A&A 486, 359-373 (2008)
DOI: 10.1051/0004-6361:200809538
A. Leccardi1,2 - S. Molendi2
1 - Università degli Studi di Milano, Dip. di Fisica, via Celoria 16,
20133 Milano, Italy
2 -
INAF-IASF Milano, via Bassini 15, 20133 Milano, Italy
Received 8 February 2008 / Accepted 8 April 2008
Abstract
Aims. We measure radial temperature profiles as far out as possible for a sample of
50 hot, intermediate redshift galaxy clusters, selected from the XMM-Newton archive, keeping systematic errors under control.
Methods. Our work is characterized by two major improvements. First, we used background modeling, rather than background subtraction, and the Cash statistic rather than the
.
This method requires a careful characterization of all background components. Second, we assessed systematic effects in detail. We performed two groups of tests. Prior to the analysis, we made use of extensive simulations to quantify the impact of different spectral components on simulated spectra. After the analysis, we investigated how the measured temperature profile changes, when choosing different key parameters.
Results. The mean temperature profile declines beyond 0.2 R180. For the first time, we provide an assessment of the source and the magnitude of systematic uncertainties. When comparing our profile with those obtained from hydrodynamic simulations, we find the slopes beyond
0.2 R180 to be similar. Our mean profile is similar but somewhat flatter with respect to those obtained by previous observational works, possibly as a consequence of a different level of characterizing systematic effects.
Conclusions. This work allows us to not only constrain cluster temperature profiles in outer regions with confidence, but also, from a more general point of view, to explore the limits of the current X-ray experiments (in particular XMM-Newton) with respect to the analysis of low surface-brightness emission.
Key words: X-rays: galaxies: clusters - galaxies: clusters: general - cosmology: observations
Clusters of galaxies are the most massive gravitationally bound systems in the universe. They are permeated by the hot, X-ray emitting, intra-cluster medium (ICM), which represents the dominant baryonic component. The key ICM observable quantities are its density, temperature, and metallicity. Assuming hydrostatic equilibrium, the gas temperature and density profiles allow us to derive the total cluster mass and thus to use galaxy clusters as cosmological probes (e.g. Voit 2005; Henry & Arnaud 1991; Ettori et al. 2002; Fabian & Allen 2003). Temperature and density profiles can also be combined to determine the ICM entropy distribution, which provides valuable information on the cluster thermodynamic history and has proven to be a powerful tool in investigating non-gravitational processes (e.g. Voit 2005; Ponman et al. 2003; Pratt et al. 2006; McCarthy et al. 2004).
The outer regions of clusters are rich in information and interesting to study, because clusters are still forming there by accretion (e.g. Borgani et al. 2004; Tozzi et al. 2000). Moreover, far from the core it is easier to compare simulations with observations, because feedback effects are less important (e.g. Roncarelli et al. 2006; Borgani et al. 2004; McNamara et al. 2005). Cluster surface brightness rapidly declines with radius, while background (of instrumental, solar, local, and cosmic origin) is roughly constant over the detector. For this reason, spectra accumulated in the outer regions are characterized by poor statistics and high background, especially at high energies, where the instrumental background dominates other components. These conditions make temperature measurement at large distances from the center a technically challenging task, requiring an adequate treatment of both statistical and systematic issues (Leccardi & Molendi 2007).
Given the technical difficulties, early measurements of cluster temperature
profiles have been controversial.
At the end of the ASCA and BeppoSAX era, the shape of the
profiles at large radii was still the subject of debate (De Grandi & Molendi 2002; White 2000; Markevitch et al. 1998; Irwin et al. 1999; Finoguenov et al. 2001; Irwin & Bregman 2000).
Recent observations with current experiments (i.e. XMM-Newton and
Chandra) have clearly shown that cluster temperature profiles decline
beyond the 15-20% of R180 (Pratt et al. 2007; Vikhlinin et al. 2005; Piffaretti et al. 2005; Snowden et al. 2008).
However, most of these measurements might be unreliable at very large radii
(
50% of R180) because they are affected by a number
of systematics related to the analysis technique and to the background
treatment (Leccardi & Molendi 2007).
The aim of this work is to measure the mean temperature profile of galaxy
clusters as far out as possible, while keeping systematic errors under control.
From the XMM-Newton archive, we selected all hot
(kT > 3.5 keV), intermediate redshift (
)
clusters that are not strongly interacting and measured their radial
temperature profiles.
The spectral analysis followed a new approach by using the background
modeling rather than the background subtraction, and the Cash statistic
rather than the
.
This method requires a careful characterization (reported in the Appendices)
of all background components, which unfortunately was not possible for EPIC-pn.
For this reason, we used only EPIC-MOS data in our analysis.
Background parameters are estimated in a peripheral region, where the cluster emission is almost negligible, and rescaled in the regions of interest. The spectral fitting is performed in the 0.7-10.0 keV and in the 2.0-10.0 keV energy bands, which are characterized by different statistics and level of systematics, to check the consistency of our results. A second important point is a particular attention to systematic effects. We performed two groups of test: prior to the analysis, we made use of extensive simulations to quantify the impact of different components (e.g. the cosmic variance or the soft proton contribution) on simulated spectra; after the analysis, we investigated how the measured temperature profile changes, when choosing different key parameters (e.g. the truncation radius or the energy band). At the end of our tests, we provided an assessment of the source and the magnitude of systematic uncertainties associated to the mean profile.
The outline of the paper is the following. In Sect. 2 we describe sample properties and selection criteria and in Sect. 3 we describe our data analysis technique in detail. In Sect. 4 we present the radial temperature profiles for all clusters in our sample and compute the average profile. In Sect. 5 we describe our analysis of systematic effects. In Sect. 6 we characterize the profile decline, investigate its dependency from physical properties (e.g. the redshift), and compare it with hydrodynamic simulations and previous observational works. Our main results are summarized in Sect. 7. In the Appendices we report the analysis of closed and blank field observations, which allows us to characterize most background components.
Quoted confidence intervals are 68% for one interesting parameter
(i.e.
= 1), unless otherwise stated.
All results are given assuming a
CDM cosmology with
,
,
and
H0 = 70 km s-1 Mpc-1.
We selected from the XMM-Newton archive a sample of hot
(kT > 3.3 keV), intermediate redshift (
),
and high galactic latitude (
)
clusters of galaxies.
Upper and lower limits to the redshift range are determined, respectively,
by the cosmological dimming effect and the size of the EPIC field of view
(![]()
radius). Indeed, our data analysis technique requires that the intensity of
background components be estimated in a peripheral region, where the
cluster emission is almost negligible (see Sect. 3.2.1).
We retrieved from the public archive all observations of clusters satisfying
the above selection criteria, performed before March 2005 (when the CCD6
of EPIC-MOS1 was switched off
) and available at the end of May 2007.
Unfortunately, 23 of these 86 observations are highly affected by soft
proton flares (see Table 1).
We excluded them from the sample, because their good (i.e. after flare
cleaning, see Sect. 3.1.1) exposure time is not long enough
(less than 16 ks when summing MOS1 and MOS2) to measure reliable temperature
profiles out to external regions.
Furthermore, we excluded 14 observations of clusters that show evidence
of recent and strong interactions (see Table 2).
For such clusters, a radial analysis is not appropriate, because
the gas distribution is far from being azimuthally symmetric.
