 -0.32 0.16 0.24 3 3 2.41 0.17 0.22 -0.58 0.16 0.24 5 3 5.10 0.12 0.18 0.00 0.14 0.22 55 48 2.60 0.17 0.23 0.08 0.15 0.25 6 5 3.68 0.18 0.25 -0.17 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.28 0.20 0.29 -0.29 0.19 0.29 3 2 -0.50 0.17 0.22 -0.34 0.16 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.64 0.21 0.25 -0.37 0.18 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2240-0412 30 5852 100 4.33 0.29 0.39 -2.20 0.12 0.18 1.30 0.18 0.28 7.54 0.17 0.24 1.35 0.16 0.26 1 1 5.66 0.12 0.18 0.28 0.15 0.24 5 1 3.51 0.19 0.27 -0.76 0.21 0.29 1 1 4.39 0.12 0.21 0.23 0.15 0.25 5 3 1.09 0.19 0.24 0.12 0.19 0.27 3 1 3.06 0.14 0.19 0.25 0.15 0.24 11 8 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.31 0.19 0.26 -0.16 0.20 0.27 1 1 2.59 0.17 0.21 -0.60 0.17 0.24 4 2 5.30 0.12 0.18 0.00 0.14 0.22 35 24 2.91 0.16 0.22 0.19 0.16 0.25 4 2 4.04 0.18 0.25 -0.01 0.20 0.27 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 1 0 1.01 0.17 0.24 0.24 0.17 0.26 2 2 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.30 0.13 0.19 1.37 0.16 0.23 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 7 0 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0
HE 2242-1930 33 5281 100 2.99 0.26 0.36 -2.21 0.13 0.19 1.81 0.15 0.25 6.27 0.20 0.25 0.09 0.17 0.26 1 1 5.59 0.13 0.19 0.22 0.15 0.23 7 6 3.19 0.22 0.29 -1.07 0.23 0.30 1 1 4.49 0.12 0.20 0.34 0.15 0.25 9 8 0.99 0.18 0.23 0.03 0.17 0.26 5 4 3.05 0.17 0.22 0.24 0.16 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.18 0.19 0.27 -0.28 0.18 0.26 3 3 2.89 0.16 0.21 -0.29 0.16 0.24 5 3 5.29 0.13 0.19 0.00 0.14 0.22 55 49 2.95 0.18 0.24 0.24 0.16 0.25 6 5 4.10 0.21 0.30 0.06 0.21 0.29 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.72 0.20 0.28 -0.04 0.20 0.29 3 2 -0.01 0.19 0.24 -0.04 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.18 0.24 0.29 -0.10 0.22 0.30 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.15 0.19 0.24 0.56 0.17 0.27 4 1
HE 2243-0151 41 6113 100 3.88 0.25 0.35 -1.61 0.11 0.18 1.65 0.14 0.24 7.04 0.16 0.23 0.26 0.17 0.27 1 1 6.15 0.11 0.17 0.18 0.15 0.24 7 4 3.97 0.16 0.24 -0.89 0.19 0.27 1 1 5.11 0.11 0.20 0.36 0.15 0.24 9 8 1.59 0.18 0.23 0.03 0.17 0.27 5 4 3.79 0.15 0.21 0.38 0.16 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.99 0.16 0.24 -0.07 0.17 0.25 3 3 3.37 0.14 0.20 -0.41 0.16 0.23 5 3 5.89 0.11 0.18 0.00 0.14 0.22 55 48 3.42 0.15 0.21 0.11 0.16 0.25 6 4 4.82 0.18 0.26 0.18 0.19 0.26 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 1.50 0.17 0.25 0.14 0.17 0.26 3 2 0.82 0.18 0.23 0.19 0.17 0.27 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.51 0.23 0.28 -0.01 0.22 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 0.68 0.18 0.23 0.79 0.18 0.27 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2244-1503 46 5122 100 2.57 0.25 0.35 -2.88 0.12 0.18 1.52 0.13 0.23 5.67 