A&A 476, 1205-1217 (2007)
DOI: 10.1051/0004-6361:20077342
A. Dobrzycki1 - M. Nikolajuk2 - J. Bechtold3 - H. Ebeling4 - B. Czerny5 - A. Rózanska5
1 - ESO, Karl-Schwarzschild-Strasse 2, 85748 Garching bei München, Germany
2 -
Faculty of Physics, University of Biaystok, Lipowa 41, 15424
Bia
ystok, Poland
3 -
Steward Observatory, University of Arizona, Tucson, AZ 85721, USA
4 -
Institute for Astronomy, University of Hawai'i, 2680 Woodlawn Drive,
Honolulu, HI 96822, USA
5 -
Copernicus Astronomical Center, Bartycka 18, 00716 Warszawa, Poland
Received 22 February 2007 / Accepted 27 September 2007
Abstract
Context. We present multi-wavelength observations of the bright quasar HS1603+3820: the optical data taken with the MMT and Keck telescopes, with the 40-50 kms-1 resolution, and X-ray data taken by the Chandra X-ray Observatory satellite.
Aims. The optical spectra contain a very large number of absorption lines from numerous heavy elements. Our goal is to analyze these features to obtain constraints on the properties of associated absorbers, to be used in modeling of the quasar intrinsic flux and properties of the clouds.
Methods. We have determined the properties - column densities and redshifts - of the individual components. We derived the X-ray properties of HS1603+3820 and the optical-to-X-ray slope index
.
Results. We found
of 1.70, which is at the high end of the typical range for a radio quiet quasar. We found 49 individual heavy element absorption clouds, which can be grouped into eleven distinct systems. Absorbers from the associated system, which likely is the one spatially closest to the quasar, show large C IV to H I column density ratio, reaching
20.
Conclusions. Intrinsic X-ray properties of the quasar are typical. Determination of column densities of ions (including hydrogen) gives a strong foundation for modeling of the quasar ionising flux.
Key words: quasars: absorption lines - quasars: individual: HS1603+3820
HS1603+3820 is a
quasar discovered during the
Hamburg/CfA Bright Quasar Survey (Dobrzycki et al. 1996). With B=15.9,
it is among the top few brightest quasars known in the
redshift interval (Véron-Cetty & Véron 2006). The most striking feature of HS1603+3820 is, however, the extreme richness of its heavy element absorption
spectrum, and in particular, the
absorption.
The absorption spectrum of HS1603+3820 was first described in Dobrzycki et al. (1999, hereafter D99), dobrzycki1999D99 based on medium-resolution (90-100 kms-1) spectrum obtained in 1997 April with the MMT and the Blue Channel spectrograph. Although in this spectrum many of the absorption systems were blended, it was clear that the quasar held great promise for the analysis of the properties of associated absorbers.
The absorption systems that are spatially close to the quasar can be used as probes for the intrinsic emission of the quasar itself, since the conditions in the systems are undoubtedly heavily influenced by the quasar flux (e.g. Gabel et al. 2005; Crenshaw et al. 2003; Scott et al. 2005, and references therein). Systems that contain lines originating from various species and various ionisation levels are particularly interesting, since they can provide an independent way of determining physical properties of the absorbing medium, which can cast light at the intrinsic quasar continuum in the far UV band as well as the absorbing cloud formation.
With that as the principal goal, we initiated a project of multi-wavelength observations of HS1603+3820, aiming to obtain spectral information at various wavelengths. In this paper we present the results of our X-ray and optical observations of the quasar. In the forthcoming paper (Rózanska et al. 2007, in preparation, Paper II), we use those observations to constrain models of the quasar broad band continuum and the cloud confinement.
misawa2003M03 misawa2005M05 In the meantime, Misawa et al. (2005, hereafter referred to as M03 and M05, respectively,2003) observed HS1603+3820 in 2002 March and 2003 July in very high resolution (6.7 kms-1), using the Subaru telescope with the High Dispersion Spectrograph. The primary goal of these observations was to establish the nature of the absorbers (intervening or associated), using the analysis of line time variability, partial coverage and profile shapes. High resolution of their observations enabled resolving many of the systems into a number of narrow components. M03 and M05 grouped the absorbers into several systems, designated with the letters from A to H. In our optical spectroscopy data we see all those systems and three additional intervening systems. For consistency, and to enable easy comparisons, wherever possible we will use these designations throughout this paper.
