A&A 441, 893-903 (2005)
DOI: 10.1051/0004-6361:20052856
M. Arnaud1 - E. Pointecouteau1 - G. W. Pratt2
1 - CEA/DSM/DAPNIA Service d'Astrophysique, CE
Saclay, L'Orme des Merisiers,
Bât. 709, 91191 Gif-sur-Yvette, France
2 -
MPE, Giessenbachstraße, 85748 Garching, Germany
Received 10 February 2005 / Accepted 19 June 2005
Abstract
Using a sample of ten nearby (
), relaxed
galaxy clusters in the temperature range [2-9]
,
we have
investigated the scaling relation between the mass at various density
contrasts (
)
and the cluster
temperature.
The masses are derived from NFW-type model fits to
mass profiles, obtained under the hydrostatic assumption
using precise measurements, with XMM-Newton, at least down to
.
The logarithmic slope of the M-T relation is well
constrained and is the same at all
,
reflecting the
self-similarity of the mass profiles. At
,
the slope of
the relation for the sub-sample of hot clusters (
)
is
consistent with the standard self-similar expectation:
.
The relation steepens when the whole sample is
considered:
.
The normalisation of the relation
is discrepant (by
30 per cent), at all density contrasts, with the
prediction from purely gravitation based models. Models that take
into account radiative cooling and galaxy feedback are generally in
better agreement with our data. We argue that remaining
discrepancies, in particular at low
,
are more likely due to
problems with models of the ICM thermal structure rather than to
an incorrect estimate of the mass from X-ray data.
Key words: cosmology: observations - cosmology: dark matter - galaxies: clusters: general - galaxies: intergalactic medium - X-rays: galaxies: clusters
From a theoretical
point of view, galaxy clusters are characterised by their mass. Models
of
structure formation predict the space density, spatial distribution
and physical properties of clusters (internal structure, radius,
temperature, luminosity, etc) as a function of mass and redshift
(see Bertschinger 1998, for a review). However, observationally,
the mass is not easily measured, and the observed scaling relations
are in fact expressed in terms of the temperature T, rather than the
mass M. These scaling relations are important sources of
information on the physics of cluster formation
(e.g. Voit & Ponman 2003). For the information to be complete, we must
determine the
M-T relation itself, which provides the missing link between the gas
properties and the mass. Furthermore, measures of the cosmological
parameters, such as
,
and w, from cluster
abundance or spatial distribution, rely heavily on this relation to
link the mass to the X-ray observables available from X-ray cluster
surveys. The present error on the value of
,
as determined
from X-ray observations, is dominated by uncertainty on the M-T relation
(Henry 2004; Viana et al. 2003; Pierpaoli et al. 2003), and a precise calibration of this
relation is mandatory if we want to do "precision'' cosmology with clusters
(Borgani 2003).
The average temperature is expected to be closely related to the mass,
via the virial theorem. We can first define
as the mass
within the radius
,
inside which the mean mass density is
times the critical density,
,
at the cluster redshift. We then expect
,
if clusters are in hydrostatic
equilibrium and they obey self-similarity. Here h(z) is the
Hubble
constant normalised to its local value and
depends on the
internal structure. The above relation is remarkably well verified by
adiabatic numerical simulations, down to
,
which
roughly corresponds to the virialised part of clusters
(e.g. Evrard & Gioia 2002).
For relaxed clusters, the mass can be derived from X-ray observations
of the gas density and temperature profile and the hydrostatic
equilibrium equation. In recent years, a sustained observational
effort to measure the local M-T relation has been undertaken using
ROSAT, ASCA and BeppoSAX, but no definitive picture has yet emerged. It
is unclear whether the mass scales as T3/2 as expected
(Castillo-Morales & Schindler 2003; Horner et al. 1999; Ettori et al. 2002); or if this is true only in the
high mass
regime (
), with a steepening at lower mass
(Nevalainen et al. 2000; Xu et al. 2001; Finoguenov et al. 2001); or even if the slope is higher
over the entire mass range (Sanderson et al. 2003). The derived
normalisations of the M-T relation derived from ASCA data are
generally lower than predicted by adiabatic numerical simulations
(e.g. Nevalainen et al. 2000; Finoguenov et al. 2001), typically 40 per cent
below the
prediction of Evrard et al. (1996). On the other hand, using BeppoSAX data,
Ettori et al. (2002) found a normalisation consistent with the predictions
(although the errors were large).
These studies had to rely largely on extrapolation to derive the
virial mass, and were limited by the low resolution and statistical
quality of the temperature profiles. With XMM-Newton and Chandra we can
now measure the mass profile of clusters with unprecedented accuracy.
Using Chandra observations, Allen et al. (2001) derived an M-T relation
slope of
,
consistent with the self-similar model, and
confirmed the offset in normalisation. However, their sample comprised
only 5 hot (i.e massive) clusters (kT>5.5 keV), and, due to the
relatively small Chandra field of view, their M-T relation was
established at R2500 (i.e. about
0.3R200).