Finally, we find that the target of observation 0201901901, which is
classified as a cluster, is probably a point-like source; therefore,
we excluded this observation too from our sample.
| Name | Obs ID |
| RXC J0303.8-7752 | 0042340401 |
| RXC J0516.7-5430 | 0042340701 |
| RXC J0528.9-3927 | 0042340801 |
| RXC J2011.3-5725 | 0042341101 |
| Abell 2537 | 0042341201 |
| RXC J0437.1+0043 | 0042341601 |
| Abell 1302 | 0083150401 |
| Abell 2261 | 0093030301 |
| Abell 2261 | 0093030801 |
| Abell 2261 | 0093030901 |
| Abell 2261 | 0093031001 |
| Abell 2261 | 0093031101 |
| Abell 2261 | 0093031401 |
| Abell 2261 | 0093031501 |
| Abell 2261 | 0093031601 |
| Abell 2261 | 0093031801 |
| Abell 2219 | 0112231801 |
| Abell 2219 | 0112231901 |
| RXC J0006.0-3443 | 0201900201 |
| RXC J0145.0-5300 | 0201900501 |
| RXC J0616.8-4748 | 0201901101 |
| RXC J0437.1+0043 | 0205330201 |
| Abell 2537 | 0205330501 |
| Name | Obs ID |
| Abell 2744 | 0042340101 |
| Abell 665 | 0109890401 |
| Abell 665 | 0109890501 |
| Abell 1914 | 0112230201 |
| Abell 2163 | 0112230601 |
| Abell 2163 | 0112231501 |
| RXC J0658.5-5556 | 0112980201 |
| Abell 1758 | 0142860201 |
| Abell 1882 | 0145480101 |
| Abell 901 | 0148170101 |
| Abell 520 | 0201510101 |
| Abell 2384 | 0201902701 |
| Abell 115 | 0203220101 |
| ZwCl2341.1+0000 | 0211280101 |
| Name | Obs ID | za |
|
R180c | Exp. timed |
|
Filter | |
| RXC J0043.4-2037 | 0042340201 | 0.2924 | 6.8 | 1.78 | 11.9 | 11.3 | 1.25 | THIN1 |
| RXC J0232.2-4420 | 0042340301 | 0.2836 | 7.2 | 1.85 | 12.1 | 11.7 | 1.08 | THIN1 |
| RXC J0307.0-2840 | 0042340501 | 0.2534 | 6.8 | 1.82 | 11.4 | 12.6 | 1.08 | THIN1 |
| RXC J1131.9-1955 | 0042341001 | 0.3072 | 8.1 | 1.93 | 12.4 | 12.3 | 1.08 | THIN1 |
| RXC J2337.6+0016 | 0042341301 | 0.2730 | 7.2 | 1.86 | 13.4 | 13.1 | 1.19 | THIN1 |
| RXC J0532.9-3701 | 0042341801 | 0.2747 | 7.5 | 1.90 | 10.9 | 10.5 | 1.09 | THIN1 |
| Abell 68 | 0084230201 | 0.2550 | 7.2 | 1.88 | 26.3 | 25.9 | 1.37 | MEDIUM |
| Abell 209 | 0084230301 | 0.2060 | 6.6 | 1.85 | 17.9 | 17.8 | 1.19 | MEDIUM |
| Abell 267 | 0084230401* | 0.2310 | 4.5 | 1.49 | 17.0 | 16.5 | 1.79 | MEDIUM |
| Abell 383 | 0084230501 | 0.1871 | 4.4 | 1.52 | 29.3 | 29.8 | 1.33 | MEDIUM |
| Abell 773 | 0084230601 | 0.2170 | 7.5 | 1.96 | 13.6 | 15.5 | 1.16 | MEDIUM |
| Abell 963 | 0084230701 | 0.2060 | 6.5 | 1.83 | 24.4 | 26.0 | 1.19 | MEDIUM |
| Abell 1763 | 0084230901 | 0.2230 | 7.2 | 1.92 | 13.0 | 13.2 | 1.08 | MEDIUM |
| Abell 1689 | 0093030101 | 0.1832 | 9.2 | 2.21 | 36.8 | 36.8 | 1.14 | THIN1 |
| RX J2129.6+0005 | 0093030201 | 0.2350 | 5.5 | 1.66 | 36.0 | 37.5 | 1.21 | MEDIUM |
| ZW 3146 | 0108670101 | 0.2910 | 7.0 | 1.81 | 52.9 | 52.9 | 1.07 | THIN1 |
| E1455+2232 | 0108670201 | 0.2578 | 5.0 | 1.56 | 35.3 | 35.8 | 1.11 | MEDIUM |
| Abell 2390 | 0111270101 | 0.2280 | 11.2 | 2.37 | 9.9 | 10.3 | 1.11 | THIN1 |
| Abell 2204 | 0112230301 | 0.1522 | 8.5 | 2.16 | 18.2 | 19.5 | 1.06 | MEDIUM |
| Abell 1413 | 0112230501 | 0.1427 | 6.7 | 1.92 | 25.4 | 25.4 | 1.10 | THIN1 |
| Abell 2218 | 0112980101 | 0.1756 | 6.5 | 1.86 | 18.2 | 18.2 | 1.17 | THIN1 |
| Abell 2218 | 0112980401 | 0.1756 | 7.0 | 1.93 | 13.7 | 14.0 | 1.42 | THIN1 |
| Abell 2218 | 0112980501 | 0.1756 | 6.1 | 1.80 | 11.3 | 11.0 | 1.07 | THIN1 |
| Abell 1835 | 0147330201 | 0.2532 | 8.6 | 2.05 | 30.1 | 29.2 | 1.16 | THIN1 |
| Abell 1068 | 0147630101 | 0.1375 | 4.5 | 1.58 | 20.5 | 20.8 | 1.09 | MEDIUM |
| Abell 2667 | 0148990101 | 0.2300 | 7.7 | 1.96 | 21.9 | 21.6 | 1.48 | MEDIUM |
| Abell 3827 | 0149670101 | 0.0984 | 7.1 | 2.02 | 22.3 | 22.4 | 1.16 | MEDIUM |
| Abell 3911 | 0149670301 | 0.0965 | 5.4 | 1.77 | 25.8 | 26.1 | 1.43 | THIN1 |
| Abell 2034 | 0149880101 | 0.1130 | 7.0 | 1.99 | 10.2 | 10.5 | 1.16 | THIN1 |
| RXC J0003.8+0203 | 0201900101 | 0.0924 | 3.7 | 1.47 | 26.3 | 26.6 | 1.10 | THIN1 |
| RXC J0020.7-2542 | 0201900301 | 0.1424 | 5.7 | 1.78 | 14.8 | 15.4 | 1.02 | THIN1 |
| RXC J0049.4-2931 | 0201900401 | 0.1080 | 3.3 | 1.37 | 19.2 | 18.8 | 1.28 | THIN1 |
| RXC J0547.6-3152 | 0201900901 | 0.1483 | 6.7 | 1.92 | 23.3 | 24.0 | 1.12 | THIN1 |
| RXC J0605.8-3518 | 0201901001 | 0.1410 | 4.9 | 1.65 | 18.0 | 24.1 | 1.07 | THIN1 |
| RXC J0645.4-5413 | 0201901201 | 0.1670 | 7.1 | 1.95 | 10.9 | 10.9 | 1.11 | THIN1 |
| RXC J1044.5-0704 | 0201901501 | 0.1323 | 3.9 | 1.47 | 25.7 | 25.9 | 1.03 | THIN1 |
| RXC J1141.4-1216 | 0201901601 | 0.1195 | 3.8 | 1.46 | 28.4 | 28.6 | 1.03 | THIN1 |
| RXC J1516.3+0005 | 0201902001 | 0.1183 | 5.3 | 1.73 | 26.7 | 26.6 | 1.13 | THIN1 |
| RXC J1516.5-0056 | 0201902101 | 0.1150 | 3.8 | 1.46 | 30.0 | 30.0 | 1.08 | THIN1 |
| RXC J2014.8-2430 | 0201902201 | 0.1612 | 7.1 | 1.96 | 23.0 | 23.4 | 1.05 | THIN1 |
| RXC J2048.1-1750 | 0201902401 | 0.1470 | 5.6 | 1.75 | 24.6 | 25.3 | 1.07 | THIN1 |
| RXC J2149.1-3041 | 0201902601 | 0.1179 | 3.3 | 1.37 | 25.1 | 25.5 | 1.11 | THIN1 |
| RXC J2218.6-3853 | 0201903001 | 0.1379 | 6.4 | 1.88 | 20.2 | 21.4 | 1.11 | THIN1 |
| RXC J2234.5-3744 | 0201903101 | 0.1529 | 8.6 | 2.17 | 18.9 | 19.3 | 1.31 | THIN1 |
| RXC J0645.4-5413 | 0201903401 | 0.1670 | 8.5 | 2.13 | 11.5 | 12.1 | 1.51 | THIN1 |
| RXC J0958.3-1103 | 0201903501 | 0.1527 | 6.1 | 1.83 | 8.3 | 9.4 | 1.16 | THIN1 |
| RXC J0303.8-7752 | 0205330101 | 0.2742 | 7.5 | 1.89 | 11.7 | 11.5 | 1.18 | THIN1 |
| RXC J0516.7-5430 | 0205330301 | 0.2952 | 7.5 | 1.87 | 11.4 | 11.7 | 1.19 | THIN1 |
| Notes. a Redshift taken from the NASA Extragalactic Database; b mean temperature in keV derived from our analysis; c scale radius in Mpc derived from our analysis; d MOS1 and MOS2 good exposure time in ks; e intensity of residual soft protons (see Eq. (1)); * excluded due to high residual soft proton contamination. |
In Table 3 we list the 48 observations that survived our selection criteria and report cluster physical properties. The redshift value (from optical measurements) is taken from
the NASA Extragalactic Database
;
and R180 are derived from our analysis (see Sect. 4).