In a very recent paper, Misawa et al. (2007, hereafter M07) misawa2007M07 expanded the analysis of absorber variability, using new spectra from the Subaru and Hobby-Eberly telescopes, and confirmed the finding from misawa2005 that C IV in System A is highly variable. This paper also described one system (labeled I) that they did not have in their older data. This system was seen in our data, and for consistency with misawa2007 we rewrote parts of this paper to also use this designation.
Our optical spectra are of lower resolution (FWHM of
40-50 kms-1), but
they complement the Subaru data in two important areas: they have
higher signal-to-noise ratio (100-140 per pixel in the C IV and Ly
regions) and they cover much larger wavelength range (
3700 to
10 000 Å). The former reduces uncertainty in blended regions
containing thick lines and helps in finding weak lines, while the
latter allows analyzing lines from species inaccessible in the Subaru
spectra. The most important addition is detection and
analysis of hydrogen lines, not seen in Misawa et al.'s spectra,
as well as detection of heavy-element lines other than C IV in System A.
This paper is organised as follows. In Sect. 2 we discuss the Chandra X-ray observation of HS1603+3820. In Sect. 3 we present our optical observations of HS1603+3820, and we discuss the individual systems and compare our results with those of Misawa et al., discussing the possible sources of discrepancies. We comment on the absorber variability in Sect. 4. We summarize the results in Sect. 5.
HS1603+3820 was observed for 9.2 ks with the Chandra X-ray Observatory on 2002 November 29 (ObsID 4026), with the 128 row subarray of the ACIS-S3 chip in VFAINT mode, with frame time of 0.4 s. The effective good time for the observation was 8.3 ks.
The data were reduced using the tools available in the CIAO v. 3.3 and
SHERPA software packages, using
Chandra calibration database (CALDB) v. 3.2.1. Because of large
calibration uncertainties for soft X-rays, the data with E<0.5 keV
were excluded from the analysis. We extracted source and background
spectra from the regions around the quasar using dmextract. In
total, the net photon yield from the quasar was 145 photons, allowing
for most fundamental spectral fits only. We note that the ACIS pile-up
is not a problem, both because of the low source count rate and
because of the low frame time resulting from the use of the chip
subarray.
We performed spectral fits with SHERPA, applying the newest gain
corrections to the event list. We performed the fit assuming the
intrinsic quasar spectrum to be a power law,
,
with
fixed Galactic absorption towards HS1603+3820 of
cm-2, as obtained with
COLDEN
. The best
fit gave the photon spectral index of
and
normalization at (rest) 1 keV of
photons cm-2 s-1 keV-1. The slope of the spectrum is
within the typical range for quasars
(e.g. Reeves & Turner 2000; Fiore et al. 1998). The spectrum and the fit are
shown in Fig. 1. We also attempted fits in which we
allowed for additional absorption from the quasar, but there was no
improvement in the fit.
![]() |
Figure 1: Chandra ACIS-S3 X-ray spectrum of HS1603+3820 and best fit power law plus Galactic absorption. The bottom panels shows the fit residuals. |
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The combination of the above result with the spectrophotometric data from
Scott et al. (2000) yields the value of the optical-to-X-ray slope,
,
of 1.70, which is at the high end of the typical parameter range at
(Bechtold et al. 2003).
HS1603+3820 has been observed by us with two instruments. On 2001 August 19
we used the ESI, Echelle Spectrograph and Imager (Sheinis et al. 2002),
on the Keck II telescope, with the MIT-LL 2048 4096 CCD, with
the 0.5
slit. Observing conditions were excellent throughout
the night, with clear sky and seeing of the order of 0.7
.