0.19 0.26 0.15 0.19 0.28 1 1 5.01 0.12 0.18 0.30 0.15 0.23 7 5 2.65 0.18 0.26 -0.95 0.19 0.27 1 1 3.81 0.12 0.20 0.32 0.15 0.25 9 7 0.29 0.18 0.23 -0.01 0.16 0.26 5 3 2.47 0.16 0.21 0.32 0.15 0.24 17 14 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.58 0.17 0.25 -0.23 0.17 0.25 3 3 2.01 0.17 0.22 -0.51 0.16 0.24 5 3 4.63 0.12 0.18 0.00 0.14 0.22 55 43 2.24 0.16 0.22 0.19 0.16 0.25 6 5 3.50 0.19 0.28 0.12 0.19 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.10 0.22 0.32 -0.20 0.21 0.31 3 2 -0.78 0.19 0.23 -0.15 0.17 0.26 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.29 0.23 0.29 0.45 0.21 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.41 0.18 0.23 0.95 0.17 0.27 4 3
HE 2247-3705 57 5366 100 3.04 0.24 0.34 -2.27 0.12 0.18 1.48 0.12 0.22 6.48 0.19 0.25 0.36 0.18 0.26 1 1 5.46 0.11 0.18 0.14 0.15 0.23 7 4 3.19 0.15 0.24 -1.02 0.17 0.26 1 1 4.28 0.11 0.20 0.18 0.14 0.24 9 8 1.03 0.18 0.23 0.12 0.16 0.26 5 3 2.99 0.16 0.21 0.24 0.15 0.24 17 14 1.74 0.15 0.20 0.01 0.15 0.24 3 1 3.25 0.16 0.25 -0.15 0.17 0.25 3 3 2.88 0.15 0.20 -0.25 0.15 0.23 5 4 5.24 0.12 0.18 0.00 0.14 0.22 55 53 2.97 0.16 0.23 0.32 0.16 0.25 6 6 3.87 0.20 0.28 -0.11 0.20 0.27 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.38 0.19 0.28 -0.33 0.19 0.28 3 2 -0.48 0.19 0.23 -0.46 0.17 0.27 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.96 0.19 0.24 -0.83 0.17 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2248-3345 53 5011 100 2.11 0.25 0.35 -2.74 0.12 0.18 1.71 0.13 0.23 5.88 0.19 0.26 0.21 0.18 0.28 1 1 4.78 0.12 0.18 -0.08 0.15 0.24 7 5 2.49 0.16 0.24 -1.25 0.17 0.26 1 1 3.61 0.12 0.20 -0.02 0.15 0.25 9 7 -0.03 0.18 0.23 -0.47 0.16 0.25 5 4 2.11 0.16 0.21 -0.18 0.15 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.73 0.17 0.26 -0.22 0.16 0.25 3 3 2.39 0.15 0.20 -0.27 0.15 0.23 5 3 4.77 0.12 0.18 0.00 0.14 0.22 55 53 1.99 0.16 0.22 -0.21 0.16 0.25 6 5 3.45 0.19 0.28 -0.07 0.18 0.26 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.75 0.19 0.25 -1.99 0.17 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.97 0.19 0.23 -1.37 0.17 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2250-2132 54 5705 100 3.69 0.25 0.35 -2.22 0.12 0.18 1.43 0.13 0.23 6.58 0.17 0.24 0.41 0.17 0.26 1 1 5.68 0.11 0.17 0.31 0.14 0.23 7 5 3.19 0.15 0.23 -1.07 0.16 0.26 1 1 4.43 0.11 0.19 0.29 0.14 0.24 9 8 1.44 0.17 0.23 0.49 0.16 0.26 5 5 3.15 0.16 0.21 0.35 0.15 0.24 17 13 2.17 0.15 0.20 0.39 0.15 0.24 3 1 3.34 0.16 0.23 -0.12 0.16 0.24 3 3 2.83 0.16 0.20 -0.35 0.16 0.24 5 2 5.28 0.12 0.18 0.00 0.14 0.22 55 50 2.90 0.15 0.22 0.20 0.15 0.25 6 5 4.08 0.17 0.25 0.05 0.17 0.26 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.75 0.17 0.26 -0.00 0.17 0.27 3 2 -0.02 0.19 0.24 -0.04 0.17 0.27 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.40 0.19 0.24 -0.31 0.18 