In Fig. 1 we report the cluster distribution
in the redshift-temperature space. The only selection effect we detect is the paucity of cool
(
keV) clusters at high (z > 0.2) redshift.
Observations were performed with THIN1 and MEDIUM filters,
as reported in Table 3.
![]() |
Figure 1: Distribution of selected clusters in the redshift-temperature space. We distinguish cool core (blue), non cool core (red) and uncertain (green) clusters, as defined in Sect. 6. There is no evidence of selection effects, except for a weak positive correlation between redshift and temperature. |
The preparation of spectra comprises the following major steps:
In our analysis we used only EPIC-MOS data, because a robust characterization of EPIC-pn background was not possible, mainly due to the small regions outside the field of view and to the non-negligible fraction of out of time events (for further details, see Appendix B). Moreover, the EPIC-pn background is less stable than the EPIC-MOS one, especially below 2 keV.
Observation data files (ODF) were retrieved from the XMM-Newton archive and processed in a standard way with the Science Analysis System (SAS) v6.1.
The soft proton cleaning was performed using a double filtering process.
We extracted a light curve in 100 s bins in the 10-12 keV energy band
by excluding the central CCD, applied a threshold of 0.20 cts s-1,
produced a GTI file and generated the filtered event file accordingly.
This first step allows most flares to be eliminated, however softer flares
may exist such that their contribution above 10 keV is negligible.
We then extracted a light curve in the 2-5 keV band and fit the histogram
obtained from this curve with a Gaussian distribution.
Since most flares had been rejected in the previous step, the fit was
usually very good. We calculated the mean count rate,
,
and the standard deviation,
,
applied a threshold of
to the distribution, and
generated the filtered event file.
After soft proton cleaning, we filtered the event file according to
PATTERN and FLAG criteria (namely PATTERN
12 and
FLAG == 0).
In Table 3 we report the good exposure time after the soft
proton cleaning; as mentioned in Sect. 2, we excluded
observations for which the total (MOS1+MOS2) good exposure time is less
than 16 ks. In the left panel of Fig. 2 we report the histogram of the
frequency distribution for observation exposure times.
| |
Figure 2:
Histograms of the frequency distribution for averaged
MOS exposure time ( left panel) and
|
When fitting spectra in the 0.7-10.0 keV band (see Sect. 3.2), we also excluded the ``bright'' CCDs, i.e. CCD-4 and CCD-5 for MOS1 and CCD-2 and CCD-5 for MOS2 (see Appendix A for the discussion).
Brightest point-like sources were detected, using a procedure based on the
SAS task edetect_chain and excluded from the event file.
We estimated a flux limit for excluded sources on the order of
10-13 erg cm-2 s-1; after the source excision, the cosmic
variance of the X-ray background on the entire field of view is
20%.
A quiescent soft proton (QSP) component can survive the double filtering
process (see Sect. 3.1.1). To quantify the amount of this component, we made use of the ``IN over OUT'' diagnostic
(De Luca & Molendi 2004).
We measured the surface brightness, SB
,
in an outer region of
the field of view, where the cluster emission is negligible, and compared it
to the surface brightness, SB
,
calculated outside the field
of view in the same energy range (i.e. 6-12 keV).
Since soft protons are channeled by the telescope mirrors inside the field
of view and the cosmic ray induced background covers the whole detector,
the ratio
The cluster emission was divided in 10 concentric rings (namely
0
-0.5
,
0.5
-1
,
1
-1.5
,
1.5
-2
,
2
-2.75
,
2.75
-3.5
,
3.5
-4.5
,
4.5
-6
,
6
-8
,
and
10
-12
). The center of the rings was determined by surface brightness isocontours at large radii and is not necessarily coincident with the X-ray emission peak.
We prefer that azimuthal symmetry be preserved at large radii, where we are
interested in characterizing profiles, at the expense of central regions.
For each instrument (i.e. MOS1 and MOS2) and each ring, we accumulated a spectrum and generated an effective area (ARF). For each observation we generated one redistribution function (RMF) for MOS1 and one for MOS2. We perform a minimal grouping to avoid channels with no counts, as required by the Cash statistic.
Spectral fitting was performed within the XSPEC v11.3
package
.
The choice of the energy band for the spectral fitting was not trivial.
We fit spectra in the 0.7-10.0 keV and in the 2.0-10.0 keV energy bands, by
using the Cash statistic, with an absorbed thermal plus background model.
The high-energy band has the advantage of requiring a simplified background
model (see Appendices A and B); however,
the bulk of source counts was excluded and the statistical quality of the
measurement was substantially reduced.
Due to the paucity of source counts, there is a strong degeneracy between
source temperature and normalization, and the temperature is systematically
underestimated; therefore, when using the 2.0-10.0 keV band, an ``a posteriori'' correction was required (Leccardi & Molendi 2007).
In contrast, in the 0.7-10.0 keV band, the statistical quality of the data is
good, but the background model is more complicated and background components
are less stable and affected by strong degeneracy (see
Appendices A and B).
We excluded the band below 0.7 keV because the shape of the internal
background is very complicated and variable with time and because the source
counts reach their maximum at
1 keV.
Hereafter, all considerations are valid for both energy bands, unless
otherwise stated.
In conditions of poor statistics (i.e. few counts/bin) and high background,
the Cash statistic (Cash 1979) is more suitable than the
with
reasonable channel grouping (Leccardi & Molendi 2007).
The Cash statistic requires the number of counts in each channel to be
greater than zero (Cash 1979); thus, the background cannot be subtracted.
In our case the total background model is the sum of many components,
each one characterized by peculiar temporal, spectral, and spatial
variations (see Appendix B).
When subtracting the background, the information on single components was lost.
Conversely, background modeling allows one to preserve the information and
to manage all components appropriately.
Moreover, we recall that the background modeling does not require strong
channel grouping, error propagation, or renormalization factors.
To model the background, a careful characterization of all its components is
mandatory. Ideally, one would like to estimate background parameters in the same region
and at the same time as the source.
Since this was not possible, we estimated background parameters in the external
10
-12
ring and rescaled them in the inner rings, by making
reasonable assumptions on their spatial distribution tested by analyzing
blank-field observations (see Appendix B).
The 10
-12
ring often contains a weak cluster emission
that, if neglected, may cause a systematic underestimate of temperature
and normalization in the inner rings (see Sect. 5.1.2).
In this ring the spectral components in the 0.7-10.0 keV band are:
We fixed most parameters (namely all except for the normalization of
HALO, CXB, NXB, and fluorescence lines) to reduce the degeneracy due to the
presence of different components with similar spectral shapes.
All cluster parameters were fixed: the temperature, kT, and the
normalization,
,
were extrapolated from the final profiles
through an iterative procedure.
The metallicity, Z, was fixed to 0.2 solar (the solar abundances were
taken from Anders & Grevesse 1989) and the redshift, z, was fixed to the optical
value. The QSP normalization,
,
was calculated from
(see Appendix B) and fixed.
Minor discrepancies in shape or normalization with respect to the real QSP spectrum are possible, the model accounts for them by slightly changing the
normalization of other components, i.e.
,
,
and
(for the discussion of the systematic effects related
to QSP see Sects. 5.1.3 and 5.2.3).
Summarizing, in the 10
-12
ring, we have determined the
range of variability, [
,
], (i.e. the best fit value
1
uncertainty) for the normalization of the main background
components, i.e.
,
,
and
.
Once properly rescaled, this information allowed us to constrain background
parameters in the inner rings.
We fit spectra in internal rings with the same model as adopted in the
10
-12
ring case (see Sect. 3.2.1).
In Fig. 3 we compare spectra and best fit models for two
different regions of the same cluster.
In the inner ring (1
-1.5
)
source counts dominate, while
in the outer ring (4.5
-6
)
background counts dominate.
The equivalent hydrogen column density along the line of sight,
,
was fixed to the 21 cm measurement (Dickey & Lockman 1990).
Since clusters in our sample are at high galactic latitude
(
), the
is <1021 cm-2and the absorption effect is negligible above 1 keV.
We have always left the temperature, kT, and the
normalization,
,
free to vary.