The
combined exposure time was 4800 s. The usable part of the spectrum
covered the
3900 to
10 000 Å wavelength range and had
the resolution of 45-50 kms-1, with the signal-to-noise ratio
peaking at
140 (per pixel) near the Ly
emission line,
gradually falling to
100 near the C IV emission line and then
to
70 in the red end.
On 2003 June 21 we used the Blue Channel Spectrograph on the MMT, in
the echelette/cross-dispersed mode, using the Lesser
2688 512
"ccd35'' detector with the 1
slit. The observing conditions
were variable. Seeing became worse at the end of the night, reaching
2 arcsec, and the conditions were adversely affected by the moon
age of
0.75 and smoke from forest fires. The combined exposure
time was 18 000 s. The usable spectrum ranged from
3750 to
7100 Å and had the resolution of 40-45 kms-1. The
signal-to-noise ratio in this spectrum is in the 110-130 (per pixel)
range throughout the entire wavelength range.
For both sets of observations, the initial reduction was done in the standard way with IRAF. We note that despite several attempts, the extracted MMT spectrum appears to show residual flux. Even lines that are clearly saturated, which in the Keck spectrum have black cores, do not reach zero intensity in their bottom in the MMT spectrum. We elected to not correct manually for this effect, but we note that this will likely result in underestimating the column density of the very strong lines in the MMT spectrum.
After extracting the spectra from individual orders, we performed the continuum fits to the spectra with the use of the FINDSL programme (Aldcroft et al. 1994). The spectra were then normalized, rebinned to common wavelength pixels and co-added, weighed with the variance.
Not surprisingly, the trickiest part of this part of the analysis was
the continuum fits. The spectra are heavily absorbed bluewards of the
Ly
emission line. To fit continua in the uncertain areas, we
applied a technique similar to the one described in
misawa2003, i.e., utilizing the spectrum shapes in the
unabsorbed orders. We note that this effect is less pronounced in our
case, since a single echelle order in our spectra - which have lower
resolution than the Subaru spectra - covers a larger wavelength
range, providing for more possibilities to "anchor'' the continuum.
However, the continuum fits remain uncertain in two particularly heavily blended areas. Comparison between continuum location in the normalized spectra from Keck and MMT shows that there remains a 15-20% uncertainty in those regions. In one case, it is partly caused by the fact that one of the ESI echelle orders ends inside the blended region, forcing manual anchoring of the continuum fit. In the other case, it is the fact that the blended region is on the wing of the emission line, which coincides with the peak sensitivity of the echelle order; this results in a very uncertain shape of the continuum exactly where the technique of using shapes from unabsorbed regions cannot be applied. We will return to this issue in Sect. 3.1.1.
Table 1:
Lines from System A (
)
detected in the Keck spectrum.
Table 2:
Lines from System B (
)
detected in the Keck spectrum.
Table 3: Lines from Systems C and D detected in the Keck spectrum.
Table 4: Lines from Systems E-K detected in the Keck spectrum.
Table 5: Total column densities of ions detected in the Keck spectrum.
We note that our continuum fits generally appear to agree well with Misawa et al.'s analysis of their data. One notable exception will be discussed in more detail in Sect. 3.1.1.
The next step in the analysis - resolving and identifying absorption lines - was a very laborious process, since our spectra were heavily blended. In order to avoid bias, we performed the fits blindly, i.e., we decided not to use the information from Misawa et al. As a consequence, our results do differ quite significantly in some cases, especially in the number of individual components, into which some of the systems were resolved. However, since the primary goal of our analysis is to obtain information on the the column densities of as many ions as possible in order to use them as constraints for the modeling of the quasar intrinsic emission, the important information is the total column density in the system, and not the number of the individual components. In this regard, in the systems we have in common - primarily the vicinity of the C IV emission line - our results do qualitatively agree with those of misawa2003 and misawa2005.