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2252-4157 70 5090 100 2.87 0.24 0.34 -1.93 0.12 0.18 1.55 0.12 0.22 6.31 0.22 0.27 -0.15 0.18 0.27 1 1 5.91 0.11 0.18 0.25 0.15 0.23 7 4 3.84 0.12 0.22 -0.70 0.15 0.25 1 1 4.71 0.12 0.21 0.28 0.14 0.24 9 9 1.35 0.14 0.20 0.11 0.16 0.25 5 5 3.28 0.17 0.22 0.19 0.16 0.25 17 17 2.07 0.16 0.21 -0.00 0.15 0.24 3 3 3.65 0.14 0.23 -0.10 0.15 0.24 3 3 3.27 0.16 0.24 -0.19 0.16 0.25 5 3 5.57 0.12 0.18 0.00 0.14 0.22 55 51 3.14 0.19 0.26 0.15 0.17 0.27 6 6 3.96 0.15 0.26 -0.37 0.17 0.27 4 4 2.79 0.13 0.21 0.12 0.14 0.26 2 2 1.05 0.14 0.21 0.01 0.15 0.24 3 2 0.22 0.18 0.23 -0.09 0.16 0.27 6 6 0.96 0.18 0.23 0.29 0.16 0.27 3 2 0.49 0.15 0.20 0.29 0.16 0.24 2 1 -0.65 0.18 0.23 0.11 0.16 0.27 6 5 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.25 0.18 0.23 0.18 0.16 0.27 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.89 0.18 0.23 0.53 0.15 0.27 4 4
HE 2252-4225 68 4708 100 1.53 0.24 0.34 -2.83 0.12 0.18 1.92 0.12 0.22 5.18 0.20 0.27 -0.39 0.19 0.28 1 1 4.94 0.11 0.18 0.17 0.15 0.23 7 6 2.87 0.14 0.26 -0.78 0.17 0.27 1 1 3.68 0.12 0.20 0.14 0.14 0.25 9 8 0.31 0.17 0.22 -0.04 0.16 0.24 5 5 2.49 0.15 0.20 0.29 0.15 0.23 17 16 1.12 0.16 0.20 -0.06 0.15 0.24 3 2 2.73 0.16 0.28 -0.12 0.16 0.26 3 3 2.49 0.13 0.19 -0.08 0.15 0.23 5 5 4.68 0.12 0.18 0.00 0.14 0.22 55 51 2.22 0.15 0.22 0.12 0.15 0.24 6 6 3.70 0.17 0.28 0.26 0.16 0.26 4 4 2.39 0.13 0.20 0.61 0.14 0.25 2 2 0.21 0.17 0.27 0.06 0.17 0.27 3 2 -0.54 0.18 0.22 0.04 0.16 0.25 6 6 0.16 0.18 0.22 0.38 0.16 0.25 3 2 -0.24 0.19 0.27 0.45 0.19 0.27 2 1 -1.08 0.18 0.22 0.57 0.16 0.25 6 5 -0.70 0.18 0.24 0.54 0.16 0.27 10 4 -0.71 0.18 0.23 0.60 0.16 0.25 9 5 -0.82 0.18 0.23 0.98 0.16 0.26 8 1 -1.32 0.18 0.22 0.99 0.16 0.25 4 4
HE 2258-3456 51 4988 100 1.55 0.26 0.36 -2.97 0.12 0.18 2.00 0.13 0.23 5.22 0.19 0.26 -0.20 0.19 0.30 1 1 4.85 0.12 0.18 0.24 0.15 0.23 7 5 2.53 0.17 0.24 -0.98 0.18 0.27 1 1 3.58 0.12 0.20 0.19 0.15 0.25 9 7 0.11 0.18 0.23 -0.09 0.16 0.24 5 4 2.11 0.16 0.21 0.06 0.15 0.23 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.27 0.16 0.22 -0.43 0.15 0.23 3 3 1.48 0.17 0.21 -0.94 0.16 0.24 5 3 4.53 0.12 0.18 0.00 0.14 0.22 55 46 1.97 0.15 0.22 0.02 0.16 0.25 6 5 2.95 0.16 0.22 -0.34 0.16 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.03 0.22 0.31 -1.03 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.99 0.19 0.23 -1.15 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2259-3407 54 6266 100 4.32 0.26 0.36 -2.29 0.11 0.17 1.37 0.15 0.25 6.51 0.15 0.23 0.41 0.18 0.27 1 1 5.52 0.11 0.17 0.22 0.15 0.23 7 2 3.20 0.16 0.23 -0.98 0.17 0.26 1 1 4.36 0.11 0.19 0.29 0.15 0.25 9 6 1.01 0.18 0.23 0.13 0.18 0.27 5 2 3.13 0.15 0.21 0.40 0.16 0.24 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.23 0.13 0.19 -0.15 0.15 0.23 3 3 2.60 0.15 0.19 -0.50 0.16 0.24 5 3 5.21 0.11 0.17 0.00 0.14 