The metallicity was free below
0.4 R180 and fixed to
0.2 solar beyond. The redshift was allowed to vary between
7% of the optical measurement
in the two innermost rings and, in the other rings, was fixed to the average
value of the first two rings.
The normalization of HALO, CXB, and NXB for the inner rings were obtained
by rescaling the best-fit values in the 10
-12
ring (see
Sect. 3.2.1) by the area ratio and the correction factor, K(r),
obtained from blank field observations (see Table B.2 in
Appendix B):
For each ring, when using the 0.7-10.0 keV energy band, we determined
kT, Z, and
best fit values and one-sigma
uncertainties for each MOS and calculated the weighted average.
Conversely, when using the 2.0-10.0 keV band, we combined temperature
measurements from different instruments as described in our previous
paper (Leccardi & Molendi 2007), to correct for the bias that affects the
temperature estimator.
In the 0.7-10.0 keV band, there are many more source counts, the
temperature estimator is much less biased, and the weighted average
returns a slightly (
3% in an outer ring) biased value (see
the F=1.0 case in Sect. 5.1.1).
Finally, we produced surface brightness (i.e. normalization over area), temperature, and metallicity profiles for each cluster.
Clusters in our sample have different temperatures and redshifts, therefore it is not trivial to identify one (or more) parameters that indicate the last ring where our temperature measurement is reliable. We define an indicator, I, as the source-to-background count rate ratio calculated in the energy band used for the spectral fitting. For each observation we calculated I for each ring: the higher I, the more the source contribution, and the more reliable our measurement in this particular ring. The indicator I is affected by an intrinsic bias; i.e., upward statistical fluctuations of the temperature are associated to higher I (because of the difference in spectral shape between source and background models); therefore, near a threshold, the mean temperature is slightly overestimated. This systematic is almost negligible when considering the whole sample, but it may appear when analyzing a small number of objects. We note that, although present, this effect does not affect results obtained when dividing the whole sample into subsamples (e.g. Sects. 5.2.3 and 6.2).
In Fig. 4 we show the radial temperature profiles for all
clusters of our sample by setting a lower limit I0=0.6, and spectra are
fitted in the 0.7-10.0 keV band. Each profile is rescaled by the cluster mean temperature,
,
computed by fitting the profile with a constant
after the exclusion of the core region (i.e. for
R > 0.1 R180).
The radius is rescaled by R180, i.e. the radius encompassing a
spherical density contrast of 180 with respect to the critical density.
We compute R180 from the mean temperature and the redshift
(Arnaud et al. 2005):
The profiles show a clear decline beyond
0.2 R180, and our
measurements extend out to
0.6 R180.
The large scatter of values is mostly of statistical origin; however,
a maximum likelihood test shows that, when excluding the region below
0.2 R180, our profiles are characterized by a 6% intrinsic
dispersion, which is comparable to our systematics
(see Sect. 5.3), so that the existence of a universal
cluster temperature profile is still an open issue.
The scatter in the inner region is mostly due to the presence of
both cool core and non cool core clusters, but also to our
choice of preserving the azimuthal symmetry at large radii
(see Sect. 3.1.3). In Fig. 5 we report temperature and radius of the
innermost ring scaled by
and R180for all clusters. We define (i) cool core (hereafter CC) clusters as those for which
the temperature is significantly (at least
)
lower than
;
(ii) non cool core (hereafter NCC) clusters
as those for which the temperature profile does not significantly (at
least
)
decrease; and (iii) uncertain (hereafter UNC) clusters
as those for which the membership is not clearly determined.
It is worth noting that the error bars are usually strongly asymmetric; i.e., the upper bar is larger than the lower. Moreover, the higher the temperature, the larger the error bars. The reason is that most of the information on the temperature is located around the energy of the exponential cut-off. Due to the spectral shapes of source and background components and to the sharp decrease of the effective areas at high energies, the source-to-background count rate ratio strongly depends on the energy band (see for example Fig. 3); i.e., the higher the cut-off energy, the lower the source-to-background ratio and the larger the uncertainties.
In Fig. 6 we report the weighted average and the scatter of all profiles shown in Fig. 4. The mean profile shows the decline beyond 0.2 R180 more clearly. The temperature also decreases toward the center because of the presence of cool core clusters.
We carefully checked our results, searching for possible systematic effects. Prior to the analysis, we made use of extensive simulations to quantify the impact of different spectral components on a simulated temperature profile (``a priori'' tests). After the analysis, we investigated how the measured temperature profile changed, when choosing different key parameters (``a posteriori'' tests).
![]() |
Figure 6:
Mean radial temperature profile rescaled by R180 and
|
We performed simulations that reproduced our analysis procedure as closely
as possible. We considered two rings: the external 10
-12
,
,
where we estimated background parameters, and the
4.5
-6
,
,
where we measured the
temperature. The exposure time for each spectrum is always 20 ks, i.e. a representative
value for our sample (see Fig. 2).
We used the Abell 1689 EPIC-MOS1 observation as a guideline, for producing
RMF and ARF, and for choosing typical input parameters.
The simulation procedure is structured as follows:
We employed a simulation to quantify the effect of the cosmic variance
on temperature and normalization measurements.
In this simulation we neglected the soft proton contribution; the
background components are the HALO, the CXB, and the NXB, and they are
modeled as for MOS1 in Appendix B.
In
there are only background components, while in
there is also the thermal source.
Normalization
input values in
are:
10-4,
10-2, and
10-2; input values in
are obtained by rescaling the values in
by the area ratio (i.e. as in Eq. (2) with K(r)=1.0).
Then,
is also multiplied by a factor, F, which
simulates the fluctuation due to the cosmic variance between
and
.
After the excision of brightest point-like sources (see Sect. 3.1.1), one-sigma fluctuations are expected to be
30%.
We then considered 3 cases: a null (F=1.0), a positive (F=1.3), and
a negative (F=0.7) fluctuation. Thus, in the first case the input value for CXB in
is equal to that rescaled by the area ratio, in the second it is 30% higher,
and in the third 30% lower. Input parameters for the thermal model in
are
kT=6 keV,
,
z=0.2, and
10-4.
In
,
Z and z are fixed to the input values, while
kT and
are free. For this particular choice of the parameters, the source-to-background count rate ratio, I, is 1.13 (see Sect. 4).
As explained in Sects. 3.2.1 and 3.2.2, we
determined the ranges of variability for
,
,
and
and rescaled them in
.
Then we fit spectra in the 0.7-10.0 keV band and calculated the weighted
averages of kT and
over the 500 simulations.
In Fig. 7 we show the relative differences between
measured and input values for the temperature, kT (filled
circles), and the normalization,
(empty circles).
A positive fluctuation of CXB normalization (i.e. F=1.3) returns
higher temperature and normalization, because the excess of counts due
to the CXB is modeled by the thermal component, which is steeper than
the CXB power law. For the F=1.0 case, while
returns exactly the input
value, kT returns a slightly (
3%) underestimated
value, probably due to the bias on the temperature estimator
(Leccardi & Molendi 2007). The effect of the cosmic variance is roughly symmetric on both kTand
,
making it almost negligible when averaging over
a large sample. We also performed simulations for our worst case, i.e. I=0.6 (see
Sect. 4), and find qualitatively the same results.
For the F=1.0 case, the bias on the temperature is
8% rather
than
3% and the bias on the normalization is negligible.
The source contribution in the 10
-12
ring, which
mainly depends on cluster redshift and emission measure, is difficult
to estimate with accuracy.
We employed a simulation to determine how an inaccurate estimate
could affect our measurement of cluster temperature, kT, and
normalization,
.
Soft protons are neglected in this case, too; background components
and their input values are the same as for the F=1.0 case of the
cosmic variance tests (see Sect. 5.1.1).
Input parameters for the thermal model in
are the same as
in that case, instead in
are
keV,
,
,
and
10-4.
For this particular choice of the parameters, the source-to-background
count rate ratio, I, is 1.13 (see Sect. 4).
When fitting spectra in
,
all thermal parameters
are fixed: namely, the temperature, the metallicity, and the redshift
are fixed to the input values, while for
we consider 4 cases. In the first case, we neglect the source contribution
(
); in the other cases, the normalization
is fixed to a value lower (
10-4),
equal (
10-4), and higher
(
10-4) than the input value.
Normalizations of all background components (namely
,
,
and
)
are free parameters.
For each case, we computed the weighted average of
,
,
and
over the 300 spectra in
and compared them to the input values
(see Fig. 8).