The line fits were done using VPGUESS/VPFIT
tools. This programme fits
multiple Voigt profiles, with absorption redshift
,
column density N and Doppler parameter b as the
fitted parameters, and it is very well suited for analysis of blended
spectra. However, our spectra are exceptionally crowded and in some
cases we had to use simplifying assumptions in order to prevent the
programme from performing fits that were obviously non-physical. We
also had to apply some judgement calls. The cases where it was
necessary are mentioned in the following subsections. We note that the
absorption spectrum of HS1603+3820 is so complex and so severely blended that
misawa2003 and misawa2005 had to resort to
a similar approach, even in the Subaru spectrum, which had markedly
higher resolution.
A large part of the work presented in misawa2005 was
devoted to the analysis of partial coverage of the QSO by the
absorbers. It is clear that at least some of the absorbers in the
vicinity of the quasar do not entirely cover the continuum emitting
region. In our analysis, we accounted for this effect only in the one
case where it was clearly necessary to obtain physically sound
parameter fits - the thick C IV lines in System A (see
Sect. 3.1.1), which were clearly saturated but did not
reach zero intensity in the line bottoms. We note that
misawa2005 presented arguments indicating that other
systems - including those with
- may also show
partial coverage. We will discuss this during the description of the
relevant systems.
The resolution of our spectra was slightly higher than the expected
values of the Doppler parameter for heavy element lines. High
resolution data from Subaru indicated that in many cases the metal
lines had b as low as 5 kms-1, while FWHM of 40-50 kms-1 translates (for Gaussian lines) to
kms-1. On the other
hand, many lines have b comparable to the spectrum resolution or
higher. In our analysis of the spectra we thus used the iterative
approach. We first freed all parameters in all fitted lines. Then for
all lines where the resulting value of the Doppler parameter was
significantly below the resolution, we fixed b at the value that
corresponded to the value of the parameter for other lines for which
it was well established (using values for other metal lines
wherever it was possible and hydrogen lines in other cases),
scaled with the square root of the element's atomic mass,
and re-ran the fit. In the situation where one or more lines had
inconsistent values of the Doppler parameter, we investigated the
possibility of having the line as a blend with other features.
It is relatively easy to fall into the trap of adding narrow lines in order to improve the fits of large features. We avoided this issue by adding lines only if it resulted in significant improvement of the fit, and all cases when this was done were individually examined.
In total, we found 49 individual absorption clouds, which can be grouped into eleven distinct "systems''. We stress that the systems are defined based on their proximity in the spectrum, and the fact that two absorbers are considered members of the same system does not in principle mean that they are physically related.
In Tables 1-4 we show line lists from all
systems detected in the spectra from Keck/ESI. In the tables, the
first column shows the line designation; the first component refers to
the separate cloud within the considered system, and the second part,
after the dot, is the ordinal number of individual lines seen in this
cloud. The second column gives the ion identification (ID). The
following columns give the absorption redshift, the Doppler parameter,
column density and (in Table 1) the covering factor, ,
as defined in Hamann et al. (1997). The last column gives (where
available) the line identification in misawa2005. We mark
lines for which the derivation of parameters is made uncertain by
blending and/or by the fact that the line is saturated. The line lists
from the MMT/Blue Channel spectrum, as well as the entire Keck and MMT
spectra, are available on the World Wide Web at
http://alpha.uwb.edu.pl/mrk/hs1603/. In addition, in
Table 5 we list the total column densities of all ions
detected in all systems and compare them to the values found in the
Subaru data. The following section contains more detailed discussion
of the individual systems.
Of the eleven distinct systems, four (A-D) are close to the emission
redshift of the quasar. The ejection velocities range from
10 000 kms-1 for System A to negative (i.e.
)
1200 kms-1 for System D.