0.22 55 37 2.87 0.14 0.21 0.24 0.16 0.25 6 3 3.92 0.16 0.21 -0.04 0.17 0.23 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.50 0.21 0.29 -0.18 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.68 0.19 0.24 -0.52 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2301-4024 55 5743 100 3.76 0.25 0.35 -2.11 0.11 0.17 1.60 0.13 0.23 6.59 0.17 0.24 0.30 0.17 0.26 1 1 5.68 0.11 0.18 0.20 0.14 0.23 7 5 3.39 0.14 0.23 -0.98 0.16 0.26 1 1 4.52 0.11 0.20 0.26 0.14 0.24 9 8 1.18 0.18 0.23 0.10 0.17 0.26 5 4 3.17 0.16 0.21 0.24 0.16 0.25 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.41 0.16 0.23 -0.16 0.16 0.24 3 3 2.97 0.14 0.20 -0.32 0.15 0.23 5 3 5.40 0.11 0.17 0.00 0.14 0.22 55 52 2.96 0.15 0.21 0.14 0.15 0.25 6 4 4.13 0.16 0.24 -0.03 0.17 0.25 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.87 0.16 0.26 -0.00 0.17 0.27 3 2 0.27 0.18 0.23 0.13 0.17 0.27 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.52 0.19 0.24 0.49 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -0.61 0.18 0.23 0.98 0.17 0.27 4 3
HE 2301-4126 55 5841 100 3.66 0.26 0.36 -2.37 0.13 0.19 1.53 0.14 0.24 6.41 0.17 0.24 0.39 0.17 0.27 1 1 5.43 0.11 0.17 0.22 0.15 0.24 7 4 3.18 0.14 0.22 -0.92 0.16 0.25 1 1 4.19 0.11 0.20 0.20 0.15 0.25 9 7 0.97 0.18 0.23 0.16 0.16 0.25 5 4 2.94 0.16 0.21 0.28 0.15 0.23 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.15 0.16 0.22 -0.15 0.15 0.23 3 3 2.51 0.15 0.20 -0.51 0.15 0.23 5 2 5.13 0.13 0.19 0.00 0.14 0.22 55 42 2.66 0.15 0.21 0.10 0.15 0.25 6 2 3.81 0.17 0.23 -0.07 0.16 0.23 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.53 0.21 0.30 -0.08 0.18 0.28 3 2 -0.15 0.19 0.24 -0.02 0.17 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.13 0.20 0.25 0.11 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2304-4153 58 4663 100 1.01 0.26 0.36 -3.02 0.12 0.18 2.12 0.12 0.22 4.72 0.21 0.28 -0.65 0.20 0.29 1 1 4.66 0.12 0.18 0.10 0.15 0.23 7 6 2.91 0.15 0.26 -0.54 0.18 0.28 1 1 3.50 0.12 0.20 0.16 0.14 0.24 9 7 0.19 0.16 0.22 0.04 0.15 0.24 5 5 2.13 0.15 0.20 0.14 0.15 0.23 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.33 0.15 0.24 -0.32 0.15 0.24 3 3 2.13 0.14 0.20 -0.24 0.15 0.23 5 2 4.48 0.12 0.18 0.00 0.14 0.22 55 49 1.85 0.15 0.22 -0.04 0.15 0.24 6 5 3.22 0.15 0.27 -0.00 0.17 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.68 0.19 0.26 -1.62 0.18 0.27 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.50 0.19 0.23 -1.61 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2311+0129 58 5188 100 2.65 0.25 0.35 -2.78 0.12 0.18 1.54 0.12 0.22 5.94 0.19 0.26 0.33 0.18 0.27 1 1 5.12 0.11 0.18 0.31 0.15 0.24 7 6 2.82 0.15 0.24 -0.87 0.17 0.26 1 1 3.90 0.12 0.20 0.32 0.14 0.25 9 8 0.56 0.18 0.23 0.16 0.16 0.25 5 4 2.53 0.16 0.21 0.28 0.15 0.24 17 15 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.63 0.17 0.24 -0.26 0.16 0.24 3 