Both
and
are weakly correlated;
instead,
and, in particular,
show
a strong negative correlation with the input value for
,
which depends on their spectral shapes.
Note that, if we correctly estimate
,
then
,
,
and
converge
to their input values.
For each input value of
in
,
we fit spectra in
in the 0.7-10.0 keV band after
the usual rescaling of background parameters (see Sect. 3.2.2),
calculated the weighted averages of the source temperature, kT,
and normalization,
,
over the 500 simulations, and compared
them to the input values (see Fig. 9).
Values of kT and
measured in
show
a positive correlation with the value of
fixed in
.
This is indeed expected because of the broad similarity in the spectral shapes
of thermal and CXB models. In
an overestimate of
implies an
underestimate of
(see Fig. 8);
is then rescaled by the area ratio, hence underestimated in
too.
This results in an overestimate of kT and
in
,
as for the F=1.3 case of the cosmic variance simulations
(see Sect. 5.1.1). Typical uncertainties (![]()
)
on
cause systematic 5% and 7% errors on kT and
(see
Fig. 9). Note that, after the correction for the
3% bias mentioned in
Sect. 5.1.1, the effect on
and kT is
symmetric; thus, when averaging on a large sample, the effect on the mean
profile should be almost negligible.
Note also that if we were to neglect the cluster emission in the
10
-12
ring (
), we would cause
a systematic underestimate of kT and
on the order
of 7-10% (see Fig. 9).
In a real case we deal with a combination of fluctuations and cannot treat each
one separately, so we employed a simulation to investigate how fluctuations with
different origins combine with each other.
We combined effects due to the cosmic variance and to an inaccurate estimate of
the cluster emission in the 10
-12
ring, by considering the
F=0.7, F=1.0, and F=1.3 cases mentioned in Sect. 5.1.1 and
10-4,
10-4, and
10-4 mentioned in this section.
The simulation procedure is the same as described before.
For the cluster normalization, we find that fluctuations combine in a linear way
and that effects are highly symmetric with respect to the zero case (F=1.0 for
the cosmic variance and
10-4 for the
cluster emission in the 10
-12
ring).
For the cluster temperature, we find again the
3% bias related to the
estimator; once accounted for this 3% offset, results are roughly similar to those
found for the normalization case.
To be more quantitative, when averaging on a large sample, the expected systematic
on the temperature measurement is
3% due to the biased estimator and
2% due to deviations from the linear regime.
A careful characterization of the QSP component is crucial for our data analysis
procedure. We employed a simulation to quantify how an incorrect estimate of the QSP contribution from the ``IN over OUT'' diagnostic; i.e., the
(see Sect. 3.1.2) could affect our measurements.
The spectral components and their input values are the same as for the F=1.0 case of the cosmic variance simulations (see Sect. 5.1.1), plus the
QSP component in both rings. The model for QSP is the same as described in Appendix B. We chose two input values for
corresponding to a standard
(
)
and a high (
)
level of QSP contamination.
For these particular choices of the parameters, the source-to-background count
rate ratio, I, is 1.06 for
and 0.77 for
(see Sect. 4). For each input value we considered 2 cases: an underestimate
(
)
and an overestimate (
)
of the
correct value. By fitting spectra in
in the 0.7-10.0 keV band, we determined the
range of variability of
,
,
and
,
and rescaled it in
(see Sect. 3.2.2).
We then fit spectra in
and compared the weighted averages of cluster
temperature, kT, and normalization,
,
to their input values
(see Fig. 10).
When considering
,
the relative difference between measured and input
values is <
for all cases and the effect is symmetric, so the impact on the
mean profile obtained from a large sample should be very weak.
Instead, kT strongly depends on our estimate of the QSP component: the
relative difference is
5% for
and
20%
for
.
When overestimating
,
kT is underestimated, because of the
broad similarity in the spectral shapes of the two components.
In the
case, the values corresponding to an overestimate and an
underestimate, although symmetric with respect to zero, are characterized by different
uncertainties (errors in the first case are twice those in the second); thus, a
weighted average returns a 10% underestimated value.
In this subsection we investigate how the mean profile is affected by a particular choice of key parameters: the last ring for which we measure a temperature (see Sect. 5.2.1), the energy band used for the spectral fitting (see Sect. 5.2.2), and the QSP contamination (see Sect. 5.2.3).
In Sect. 4 we introduced the indicator I to choose the last
ring where our temperature measurement is reliable.
Here we produce mean temperature profiles by averaging over all measurements for
which I > I0, for different values of the threshold I0.
In Fig. 11 we report the profiles obtained in the 0.7-10.0 keV
band for different choices of I0 (namely 0.0, 0.2, 0.4, 0.6, 0.8, and 1.0).
As expected, the smaller the threshold, the farther the mean profile extends.
If we focus on the points between 0.3 and 0.6 of R180, we notice a clear
systematic effect: the smaller the threshold, the lower the temperature.
This means that, on average, the temperature is lower in those rings where the
background is more important.
This systematic effect becomes evident where cluster emission and background
fluctuations are comparable and is probably related to small imperfections in our
background modeling and to the bias on the temperature estimator
(see Sect. 5.1.1).
The imperfections of our background model becomes the dominant effect for low values
of I (namely
).
Thus, under a certain threshold, I0, our measurements are no longer reliable.
In Fig. 11 we show that I0=0.6 represents a good compromise.
Indeed, when considering the region between 0.4 and 0.5 of R180 and comparing
the average value for kT obtained for a threshold I0=0.6 and for
I0=1.0, we find a small (
)
relative difference.
![]() |
Figure 11: Mean temperature profiles computed by choosing different values for the threshold I0 (defined in Sect. 4) plotted with different colors. There is a clear systematic effect: the smaller the threshold, the steeper the profile. The radii have been slightly offset in the plot for clarity. |
We have fitted spectra in two different energy bands (i.e. 0.7-10.0 keV and
2.0-10.0 keV), each one characterized by different advantages and drawbacks
(see Sect. 3.2).
The indicator, I, defined in Sect. 4 depends on the band in which
the count rate is calculated: more precisely, I(0.7-10.0) is roughly 1.5 times
greater than I(2.0-10.0) for low values (i.e.
).
The threshold I0=0.6 in the 0.7-10.0 keV band corresponds to I0=0.4 in the
2.0-10.0 keV band (see Sect. 5.2.1).
In Fig. 12 we compare the mean temperature profile obtained in the
0.7-10.0 keV band (I0=0.6) with the one obtained in the 2.0-10.0 keV band (I0=0.4).
The profiles are very similar, except for the innermost point.
The uncertainties in the 0.7-10.0 case are much smaller at all radii, even if the total
number of points (i.e. the number of rings for all cluster) is the same, because the
higher statistics at low energies allows a substantial reduction of the errors on single
measurements.
In the most internal point, a high discrepancy between the two measurements is present, although in that region the background is negligible. This is due to the superposition, along the line of sight, of photons emitted by optically thin ICM with different densities and temperatures. When looking at the center of cool core clusters, the line of sight intercepts regions characterized by strong temperature gradients, so the accumulated spectrum is the sum of many components at different temperatures. In this case, the best fit value for the temperature strongly depends on the energy band (i.e. the harder the band, the higher the temperature), because the exclusion of the soft band implies the exclusion of most of the emission from cooler components (Mazzotta et al. 2004).
We divided clusters in our sample into four groups, according to the QSP contamination
that we estimate from
(see Sect. 3.1.2).
In Fig. 13 we report the mean temperature profiles for the
four groups, by fitting spectra in the 0.7-10.0 keV band and fixing I0=0.6.
When dividing clusters into subsamples, we chose larger bin sizes to reduce
the error bars. When
was high, our selection criterion based on the
source-to-background count rate ratio (see Sects. 4 and 5.2.1) excluded the outer rings, indeed the red profile only extends out to 0.5 R180.
No correlation is found between the shape of the profiles and
;
i.e., the four profiles are fully consistent.
The discrepancy in the innermost ring is due to the presence of a different
number of cool core clusters in each group.
We therefore conclude that the systematic error associated to the QSP contamination is smaller than statistical errors (
7% beyond 0.4 R180).
In this subsection we summarize the main results for what concern systematic errors associated to our mean profile. We compare expected systematics computed from ``a priori'' tests with measured systematics from ``a posteriori'' tests.
The F=1.0 case in Sect. 5.1.1 and the
10-4 case in Sect. 5.1.2
show that our analysis procedure is affected by a 3% to 8% systematic
underestimate of the temperature when analyzing the outermost rings.