Figure 2 shows the Keck spectrum of HS1603+3820 in the
vicinity of the emission redshift of the quasar for several
absorbers. One can clearly see that some of the systems contain lines
from several species.
![]() |
Figure 2: The fragments of the Keck spectrum of HS1603+3820 plotted in the same redshift range for several absorption features. Systems A-D are shown as shaded areas. The Mg II lines are near the very red end of the spectrum, and the "emission'' features seen in their vicinity are residuals of sky lines. The dotted vertical line shows the adopted location of the QSO emission redshift. |
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Five heavy-element absorbers were recognized in this system in the
medium-resolution data of dobrzycki1999. At least one of
the components, at
,
was identified as associated, since
the
ratio was 1, indicating that
the cloud was optically thick, yet the lines did not reach zero
intensity in their bottoms, suggesting that the cloud in which the
lines originated did not obscure the entire continuum emitting source.
misawa2003 decomposed this system into seven individual components, while misawa2005 increased this number to fifteen systems. Their analysis also confirmed that the absorbers do not appear to entirely cover the quasar, and they found indication that this system is variable. These findings were confirmed and expanded in the recent paper misawa2007.
![]() |
Figure 3:
The sample raw spectra from Keck ( left panel) and MMT
( right panel) as extracted from the echelle order, prior to continuum
fitting. The dotted lines show the ![]() |
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System A is unambiguously associated with HS1603+3820, and at the same time it
has a large relative velocity with respect to the quasar (ranging from
7500 to
10 000 kms-1), which means that it is almost
certainly located very close to the quasar central engine and its
properties are very likely determined by the radiation from the
quasar. This system is thus the ideal candidate for the modeling of
the quasar continuum.
In our analysis, we found twenty two components belonging to
System A. The results are listed in Table 1; we show the
Ly
and C IV lines in Fig. 4. For the thick
absorbers in the blue end of the system we applied the correction for
partial covering using empirically determined covering factors (listed
in Table 1). We estimate the uncertainty of the covering
factor to be of the order of
10%; the values agree
qualitatively with the values found in the Subaru data.
Our results for System A cannot be directly compared with the results from Subaru, since at least four of the components seen in our spectra (Nos. 19-22 in Table 1) result from the difference between the continuum fits in both sets of data.
In their analysis, Misawa et al. (also in their very recent paper)
treated the wavelength region between 5345 and
5360 Å as unabsorbed (see Fig. 4 in misawa2005 or Fig. 2 in
misawa2007). However, this region clearly contains
absorption in both the Keck and MMT data. In Fig. 3 we
show the raw spectra of this region from both the Keck and MMT
observations. In both cases one can clearly see that the continuum
does drop bluewards of
5360 Å, and we had to fit lines in this
region in order to account for this drop. This was actually a
difficult task, since it was hard to resolve the dip into individual
systems. We primarily relied on the information from the Ly
region,
where strong, but heavily blended absorption was present. We found
that at least four systems (i.e. Nos. 19-22) with reasonable
properties are necessary to satisfactorily fit this region. However,
while we are confident that the absorbers are present in this region,
we have to treat their derived physical parameters as somewhat
uncertain. We note that if the derived densities are taken at face
value, then the four systems contain of the order 20% of all H I column density in System A, but only 2% of the C IV column density;
this would suggest that the presence of those clouds in the vicinity
of System A is coincidental and there is no physical relation between
them and the system absorbers.
The other place in the System A area where there is a difference
between our analysis and the results from misawa2005 is
the 5308-5317 Å region. This area contains the
Si II(
1527) absorption from System B (it is the feature near
Å in Fig. 4). We obtained a very
good fit using eight lines, compared with 11 lines used in
misawa2005. We note, however, that in the earlier
analysis misawa2003 also used 8 lines.