3 2.00 0.17 0.22 -0.61 0.16 0.23 5 3 4.72 0.12 0.18 0.00 0.14 0.22 55 49 2.35 0.16 0.22 0.21 0.15 0.25 6 6 3.50 0.18 0.26 0.03 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.29 0.18 0.28 0.09 0.18 0.28 3 2 -0.64 0.18 0.23 -0.10 0.16 0.25 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.84 0.21 0.25 -0.19 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2314-1554 52 5139 100 2.62 0.27 0.37 -3.27 0.13 0.18 1.73 0.14 0.24 5.71 0.19 0.26 0.60 0.18 0.27 1 1 4.81 0.12 0.19 0.50 0.16 0.25 7 5 2.79 0.15 0.24 -0.41 0.17 0.26 1 1 3.52 0.12 0.20 0.43 0.15 0.25 9 5 0.28 0.18 0.23 0.38 0.16 0.25 5 4 2.14 0.16 0.21 0.39 0.15 0.24 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.97 0.16 0.20 -0.42 0.15 0.22 3 3 1.11 0.17 0.21 -1.00 0.15 0.23 5 3 4.23 0.13 0.18 0.00 0.14 0.22 55 37 2.02 0.15 0.22 0.38 0.15 0.24 6 5 3.05 0.18 0.23 0.08 0.16 0.24 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.24 0.23 0.32 0.06 0.21 0.31 3 2 -0.82 0.19 0.24 0.21 0.17 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.45 0.20 0.24 -0.31 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2319-0852 36 4724 100 1.36 0.27 0.37 -3.38 0.13 0.18 1.97 0.14 0.24 4.69 0.21 0.28 -0.32 0.20 0.30 1 1 4.33 0.13 0.20 0.13 0.15 0.24 7 3 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.34 0.12 0.20 0.36 0.15 0.25 9 3 -0.06 0.18 0.22 0.14 0.16 0.24 5 3 1.88 0.16 0.21 0.24 0.15 0.23 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.74 0.16 0.22 -0.55 0.16 0.23 3 3 1.06 0.16 0.21 -0.95 0.16 0.23 5 3 4.12 0.13 0.18 0.00 0.14 0.22 55 38 1.78 0.16 0.22 0.23 0.15 0.25 6 5 3.18 0.19 0.28 0.31 0.18 0.28 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.94 0.25 0.34 -0.54 0.24 0.33 3 2 -1.30 0.20 0.24 -0.17 0.18 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.24 0.19 0.23 -1.00 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2325-0755 57 5665 100 3.17 0.27 0.37 -2.85 0.13 0.18 1.48 0.13 0.23 5.76 0.19 0.25 0.21 0.19 0.28 1 1 5.05 0.11 0.18 0.31 0.15 0.24 7 2 2.61 0.14 0.22 -1.02 0.15 0.25 1 1 3.97 0.12 0.20 0.46 0.15 0.25 9 7 0.47 0.18 0.23 0.14 0.16 0.25 5 2 2.53 0.16 0.21 0.35 0.15 0.23 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.54 0.15 0.20 -0.29 0.15 0.22 3 3 1.84 0.16 0.20 -0.71 0.15 0.23 5 3 4.65 0.13 0.18 0.00 0.14 0.22 55 37 2.18 0.15 0.22 0.10 0.15 0.25 6 2 3.23 0.16 0.21 -0.18 0.15 0.22 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.12 0.21 0.30 -0.24 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.29 0.19 0.23 -0.57 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2326+0038 54 5145 100 2.51 0.24 0.34 -2.77 0.13 0.19 1.62 0.13 0.23 5.84 0.19 0.25 0.23 0.18 0.27 1 1 5.05 0.11 0.18 0.24 0.15 0.24 7 7 2.76 0.16 0.24 -0.93 0.17 0.26 1 1 3.81 0.12 0.20 0.23 0.15 0.25 9 8 0.53 0.18 0.23 0.13 0.15 0.24 5 4 2.45 0.16 0.21 0.21 0.15 0.23 17 13 