The bias is probably related to the temperature estimator as described in
Leccardi & Molendi (2007). In contrast, the normalization estimator is unbiased.
In Sects. 5.1.1 and 5.1.2, we also found that the
effects of the cosmic variance and of an inaccurate estimate of the cluster emission
in the external ring are symmetric for both the temperature, kT, and the
normalization,
.
In Sect. 5.1.2 we found that the effects due to fluctuations with
different origins combine in a linear way and, when averaging over a large sample,
the systematic associated to the mean profile is almost negligible for
and
2% for kT. Thus, the expected systematic for kT is
5%.
In Sect. 5.1.3 we found that, for a standard level of contamination
(
), a typical 5% error in the estimate of
causes
negligible effects on both measurements of cluster temperature and normalization.
The same error causes negligible effects on
measurements for a high
level of contamination (
).
In contrast, effects on kT for
are important: the same
5% error causes a 10% underestimate of kT, also when averaging over a large
sample. However, at the end of Sect. 5.2.3, in particular from
Fig. 13, we have concluded that, when considering the whole sample,
the systematic error associated to the QSP contamination is smaller than statistical
errors (
7% beyond 0.4 R180).
The difference between expected and measured systematic errors is only apparent.
Indeed, when analyzing our sample, we averaged measurements that span a wide range of
values for
and I; conversely, the 10% systematic error is expected for
an unfavorable case, i.e.
and I=0.77 (see Sect. 5.1.3).
In Sect. 5.2.1 we compared the mean temperature value obtained for a
threshold I0=0.6 and for I0=1.0 in an outer region (i.e. between 0.4 and 0.5 of
R180). In this ring the mean value for the indicator I is 1.14, thus the expected bias related to the temperature estimator is
3% (see Sect. 5.1.1).
We measured a
temperature discrepancy, which is consistent with the expected
bias. As pointed out in Sect. 5.2.1, the discrepancy could also be due to small
imperfections in our background model. We are not able to quantify the amount of this contribution, but we expect it to be small when considering I > 0.6.
To summarize, in external regions our measurements of the cluster temperature are affected
by systematic effects, which depend on the radius through the factor I, i.e. the
source-to-background count rate ratio.
For each ring, we calculated the mean value for I, estimated the expected bias from
simulations, and applied a correction to our mean profile.
The expected bias is negligible for internal rings out to 0.30 R180 (for which
), is 2-3% for 0.30-0.36 and 0.36-0.45 bins, and is ![]()
for the
last two bins (i.e. 0.45-0.54 and 0.54-0.70).
We associate to our correction an uncertainty close to the correction itself, accounting
for our limited knowledge from our ``a posteriori'' tests of the precise value of the bias.
In Fig. 14 we show the mean temperature profile before and after the
correction for the bias. In Table 4 we report the corrected values for each bin.
The uncertainty is the quadrature sum of the statistical error and of the error associated
to our correction. Hereafter, we will consider the mean profile corrected for the bias, unless otherwise stated. Note that the bias is always comparable to the statistical uncertainties.
For this reason, ours can be considered as a definitive work, for what concerns the
measurement of radial temperature profiles of galaxy clusters with XMM-Newton.
We have reached the limits imposed by the instrument and by the analysis technique, so that
increasing of the number of objects will not improve the quality of the measurement.
![]() |
Figure 14:
Mean temperature profile rescaled by R180 and
|
| Ringa | Temperatureb |
| 0.00-0.04 | 0.762 |
| 0.04-0.08 | 0.921 |
| 0.08-0.12 | 1.028 |
| 0.12-0.18 | 1.030 |
| 0.18-0.24 | 0.993 |
| 0.24-0.30 | 0.985 |
| 0.30-0.36 | 0.938 |
| 0.36-0.45 | 0.878 |
| 0.45-0.54 | 0.810 |
| 0.54-0.70 | 0.694 |
Notes. a In units of R180; b in units of
.
We fit profiles (see Fig. 4) beyond 0.2 R180 with a linear model and
a power law to characterize the profile decline. By using a linear model
![]() |
(4) |
![]() |
(5) |
| (6) |
![]() |
Figure 16: Mean temperature profiles for the four z-binned groups of clusters. There is no indication of profile evolution. The radii have been slightly offset in the plot for clarity. |
We divide our clusters into four groups according to the redshift, to investigate a possible evolution of temperature profiles with cosmic time. In Fig. 16 we report the mean temperature profiles for the four groups. Spectra are fitted in the 0.7-10.0 keV band and I0=0.6 (see Sect. 4). As in the following Sects. 6.3 and 6.4, when dividing clusters into subsamples, the profiles are not corrected for biases (see Sect. 5.3), because when comparing subsamples we are not interested in determining the absolute value of the temperature, but in searching for relative differences. Moreover, in Figs. 16 and 18 we choose larger bin sizes to reduce the error bars (as in Fig. 10). The four profiles are very similar: the discrepancy in the outer regions is comparable to statistical and systematic errors, and the difference in the central region is due to a different fraction of cool core clusters. We fit each group of profiles with a power law beyond 0.2 R180 and report results in Fig. 17. Since there is no clear correlation between the two parameters and the redshift, we conclude from the analysis of our sample that there is no indication of profile evolution up to z=0.3.
In Sect. 4 we defined three groups: clusters that clearly host a cool core,
clusters with no evidence of a cool core, and uncertain clusters.
In Fig. 18 we show mean temperature profiles for the three groups.
Spectra are fitted in the 0.7-10.0 keV band and I0=0.6.
Profiles differ by definition in the core region and are consistent beyond
0.1 R180.
Our sample is not complete with respect to any property.
However, most of our clusters (
2/3) belong to the REFLEX Cluster Survey catalog
(Böhringer et al. 2004), a statistically complete X-ray flux-limited sample of 447 galaxy clusters, and
a dozen objects belong to the XMM-Newton Legacy Project sample (Pratt et al. 2007), which is
representative of an X-ray flux-limited sample with z<0.2 and kT>2 keV.
We then selected two subsamples from our sample: clusters that belong to the REFLEX catalog
(REFL04 subsample) and to the Legacy Project sample (LP07 subsample).
The smaller (i.e. the LP07) is derived from Pratt's parent sample, by applying our selection
criteria based on cluster temperature and redshift.
We also excluded cluster observations that are heavily affected by soft proton contamination;
however, the latter selection should be equivalent to a random choice and introduce no bias.
Thus, we expect the LP07 subsample to be representative of an X-ray flux-limited sample of
galaxy clusters with 0.1<z<0.2 and kT>3.3 keV.
The larger (i.e. the REFL04) subsample includes the LP07 one.
Clusters that belong to the REFL04, but not to the LP07, were observed with XMM-Newton
for different reasons. They are not part of a large program and almost all observations have different PIs. Thus, there are no obvious reasons to believe that the sample is significantly biased with respect to any fundamental cluster property.
A similar reasoning leads to the same conclusion for our whole sample.
In Fig. 19 we compare mean temperature profiles obtained from the two
subsamples and the whole sample.
The three profiles are fully consistent beyond
0.1 R180, the difference in
the central region is due to a different fraction of CC clusters.
These results allow us to conclude that our whole sample is representative of hot, intermediate
redshift clusters with respect to temperature profiles, i.e. the quantity we are interested in.
In this subsection we compare our mean temperature profile with the one derived from cluster
hydrodynamic simulations by Borgani et al. (2004, hereafter B04).
The authors used the TREE+SPH code GADGET (Springel et al. 2001) to simulate a concordance cold
dark-matter cosmological model (
,
,
,
and h = 0.7) within a box of 192 h-1 Mpc on a side, 4803 dark-matter
particles, and as many gas particles.
The simulation includes radiative cooling, star formation, and supernova feedback.
Simulated cluster profiles are scaled by the emission-weighted global temperature and R180calculated from its definition (i.e. the radius encompassing a spherical density contrast of
180 with respect to the critical density).
In Fig. 20 we compare our observed profile to the projected mean profile
obtained by averaging over simulated clusters with kT > 3 keV.
The evident mismatch between the two profiles is most likely due to a different definition for
the scaling temperature: actually, it is known that the emission weighted temperature is higher
than the mean temperature obtained from observational data (Mazzotta et al. 2004).