In a recent paper (Pointecouteau et al. 2005, hereafter, Paper I), we measured the integrated mass profiles of ten relaxed, nearby clusters observed with XMM-Newton. The sample has an excellent temperature coverage, from 2 to 9 keV. The mass profiles cover a wide range of radii (from 0.01R200 to 0.7R200), and are particularly well constrained between 0.1R200 and 0.5R200. In Paper I, we studied the structural properties of the mass profiles, in order to test current scenarios for the Dark Matter clustering. In this paper, these data are used to establish a precise M-T relation up to the virial radius. In Sect. 2, we describe how we derive the temperature and mass data. In Sect. 3 we present and compare the M-T relations at various density contrasts. We discuss the reliability of the X-ray mass estimates in Sect. 4. The derived M-T relations are discussed with respect to pre-Chandra/XMM-Newton results in Sect. 5, and with expectations from models in Sect. 6. Our conclusions are presented in Sect. 7.
Throughout the paper, results are given for the currently-favoured
CDM cosmology, with H0=70 km s-1 Mpc-1,
and
.
We used the mass profiles determined in Paper I to estimate the mass
at four density contrasts:
and
200
. We recall that
the mass profiles were derived from the observed density and
temperature profiles (corrected for PSF and projection effects) using
the hydrostatic equilibrium equation. The mass and errors at each
radius of the temperature profile were calculated using a Monte Carlo
method.
In Paper I, we found that the mass profiles are well described by an
NFW-type model (Navarro et al. 1997):
We will use these mass estimates to study the
-T relation at
various density contrasts. Our study is thus based on a parametric
model of the observed mass profiles, rather than directly on the
measured mass data. Let us discuss this point in more detail. All of
the clusters are observed down to at least
(
,
averaged over the whole sample), the only
exceptions being A1983 and MKW9 (
). At
and
,
using the best fitting model rather
than the data is simply equivalent to 'smoothing' the data (without
data extrapolation).
We checked that this does not introduce a bias in the following way:
for each cluster, we estimated the mass at
by
interpolating the observed profile expressed as a function of density
contrast
in the log-log plane. We then compared the
interpolated value to that derived from the NFW fit to the mass
profile. In all cases the values are consistent within their
errors. The ratio of the two values has a median value of 0.99across the sample, and there is no significant correlation with mass.
This reflects the fact that the NFW model is a good fit to these data,
particularly in the
0.1R200-
0.5R200 range (see Paper I).
As explained above, the estimates of M2500 and M1000 are
made (almost) without data extrapolation. However, the mass estimates at
and
do involve extrapolation of the data.
The M500 and M200 estimates rely on the assumption that
the
best fitting NFW model remains a good representation of the cluster mass
profile beyond
.
We further discuss the reliability
of this assumption in Sect. 4.
Table 1:
Physical cluster parameters. Masses are in units of
,
and are given for a
CDM cosmology with
,
,
H0=70 km s-1 Mpc-1. Errors
are
errors.
![]() |
Figure 1: Temperature profiles. The temperatures have been normalised to the spectroscopic temperature measured in 0.1<r<0.5 R200region; the radius has been scaled to R200. The profiles have been corrected for PSF and projection effects (see Paper I for details). |
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To investigate the M-T relation, we need to define a global
temperature. For this quantity, we used the overall spectroscopic
temperature of the
region. The lower
boundary of
0.1 R200 was chosen so as to avoid most of the cooling
core, where a large dispersion is observed in the temperature profiles
(Fig. 1). The upper boundary is limited by the quality
of the spectroscopic data. An upper boundary of
0.5 R200 appeared a
good compromise. Only the data from A1983 and MKW9 do not quite reach
this radius; they are however detected up to
0.4 R200 (see
Table 1). Note that
0.5 R200 corresponds roughly to
.
For each cluster, we performed an isothermal fit of the spectrum
extracted within the [0.1-0.5]R200 range, R200 being derived from
the best fitting NFW model (see above). In the fit, the abundance was
let free and the
was fixed to the 21 cm value (except for A478,
see Pointecouteau et al. 2004). We corrected the derived value for PSF
blurring and
projection effects using the ratio of the mean emission-measure
weighted value of the temperature profile in the [0.1-0.5] R200region after PSF/projection correction to the mean value before
correction (see Paper I for details on the correction procedure). The
correction factor is generally negligible and is always less than
5 per cent. The resulting temperature values are given in
Table 1.
We could have estimated a "mass-weighted'' temperature in the 0.1R200< r < 0.5R200 region from the temperature profile. However, this temperature would still be a "spectroscopic'' temperature since it would be derived from averaging over measured X-ray temperatures. It would not, strictly speaking, be equivalent to the "mass-weighted'' temperature derived from numerical simulations. We thus preferred to use the overall spectroscopic temperature, which is a directly measured quantity and can also easily be estimated in numerical simulations. Since the region is defined in scaled radius, it can be derived from the simulated temperature profiles, using for instance the approach proposed recently by Mazzotta et al. (2004). In addition, we note that only a global spectroscopic temperature can be usually estimated for high z clusters. In our approach, the extraction region can be similarly defined and our definition thus allows a consistent study of the evolution of the M-T relation.