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.60 0.17 0.24 -0.30 0.16 0.24 3 3 1.91 0.17 0.21 -0.71 0.15 0.23 5 3 4.72 0.13 0.19 0.00 0.14 0.22 55 47 2.38 0.16 0.22 0.23 0.15 0.24 6 6 3.37 0.19 0.27 -0.10 0.17 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -0.26 0.23 0.33 -0.46 0.20 0.30 3 2 -1.03 0.19 0.23 -0.49 0.16 0.25 6 2 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -1.31 0.19 0.24 -0.66 0.16 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2327-5642 69 5048 100 2.22 0.25 0.35 -2.95 0.12 0.18 1.69 0.12 0.22 5.88 0.19 0.26 0.43 0.19 0.29 1 1 4.79 0.11 0.18 0.14 0.15 0.24 7 6 2.63 0.14 0.23 -0.90 0.16 0.25 1 1 3.60 0.12 0.20 0.18 0.15 0.25 9 7 0.17 0.18 0.23 -0.06 0.16 0.25 5 4 2.14 0.16 0.21 0.06 0.15 0.24 17 12 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.32 0.16 0.23 -0.42 0.16 0.23 3 3 1.78 0.17 0.22 -0.68 0.16 0.24 5 3 4.57 0.12 0.18 0.00 0.14 0.22 55 50 2.14 0.16 0.22 0.15 0.16 0.25 6 5 3.32 0.16 0.25 0.01 0.16 0.25 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.34 0.18 0.28 0.31 0.18 0.27 3 2 -0.57 0.18 0.23 0.12 0.17 0.26 6 3 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.14 0.21 0.28 0.66 0.19 0.27 2 1 -1.10 0.18 0.23 0.67 0.17 0.26 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -0.69 0.18 0.23 0.74 0.17 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -1.20 0.18 0.23 1.22 0.17 0.26 4 4
HE 2329-3702 38 6060 100 3.72 0.28 0.38 -2.16 0.12 0.18 1.65 0.15 0.25 6.39 0.20 0.26 0.15 0.21 0.30 1 1 5.74 0.11 0.17 0.31 0.15 0.24 7 3 3.26 0.15 0.23 -1.06 0.17 0.26 1 1 4.65 0.11 0.20 0.44 0.15 0.25 9 8 1.23 0.18 0.24 0.21 0.17 0.26 5 3 3.29 0.16 0.21 0.42 0.15 0.24 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.35 0.16 0.22 -0.17 0.16 0.23 3 3 2.66 0.15 0.20 -0.58 0.16 0.24 5 3 5.35 0.12 0.18 0.00 0.14 0.22 55 40 2.81 0.15 0.21 0.04 0.16 0.25 6 1 3.88 0.16 0.21 -0.22 0.16 0.23 4 1 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.96 0.21 0.30 0.14 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.16 0.20 0.24 -0.14 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2333-1358 40 5020 100 2.15 0.29 0.39 -3.34 0.13 0.18 1.57 0.15 0.25 5.38 0.20 0.27 0.33 0.19 0.29 1 1 4.70 0.12 0.19 0.46 0.16 0.24 7 4 2.20 0.17 0.24 -0.93 0.17 0.26 1 1 3.28 0.12 0.20 0.26 0.15 0.25 9 3 0.16 0.18 0.23 0.33 0.17 0.25 5 4 1.80 0.18 0.23 0.12 0.16 0.25 17 8 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.80 0.23 0.28 -0.53 0.19 0.27 3 3 1.26 0.17 0.21 -0.79 0.16 0.24 5 3 4.16 0.13 0.18 0.00 0.14 0.22 55 32 1.98 0.16 0.22 0.40 0.15 0.25 6 5 3.21 0.19 0.27 0.31 0.18 0.27 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -2.24 0.20 0.26 -1.87 0.18 0.28 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2334-0604 72 4820 100 1.51 0.25 0.35 -3.41 0.13 0.18 2.15 0.11 0.21 4.32 0.22 0.28 -0.67 0.20 0.30 1 1 4.23 0.12 0.19 0.06 0.15 0.23 7 4 2.71 0.14 