![]() |
Figure 4:
Absorption lines from System A. Top panel: C IV(![]() ![]() ![]() |
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Even though it is a heavily blended region, our analysis was aided by
the fact that our spectra cover large wavelength ranges and contain
other Si II lines from System B, which we could use to constrain the
properties of the 1527 transition. Those lines clearly
indicated that this line is not as strong as described in
misawa2005. However, this also indicated that this region
had to contain additional C IV lines. We added new C IV doublets,
which are labeled with 5, 6 and 7 in Fig. 4 and
Table 1, and we also added line No. 3. Both spectra, and
especially the Keck spectrum, show that these doublets are
required. Additionally, we split misawa2005's line No. 1
into two lines - our doublets Nos. 1 and 2. This significantly
improved our fit.
In System A, we also identified the Si IV, Si III, and N V lines. We
show the Si IV lines in Fig. 5; the lines from the
latter two ions are in the heavily crowded Ly
forest region. We
note that the Si IV absorption was not seen in Misawa et al.'s data,
even in the spectrum generated by coadding all the Subaru spectra
misawa2007. This is clearly because of the high
signal-to-noise ratio in our spectra.
![]() |
Figure 5:
The Si IV
![]() |
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We note that the components in System A have a rather large
value of the C IV/H I column density ratio, higher than 1 in
virtually all cases and reaching 20 in the extreme case. This is
seen in both Keck (Table 1) and MMT spectra, and has
strong implications for the modeling of the intrinsic spectrum of the
quasar (Paper II). This effect is not seen in other systems, where
practically all components have
.
Our determination of the C IV column density agrees well with the value obtained in the Subaru data (Table 5). As mentioned earlier, none of the other ions seen in our spectra were seen in Misawa et al.'s data.
Finally, we would like to confirm the suspicion first expressed in
misawa2003 that the feature at 5527 Å in the
dobrzycki1999 spectrum is not a
Fe II(1608) line at
.
This feature is not
present in our Keck and MMT data, and a close examination of the raw 1997 data revealed that it was in fact an artifact caused by a cosmic
ray hit.
Even the medium resolution spectrum from dobrzycki1999
clearly showed that this is a strong and complex system. The Ly
absorption was very broad, and its non-symmetric profile hinted that
it is in fact a blend of at least a few lines.
The Subaru spectrum allowed this complex to be resolved into 18-19
separate components. As mentioned earlier, our spectra could be
satisfactorily fitted with only eight clouds. We show the vicinity of
Ly
and C IV lines in Fig. 6. The derived properties
of all lines are listed in Table 2. Note that this system
contains lines from as many as fourteen distinct ions.
It needs to be noted, however, that in a few cases the line properties
are uncertain. In particular, the seemingly large column densities of
some of the Si III(1206) lines (Nos. 2 and 6 in
Table 2) very likely originate from blending with the
hydrogen lines. Several other components are also likely affected by
features in the spectra; some of those features may be unidentified
lines, while some are very likely to be spectral artifacts. All those
cases are marked in Table 2.
Also, direct fit of Si II (7.Si II in Table 2) and 4.Fe II in the Keck spectrum resulted in unrealistically high column densities. This was confirmed by visual inspection. The only workaround was to perform the fit to those lines by trial-and-error, then fix the column density for those components, and then refit the whole spectrum again.
The 4.O I lines near 4531Å are affected by the C IV doublet
from the J system (see below).
The reality of the 5.Al III, 5.Al II and 5.Fe II lines is somewhat uncertain. The programme fitted the lines and they were seen in visual inspection of the spectrum, and we decided to keep them in Table 2. However, we note that the lines themselves and their vicinity are rather noisy.
Total ion column densities seen in our spectra agree well with those seen in the Subaru data (Table 5). Differences can be seen for some ions, but they can be resolved when blends and suspected blends are taken into account.
![]() |
Figure 6:
System B: the C IV ( upper panel) and Ly![]() |
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This system (see Fig. 7) is very close to the emission
redshift of the quasar. In dobrzycki1999 it was
considered to be in-falling because of the QSO emission redshift of
2.51 adopted in this paper. However, the arguments presented in
misawa2003 favoring a higher value of the emission
redshift,
,
are convincing and we adopt this value in both
this paper and in Paper II.