By rescaling the B04 profile by 10%, we find good agreement between simulation and our data
beyond
0.25 R180. Conversely in the core region, simulations are not able to reproduce the observed profile shape.
![]() |
Figure 20: Comparison between our observed mean profile (circles) and the one derived from hydrodynamic simulations (Borgani et al. 2004) by averaging over clusters with kT > 3 keV (solid line). The dashed line is obtained by rescaling the solid one by 10%. |
In this section we compare our mean temperature profile (LM08) with those obtained by other
authors, namely De Grandi & Molendi (2002), Vikhlinin et al. (2005), and Pratt et al. (2007).
De Grandi & Molendi (DM02) have analyzed a sample of 21 hot (
kT > 3.3 keV),
nearby (
)
galaxy clusters observed with BeppoSAX.
Their sample includes both CC and NCC clusters.
Vikhlinin et al. (V05) analyzed a sample of 13 nearby (
), relaxed
galaxy clusters and groups observed with Chandra.
We selected from their sample only the hottest (
kT > 3.3 keV) 8 clusters, for a
more appropriate comparison with our sample.
Pratt et al. (P07) analyzed a sample of 15 hot (
kT > 2.8 keV), nearby
(
)
clusters observed with XMM-Newton.
Clusters of their sample present a variety of X-ray morphology.
Comparing different works is not trivial.
Cluster physical properties, instrumental characteristics, and data analysis procedures may differ.
Moreover, each author uses his own recipe to calculate a mean temperature and to derive a scale
radius. We rescaled temperature profiles obtained by other authors by using the standard cosmology
(see Sect. 1) and calculating the mean temperature,
,
and the scale radius, R180, as explained in Sect. 4; the aim is to reduce
all inhomogeneities as much as possible.
![]() |
Figure 21:
Upper panel: mean temperature profiles obtained from
this work (black circles, LM08), by De Grandi & Molendi
(blue squares, DM02), by Vikhlinin et al. (red upward
triangles, V05), and by Pratt et al. (green
diamonds, P07). All profiles are rescaled by
|
In Fig. 21 we compare the four mean temperature profiles, rescaled by
and R180.
Due to the correction for the biases described in Sect. 5.3, our mean
profile is somewhat flatter than others beyond
0.2 R180.
Discrepancies in the core region are due to a different fraction of CC clusters.
The outermost point of the P07 profile is
25% lower; however, it is only
constrained by two measurements beyond
0.6 R180.
Our indicator, I, (see Sect. 4) warns about the reliability of these two
measurements, for which
0.3, i.e. a half of our threshold, I0 = 0.6.
In Fig. 11 we show that, when using our analysis technique, lower values
of I are associated to a bias on the temperature measurement.
We assume that a somewhat similar systematic may affect the P07 analysis technique, too.
When excluding these two measurements, the P07 mean profile only extends out to
0.6 R180 and is consistent with ours (see also Fig. 22).
It is possible that measurements obtained with other experiments be also affected by a similar
kind of systematics, which make the profiles steeper.
![]() |
Figure 22: Best fit parameters, obtained by fitting observed and simulated cluster profiles with a power law, beyond 0.2 R180. In the upper panel we report the normalization, in the lower the index. We use the same symbols as in Fig. 21 for observed clusters and a violet downward triangle for Borgani's work (B04). The normalization is calculated at 0.2 R180. For P07 we report two values, empty diamonds indicate index and normalization obtained when excluding the two outermost measurements (see text for details). The empty downward triangle indicates the normalization of the B04 rescaled profile (see Sect. 6.5). In the lower panel, the dashed line and the shaded region represent the weighted average and its one sigma confidence interval derived from the observed profiles only (for P07 we use the lower value, i.e. the empty diamond). As previously noted from Fig. 21, the LM08 profile is the flattest one, but all indices of observed profiles are consistent within two sigma. Conversely, the B04 profile seems to be significantly steeper, but in this case we are not able to provide an estimate of parameter uncertainty. |
We fit observed and simulated cluster profiles with a power law beyond 0.2 R180 and
in Fig. 22 report best fit parameters.
The LM08 profile is the flattest one; however, all observed profile indices are consistent
within 2-3 sigma. In Sect. 5.3 we have quantified the systematic underestimate on the temperature measurement associated to our procedure.
Since it depends on the indicator I, which itself depends on the radius, we also expect a
net effect on the profile index,
;
namely, we expect
to be overestimated.
For this reason, it is possible that the discrepancy between indices obtained from different
works (reported in Fig. 22) may not have a purely statistical origin.
We calculate an average profile index,
0.02, which is significantly lower
than obtained from the B04 profile,
;
however, for the simulation we are not
able to provide an estimate of parameter uncertainty.
We have analyzed a sample of
50 hot, intermediate redshift galaxy clusters (see
Sect. 2) to measure their radial properties.
In this paper we focused on the temperature profiles and postponed the analysis of the
metallicity to a forthcoming paper (Leccardi & Molendi 2008, submitted).
In Sect. 6.4 we showed that our sample should be representative of hot,
intermediate redshift clusters, at least with respect to the temperature profile.
Our main results are summarized as follows.
Our work not only provides a confirmation of previous results.
For the first time, we believe we know where the systematics come from and how large they are.
Indeed, this work allows us to not only constrain cluster temperature profiles with confidence
in the outer regions, but also, from a more general point of view, to explore the limits of
the current X-ray experiments (in particular XMM-Newton).
It is crucial that we learn how best to exploit XMM-Newton data, because for the next
5-10 years there will be no experiments with comparable or improved capabilities, as far as
low surface-brightness emission is concerned.
Our work will also allow us to look forward to ambitious new measurements: an example is the
attempt to measure the putative shock in Abell 754, for which we have obtained a
200 ks observation with XMM-Newton in AO7.
Acknowledgements
We acknowledge the financial contribution from contracts ASI-INAF I/023/05/0 and I/088/06/0. We thank S. Ghizzardi, M. Rossetti, and S. De Grandi for a careful reading of the manuscript. We thank S. Borgani, G. W. Pratt, and A. Vikhlinin for kindly providing their temperature profiles.
We analyzed a large number (
50) of observations with the filter wheel in the
``closed'' position to characterize the EPIC-MOS internal background in detail and to provide
constraints to the background model, which we use for analyzing our data.
Exposure times of individual observations cover between 5 and 100 ks for a total exposure time
of
650 ks.
For each observation, we selected 6 concentric rings (0
-2.75
,
2.75
-4.5
,
4.5
-6
,
6
-8
,
8
-10
,
and 10
-12
)
centered on the detector center.
For each instrument (i.e. MOS1 and MOS2) and each ring, we produced the total spectrum by
summing, channel by channel, spectral counts accumulated during all observations.
We associated the appropriate RMF to each total spectrum and performed a minimal grouping to
avoid channels with no counts. In Fig. A.1 we report the total spectra accumulated in the 10
-12
ring, for MOS1 and MOS2, in the 0.2-11.3 keV band.
Closed observation events are solely due to the internal background, which is characterized by
a cosmic-ray induced continuum (NXB) plus several fluorescence emission lines.
The most intense lines are due to Al (
1.5 keV) and Si (
1.8 keV).
Beyond 2 keV we fit the NXB with a single power law (index 0.24 and 0.23 for MOS1 and MOS2
respectively); instead, for the 0.7-10.0 keV range, a broken power-law (see Table A.1)
was more appropriate. Emission lines were modeled by Gaussians.
Note that particle background components were not multiplied by the effective area.
| MOS1 | 0.22 | 7.0 | 0.05 |
| MOS2 | 0.32 | 3.0 | 0.22 |
| Line | E [keV] | Line | E [keV] |
| Al K |
1.487 | Mn K |
6.490 |
| Al K |
1.557 | Fe K |
7.058 |
| Si K |
1.740 | Ni K |
7.472 |
| Si K |
1.836 | Cu K |
8.041 |
| Au M |
2.110 | Ni K |
8.265 |
| Au M |
2.200 | Zn K |
8.631 |
| Cr K |
5.412 | Cu K |
8.905 |
| Mn K |
5.895 | Zn K |
9.572 |
| Cr K |
5.947 | Au L |
9.685 |
| Fe K |
6.400 |
In Table A.2 we list the emission lines of our model with their rest frame energies.
Normalization values are always reported in XSPEC units.
Lines are determined by 3 parameters: peak energy, intrinsic width and normalization.
The energy of Al K
,
,
was free to allow for a small shift in the energy
scale; the energies of Al, Si, and Au-M lines were linked to
in such a way that
a common shift,
,
was applied to all lines.
Similarly, the energy of Cr K
,
,
was free and the energies of all other
lines were linked to
.