0.24 -0.36 0.16 0.26 1 1 3.05 0.12 0.20 0.10 0.15 0.25 9 3 -0.25 0.17 0.22 -0.02 0.15 0.24 5 4 1.61 0.16 0.21 -0.00 0.15 0.23 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 1.68 0.15 0.20 -0.59 0.15 0.22 3 3 1.26 0.16 0.21 -0.72 0.15 0.23 5 3 4.09 0.13 0.18 0.00 0.14 0.22 55 44 1.73 0.15 0.22 0.22 0.15 0.24 6 5 2.82 0.16 0.22 -0.03 0.15 0.23 4 4 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -1.28 0.19 0.27 -0.84 0.17 0.27 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -2.58 0.19 0.23 -1.30 0.16 0.24 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2335-5958B 37 5765 100 3.24 0.28 0.38 -2.33 0.13 0.18 1.63 0.14 0.24 6.15 0.19 0.26 0.08 0.20 0.29 1 1 5.47 0.12 0.18 0.21 0.15 0.24 7 3 3.10 0.18 0.24 -1.05 0.18 0.27 1 1 4.45 0.12 0.20 0.41 0.15 0.25 9 8 0.93 0.17 0.23 0.08 0.16 0.25 5 3 3.01 0.16 0.21 0.31 0.15 0.23 17 10 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.25 0.17 0.24 -0.10 0.16 0.24 3 3 2.57 0.16 0.21 -0.50 0.16 0.23 5 3 5.18 0.13 0.18 0.00 0.14 0.22 55 42 2.73 0.15 0.22 0.13 0.16 0.25 6 3 4.03 0.20 0.27 0.10 0.18 0.26 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.60 0.23 0.33 -0.05 0.21 0.31 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.51 0.21 0.25 -0.32 0.18 0.26 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2338-1311 20 5582 100 3.50 0.28 0.38 -2.86 0.13 0.18 1.27 0.18 0.28 5.87 0.19 0.25 0.34 0.18 0.27 1 1 5.10 0.12 0.18 0.38 0.16 0.25 7 1 -9.99 0.00 0.00 -9.99 0.00 0.00 0 0 3.82 0.12 0.20 0.32 0.15 0.25 9 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 2.52 0.16 0.21 0.36 0.16 0.24 17 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.57 0.15 0.21 -0.24 0.15 0.23 3 1 -9.99 0.00 0.00 -9.99 0.00 0.00 5 0 4.64 0.13 0.18 0.00 0.14 0.22 55 16 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2338-1618 40 5515 100 3.38 0.27 0.37 -2.65 0.12 0.18 1.43 0.16 0.26 6.22 0.18 0.25 0.47 0.18 0.27 1 1 5.10 0.12 0.18 0.16 0.15 0.24 7 2 2.86 0.16 0.24 -0.97 0.17 0.26 1 1 3.94 0.12 0.20 0.23 0.15 0.25 9 6 0.61 0.18 0.23 0.08 0.18 0.27 5 2 2.55 0.16 0.21 0.17 0.16 0.25 17 7 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 2.87 0.18 0.24 -0.16 0.18 0.25 3 3 2.12 0.16 0.21 -0.62 0.16 0.24 5 3 4.86 0.12 0.18 0.00 0.14 0.22 55 38 2.61 0.16 0.22 0.34 0.16 0.25 6 3 3.82 0.21 0.27 0.21 0.19 0.26 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.11 0.23 0.32 -0.22 0.22 0.32 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2345-1919 44 5617 100 4.46 0.25 0.35 -2.46 0.12 0.18 1.47 0.16 0.26 6.17 0.19 0.24 0.24 0.17 0.26 1 1 5.45 0.12 0.18 0.33 0.14 0.24 7 3 3.42 0.13 0.23 -0.59 0.16 0.25 1 1 4.15 0.12 0.20 0.25 0.14 0.25 9 8 0.68 0.18 0.23 -0.03 0.17 0.28 5 2 2.78 0.16 0.21 0.22 0.16 0.26 17 9 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.13 0.15 0.22 -0.08 0.16 0.24 3 3 2.51 0.15 0.21 -0.41 0.16 0.24 5 3 5.04 