The derived properties of C IV absorption (see Table 3)
in this system agree well with the Subaru data. In our data we also
see the Ly
line. There is no significant absorption seen in other
lines, including Mg II.
![]() |
Figure 7:
The C IV ( upper panel) and Ly![]() |
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![]() |
Figure 8: As in Fig. 7, for System D. |
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This system is undoubtedly a
system (see
Fig. 8), even with the QSO emission redshift of 2.54. The natural explanation is that this system is infalling onto
the quasar.
Misawa et al. resolved this system into four separate components, and
we see the very same absorbers in our data. For all of them we
identify Ly
and C IV lines.
The stronger two components (lines Nos. 3 and 4 in Fig. 8 and Table 3) also show Si IV and N V lines. We list N V only under component No. 4, but it is very likely a blend of components Nos. 3 and 4, since both lines in the doublet are broader than what would be expected based on the value of the Doppler parameter of the other lines. The nitrogen absorption is certainly real, but the troughs are shallow and are only visible because of high signal-to-noise of our spectra; resolving it into two components would be meaningless.
In the case of the Keck spectrum, the fits of the Ly
lines Nos. 3 and 4 were diverging when they were combined with lines from other ions.
We therefore fitted them separately and then fixed the values; this is
reflected in Table 3, where their values of N and bare listed as fixed.
We also note that the H I line No. 1 in the Keck spectrum shows an unusually low value of the Doppler parameter. However, this was confirmed by the visual inspection of the spectrum: the line is isolated but does appear to be very narrow. Since the corresponding C IV absorption is unambiguously identified, we have no doubts about the reality of this line, and we attribute the unusually low measured value of b to noise fluke.
The spectrum of HS1603+3820 contains several other heavy-element systems at
.
We identified seven of them in our spectra; the lists
of lines are shown in Table 4. Four of those systems, E
(
), F (
), G (
), and H
(
), were identified in the early Subaru spectra, while
System I (
)
was described in the recent paper by
misawa2007.
In almost all cases, the properties derived from our spectra match
reasonably well with those from the Subaru data. The two exceptions
are the Nos. 3 and 4 C IV lines from System F. In the first case
misawa2003 and misawa2005 have a doublet of
lines of similar strength separated by 7 kms-1, which in our
spectrum is not deblended, and the second case is a weak line buried
in a nearby, stronger line. The total column density derived
from our data does, however, agree well with the Subaru value
(Table 5).
Although the Si IV(
1394,1403) lines in System E
(Fig. 9) lie in the Ly
forest, they are clearly
identified in both Keck and MMT spectra. Existence of the second
Si IV doublet is rather uncertain. We could not see it in the Keck
data, although it is perhaps present in the MMT spectrum.
The natural interpretation for the origin of the systems with
is that they are intervening, i.e., they are caused by
objects that happen to be placed on the line of sight to the quasar
but are not related to it, although there are cases in the literature
where convincing arguments were presented that systems seemingly far
from the quasar could be associated
(e.g. Richards et al. 1999; Hamann et al. 1997). misawa2005
indicated that Systems E and F could be associated, since their
analysis seemed to show that some of the components in those systems
had partial coverage, although the lines did not show any
variability. In our analysis we obtained satisfactory profile fits
without the assumption of partial coverage. This accounts for the
difference between line parameters derived here and in the Subaru
spectra. However, the total column densities agree well
(Table 5).
![]() |
Figure 9: The C IV (upper panel) and Si IV ( lower panel) regions for System E. Markings as in Fig. 7. |
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In our spectra, we also identify two systems that are not seen in the
Subaru spectra. We label them J (
)
and K
(
); the line properties are listed in
Table 4. We show the two systems in
Fig. 10.