The intrinsic width was always fixed to zero, except for Al and Si lines for which it was fixed
to 0.0022 keV to allow for minor mismatches in energy calibrations for different observations.
Normalizations of K
,
Al, and Si lines were free, while normalizations of K
lines
were forced to be one seventh of the correspondent K
line (Keith & Loomis 1978).
The correlation between broken power-law and Gaussian parameters is very weak.
As noticed by Kuntz (2006), there are observations in which the count rate of some CCDs is very different, especially at low energies, indicating that the NXB spectral shape is not constant over the detector. In particular, this problem affects MOS1 CCD-4 and CCD-5 and MOS2 CCD-2 and CCD-5. Since our procedure requires background parameters to be rescaled from the outer to the inner rings, we always excluded the above mentioned ``bright'' CCDs from data analysis when using the 0.7-10.0 keV band (see Sect. 3.1.1). This was not necessary when using the band above 2 keV, because the effect is negligible for almost all observations.
![]() |
Figure A.2:
|
After the exclusion of the bright CCDs, we fit spectra accumulated in the 10
-12
ring for different closed observations, to check for temporal variations of the NXB.
In Fig. A.2 we report the values of broken power-law free parameters (namely the
slopes,
and
,
and the normalization, N) for both MOS in the 0.7-10.0 keV
band. The scatter of
and
values is the same order of magnitude as the
statistical uncertainties, while the scatter of the N values (
20%) is not purely
statistic; i.e., NXB normalization varies for different observations.
We also checked for spatial variations of the internal background.
As explained at the beginning of this section, we accumulated the total spectrum for each of
the 6 rings and for each instrument.
We defined the surface brightness, SB, as the ratio between N and the area of the ring.
In Fig. A.3 we report MOS1 and MOS2 best fit values of SB as a function of
the distance from the center, by fixing
and
.
The spatial variations are greater than statistical errors but less than 5%.
To a first approximation, the NXB is flat over the detector.
We find similar results, both in terms of temporal and spatial variations, when fitting spectra
above 2 keV.
Emission lines showed rather weak temporal variations and most of them (namely, all except for
Al, Si, and Au) have a uniform distribution over the detector.
Al lines are more intense in the external CCDs, while Si lines are more intense in the central CCD.
Conversely, Au lines are very localized in the outer regions of the field of view, thus we
model them only when analyzing rings beyond 3.5
.
| |
Figure A.3: Surface brightness best fit values for MOS1 ( left) and MOS2 ( right) as a function of the distance from the detector center. |
A large number (
30) of ``blank field'' observations were analyzed to characterize the
spectrum of other background components.
Exposure times of individual observations cover between 30 and 90 ks for a total exposure time
of
600 ks. Almost all observations have different pointing in order to maximize the observed sky region and minimize the cosmic variance of the X-ray background.
Data were prepared and cleaned as described in Sects. 3.1.1 and 3.1.2.
For each instrument (i.e. MOS1 and MOS2) and each filter (i.e. THIN1 and MEDIUM), we produced
total spectra by summing, channel by channel, spectral counts accumulated during all
observations after the selection of the same rings used for closed observations (see
Appendix A). We associated the appropriate RMF and ARF to each spectrum and performed a minimal grouping to avoid channels with no counts.
We also calculated the average
(see Sect. 3.1.2), obtaining
1.09
0.01 for both filters and both detectors.
Inside the field of view, the spectral components are the following (see Fig. B.1):
![]() |
Figure B.1:
MOS1 spectrum from blank field observations in the
10 |
The photon components only (i.e., HALO and CXB) were multiplied by the effective area and
absorbed by our Galaxy. The equivalent hydrogen column density along the line of sight,
,
was fixed to the 21 cm measurement (Dickey & Lockman 1990), averaged over all fields.
We selected blank field observations pointed at high galactic latitude, therefore
is <1021 cm-2 and the absorption effect is negligible above 1 keV.
In the 0.7-10.0 keV band, the total model is composed of a thermal component (HALO), a power law (CXB), two broken power laws (QSP and NXB), and several Gaussians (fluorescence emission
lines). The thermal model (APEC in XSPEC) parameters are:
kT=0.197 keV,
,
and z=0.0 (Kuntz & Snowden 2000).
The slope of the CXB power law was fixed to 1.4 (De Luca & Molendi 2004), and the normalization was
calculated at 3 keV to minimize the correlation with the slope.
The QSP broken power law has a break energy at 5.0 keV, and the slopes were fixed
to 0.4 (below 5 keV) and 0.8 (above 5 keV).
The model parameters for the internal background are the same as reported in
Appendix A. In the 2.0-10.0 keV band the model is simpler (namely, three power laws and several Gaussians) and more stable.
The HALO component is negligible above 2 keV, the CXB model is the same as in the 0.7-10.0 keV
band, the slope of the QSP power law was fixed to 1.0, and the model parameters for the internal
background are those reported in Appendix A.
Most components have rather similar spectral shapes (see Fig. B.1),
therefore a high degree of parameter degeneracy is present.
In such cases, it is useful to constrain as many parameters as possible.
Events outside the field of view are exclusively due to the internal background, therefore the
spectrum accumulated in this region provides a good estimate of the NXB normalization,
.
By analyzing closed (CL) observations we find that the ratio between
calculated in two regions of the detector is independent of the particular observation:
| Instr. | Filter |
|
|
|
| [10-4] | [10-3] | [10-2] | ||
| MOS1 | THIN1 | 1.7 |
2.4 |
5.1 |
| MOS2 | THIN1 | 1.6 |
2.5 |
5.0 |
| MOS1 | MEDIUM | 1.4 |
2.6 |
6.0 |
| MOS2 | MEDIUM | 1.6 |
2.4 |
5.8 |
Notes. a calculated at 3 keV.
In Table B.1 we report the best fit values for the normalization of the HALO,
,
of the QSP,
,
and of the CXB,
,
in the
10
-12
ring, for MOS1 and MOS2 instruments and for THIN1 and MEDIUM filters.
We fit spectra in the 0.7-10.0 keV energy band.
We stress the remarkably good agreement between MOS1 and MOS2 for all parameters.
Moreover, we point out that, when comparing observations with different filters, values for
and
agree, while values for
are significantly
different (
20%) because of the cosmic variance (
15% expected for the
considered solid angles).
By construction (see Eq. (1)) there is a relation between
and
,
so that the higher
,
the higher
.
For observations that are not contaminated by QSP,
and
are expected. Since
values span a relatively narrow range (roughly between 1.0 and 1.5), we approximated the relation between
and
with a linear function:
.
The scaling factor,
,
was determined from the analysis of blank fields
observations, for which we measured
0.01 and
10-3. Thus, for each observation we model the bulk of the QSP component by deriving
from
(see Sects. 3.2.1 and 3.2.2). In Sects. 5.1.3 and 5.2.3 we discuss possible systematics related to QSP, and show that the linear approximation used above is satisfactory.
As mentioned in Sect. 3.2.1, we estimated the normalizations of the background
components in the 10
-12
ring, and rescaled them in the inner rings.
When considering the 0.7-10.0 keV energy band, a simple rescaling by the area ratio was too
rough and caused systematic errors, especially in the outer regions where cluster emission
and background fluctuations are comparable.
To overcome this problem, we have proceeded in the following manner.
We fit blank field spectra, by fixing
and
,
and determined
and
best fit values.
For each ring and instrument, we defined a correction factor, K(r):
![]() |
(B.3) |
| Ring | HALO | CXB | ||
| MOS1 | MOS2 | MOS1 | MOS2 | |
| 0 |
0.62 | 0.68 | 0.80 | 0.91 |
| 2.75 |
0.74 | 0.70 | 0.70 | 0.78 |
| 4.5 |
0.63 | 0.65 | 0.89 | 0.95 |
| 6 |
0.74 | 0.71 | 0.89 | 0.92 |
Unfortunately, a precise characterization of the QSP component for EPIC-pn was not possible.
Uncertainties on
were very large, because the region outside the EPIC-pn
field of view is much smaller than the MOS one, and the presence of a non negligible
fraction of out-of-time events introduced a further complication.
Moreover, the EPIC-pn background is much less stable than the EPIC-MOS one, especially below
2 keV. The EPIC-pn instrument has further drawbacks due to the electronic board near the detector:
the NXB spatial distribution is not flat and the emission due to Ni-Cu-Zn lines (between
7.5 keV and
9.5 keV) is more intense in the outer rings.
For these reasons, as mentioned in Sect. 3, we considered only EPIC-MOS
data in our analysis.