0.12 0.18 0.00 0.14 0.22 55 39 2.63 0.16 0.22 0.17 0.16 0.26 6 3 3.78 0.16 0.22 -0.01 0.17 0.24 4 3 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.23 0.18 0.25 -0.28 0.19 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.79 0.19 0.24 -0.45 0.18 0.29 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2347-1254 80 6132 100 3.95 0.24 0.34 -1.83 0.13 0.18 1.67 0.12 0.22 6.83 0.15 0.22 0.27 0.16 0.26 1 1 6.04 0.11 0.17 0.29 0.15 0.23 7 4 3.90 0.12 0.22 -0.74 0.15 0.25 1 1 4.90 0.11 0.20 0.37 0.15 0.25 9 9 1.60 0.17 0.22 0.26 0.15 0.24 5 4 3.58 0.15 0.20 0.39 0.14 0.23 17 14 2.39 0.14 0.19 0.22 0.15 0.23 3 1 3.72 0.15 0.22 -0.13 0.15 0.23 3 3 3.17 0.15 0.20 -0.39 0.15 0.23 5 3 5.67 0.13 0.18 0.00 0.14 0.22 55 53 3.23 0.14 0.21 0.14 0.15 0.24 6 4 4.26 0.16 0.22 -0.16 0.16 0.23 4 2 2.90 0.13 0.20 0.13 0.15 0.25 2 1 1.36 0.16 0.25 0.21 0.16 0.26 3 2 0.57 0.17 0.22 0.16 0.15 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 0.31 0.20 0.25 0.01 0.17 0.25 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0
HE 2347-1334 81 4453 100 0.95 0.24 0.34 -2.55 0.12 0.19 2.38 0.11 0.21 5.33 0.21 0.26 -0.50 0.18 0.27 1 1 5.31 0.12 0.19 0.28 0.15 0.23 7 5 3.32 0.15 0.25 -0.59 0.16 0.26 1 1 3.97 0.11 0.20 0.17 0.14 0.24 9 9 0.59 0.15 0.20 -0.02 0.14 0.23 5 5 2.51 0.15 0.20 0.05 0.15 0.23 17 17 1.23 0.16 0.20 -0.22 0.15 0.23 3 3 2.61 0.19 0.29 -0.50 0.17 0.26 3 3 2.38 0.14 0.20 -0.45 0.15 0.23 5 5 4.94 0.12 0.19 0.00 0.14 0.22 55 54 2.26 0.17 0.24 -0.10 0.16 0.25 6 6 3.62 0.31 0.38 -0.07 0.26 0.34 4 4 2.16 0.12 0.20 0.12 0.14 0.25 2 2 0.20 0.16 0.23 -0.21 0.15 0.25 3 1 -0.61 0.17 0.22 -0.30 0.14 0.24 6 6 0.15 0.17 0.21 0.11 0.14 0.25 3 2 -1.21 0.19 0.25 -0.78 0.17 0.26 2 1 -1.88 0.17 0.21 -0.49 0.14 0.25 6 1 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -1.49 0.18 0.23 -0.43 0.15 0.26 9 2 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -2.30 0.18 0.22 -0.25 0.15 0.26 4 3
HE 2347-1448 43 6162 100 3.98 0.27 0.37 -2.31 0.12 0.18 0.84 0.17 0.27 6.58 0.18 0.24 0.50 0.19 0.27 1 1 5.40 0.12 0.18 0.13 0.15 0.24 7 1 3.05 0.16 0.22 -1.11 0.17 0.26 1 1 4.25 0.11 0.20 0.21 0.15 0.25 9 3 0.93 0.18 0.23 0.07 0.18 0.27 5 2 3.01 0.16 0.21 0.31 0.16 0.25 17 5 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 3.31 0.16 0.22 -0.05 0.17 0.24 3 3 2.40 0.16 0.20 -0.68 0.16 0.25 5 1 5.19 0.12 0.18 0.00 0.14 0.22 55 32 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 4.21 0.21 0.27 0.27 0.21 0.27 4 2 -9.99 0.00 0.00 -9.99 0.00 0.00 2 0 0.74 0.20 0.29 0.08 0.20 0.29 3 2 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 3 0 -0.34 0.19 0.24 -0.16 0.19 0.27 2 1 -9.99 0.00 0.00 -9.99 0.00 0.00 6 0 -9.99 0.00 0.00 -9.99 0.00 0.00 10 0 -9.99 0.00 0.00 -9.99 0.00 0.00 9 0 -9.99 0.00 0.00 -9.99 0.00 0.00 8 0 -9.99 0.00 0.00 -9.99 0.00 0.00 4 0




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