![]() |
Figure 10: The C IV regions for System J ( upper panel) and System K ( lower panel). |
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System J requires a special comment. The Ly
line for this system
would be outside of the wavelength region covered by both MMT and Keck
spectra, and the only identified feature is the C IV doublet. Before
we proceed, we note that it is somewhat surprising that the redder of
the two lines, at
Å, is apparently
not identified in any of the Subaru spectra, since none of the line
lists seem to contain it. This line is unambiguously present in both
of our spectra.
What makes this system somewhat uncertain is the fact that both those
lines coincide very well with the locations of what we expect to be
the strongest O I(1302) and Si II(
1304) lines from
System B. However, there are indications that C IV is in fact present
in this location. First, the spectra contain several other Si II lines, and they constrain the column density of that ion quite well,
suggesting that Si II(
1304) alone cannot account for all of
the absorption in the redder of the two lines. Second, for O I to be
responsible for all of the absorption in the bluer of the two lines,
at
Å, it would require an O I column
density of
1015 cm-2, which we consider implausible.
The above considerations lead us to believe that System J is real, although the fact that both lines are blends makes its properties rather uncertain.
Another of the previously unidentified systems is a system at
,
which we label K. It is clearly seen in both our
spectra; obviously, we could identify it because of the high
signal-to-noide ratio in our data. The system is displaced by
400 kms-1 from System H. It is thus likely that both these
systems originate in objects from the same group of galaxies.
Misawa et al. present convincing arguments that the System A absorber
is variable, but they did not see variability in any of the other
systems. In general, unlike the Subaru observations, our optical data
are not well suited for the analysis of absorber variability. First,
we have data from two epochs only. Second, the data were obtained with
two different telescopes/instruments, at different locations and under
different atmospheric conditions - not to mention that one of the
observations was likely affected by smoke from forest fires. Third,
one of the extracted spectra had issues with residual flux. Fourth, in
some places the continuum fits had to be adjusted manually. Fifth,
the variability range reported in misawa2007 was of the
order of
,
which is only slightly higher than our
typical measurement uncertainties. All these factors make direct
comparison of the derived properties of the absorption lines
questionable, and especially in the regions affected by the continuum
fit uncertainty. Any difference between absorber properties derived
from the two spectra will likely contain an unknown component
attributable to these issues.
Being aware of all these considerations, we examined the column
densities derived from the MMT and Keck data looking for any
systematic differences between the two datasets. In
Fig. 11 we show column densities for the same
components as derived from the MMT and Keck data. Note that the error
bars only show formal uncertainties as derived from the fits and do
not include the unknown uncertainty related to the analysis
issues. Despite this fact, one can clearly see that the properties of
components as derived from our two observations agree very well. Only
very few data points deviate from the
line
by more than 1
,
and the ones that do are practically all in
the high-N region, where issues related to the residual flux in the
MMT spectrum are expected to play a role.
![]() |
Figure 11: Comparison of column densities of all lines for which measurements exist from both MMT (x-axis) and Keck (y-axis) data. See text for discussion. |
Open with DEXTER |
This conclusion applies to both
- including
System A, which Misawa et al. have shown to be variable - as well as
the
systems. For the latter systems this is not
surprising, although, as mentioned earlier, there were claims in the
literature (e.g. Richards et al. 1999; Hamann et al. 1997) indicating that
systems with large redshift difference show variability (see
also Hao et al. 2007).
Acknowledgements
We thank J. Liske for his help with the VPGUESS/VPFIT packages, T. Aldcroft and A. Siemiginowska for helpful comments, and the referee for a very careful review. M.N. would like to thank ESO for hospitality during his stay there. This work was partially supported by the ESO Director General Discretionary Fund, by the National Aeronautics and Space Administration through Chandra Award Number 04700527 issued by the Chandra X-ray Observatory Center, which is operated by the Smithsonian Astrophysical Observatory for and on behalf of the National Aeronautics Space Administration under contract NAS8-03060, and by grant 1P03D00829 of the Polish State Committee for Scientific Research.