We note that Allen et al. (2001) use a mass-weighted temperature,
T2500, estimated from the temperature profile in the
region. In practice, their definition is equivalent to
ours because i) the temperature profiles are fairly flat beyond the
cooling core region (
r> 0.1R200) in both studies, and ii) the cooling
core does not contribute much in mass to the average. This can be
checked from Fig. 1 of Allen et al. (2001), where T2500 cannot be
distinguished from the spectroscopic temperature of the region beyond
the cooling core.
In order to check the consistency of our XMM-Newton results with the
Chandra study of Allen et al. (2001), we first investigated the
M2500-T relation. For our sample,
corresponds to an
average radius of
,
where the mass is particularly
well constrained for all clusters.
The sample studied by Allen et al. (2001) comprises hot lensing clusters
(5.5 to
). We thus considered only the sub-sample of
clusters with moderate to high temperatures (i.e.
), and
fitted the M2500-T relation using a power law model of the
form:
![]() |
Figure 2:
The M-T relation at
|
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![]() |
Figure 3:
The M-T relation as seen by XMM-Newton from a sample of 10
clusters covering a temperature range from 2 to 9 keV. From top to
bottom and left to right, the M-T relation is given at the density
contrasts |
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The data are well fitted by a power law (
).
The slope,
,
is perfectly consistent with the
expectation from the standard self-similar model, and with the results
from Chandra observations (
). The derived
normalisation,
,
is also
consistent with the Chandra normalisation (see
Table 3). As noted by Allen et al. (2001), such a
normalisation is discrepant with the value derived from numerical
simulations including gravitational heating only: our measured value
is about
30 per cent below the prediction of
Evrard et al. (1996). When the Chandra data for 4 of the 5 clusters
studied by Allen et al. (2001) are added to the present data
set
, the
best fitting values are almost unchanged (
with the
same intercept). This is due to the larger uncertainties in the
Chandra temperature and mass determinations compared to those measured
here (see Fig. 2). Figure 2 shows the
best fit for the combined XMM-Newton and Chandra data compared to the
expectations from the adiabatic numerical simulations of
Evrard et al. (1996).
Still working at
,
we performed a fit over the whole
XMM-Newton sample, i.e. now including the four low mass systems. We obtain
,
and a normalisation
.
The fit is acceptable, although formally less good
(
). The slope now differs significantly
from the expected value of
,
and is just barely consistent
with it at a
level. This is further discussed in
Sect. 6.2.
Table 2:
Results of power law fits to the
-T and
-T relation at various density contrasts
.
The data are fitted with a power law of the form
and
,
where kT is
the overall spectroscopic temperature of the
[0.1R200-
0.5R200] region. A
CDM cosmology is assumed:
,
,
and H0=70 km s-1 Mpc-1.
Figure 3 shows the
-T relations at various
,
together with the best fitting power law (Eq. (2)) in each
case, and the prediction from the numerical simulations of Evrard et al. (1996). The best fitting slopes and normalisations are listed
in Table 2, together with the standard errors. The
best fits are listed and plotted both for
the whole sample, and for the sub-sample of hot clusters. The
corresponding
-T relations are also given in the Table.
The normalisation and slope are nearly independent parameters for
the whole sample. The covariance in
and
,
normalised to the product of their standard errors, is small:
0.045, 0.071, 0.092 and 0.11 for
and 200,
respectively. This is due to our choice of the pivot of the
-T
relation,
(Eq. (2)), close to the mean
temperature of the whole sample (
)
or the median value of its
temperature range (
). The normalisation for other
pivots can be derived using our best fitting values from Eq. (2).
For instance, for a pivot at
,
used in several works on
cluster scaling relations, the normalisation
is
36 per cent higher. The relative error,
,
is
increased by
10 per cent.
We have also computed the raw and intrinsic scatter about the best fitting
relations in the log-log plane. They are given in Table 2.
To estimate the raw scatter, we used the orthogonal distances to the
regression line, weighted by the error
. The
intrinsic scatter is computed from the quadratic difference between the
raw scatter and the scatter expected from the statistical errors.
The behaviour of the M2500-T relation is reproduced at all
other density contrasts. The slope is stable on all spatial scales:
the variation is at most 10 per cent of the statistical error. It is
always
consistent with the expected
value for the sub-sample of
clusters, whereas it steepens to
when the
cool clusters are included. Similarly, the normalisation remains
per cent below the value from adiabatic numerical simulations of
Evrard et al. (1996) at all
.
This stable behaviour is a direct consequence of the self-similarity of
the mass profiles (Paper I). For an NFW type profile, the ratio of the
masses at different density contrasts only depends on the
concentration parameter, and
.
If
all clusters had exactly the same concentration parameter (i.e.,
perfect self-similarity) the
-T relations at various
should differ only in their normalisation:
,
for
.
The
clusters in our sample are not perfectly self-similar but there is no
significant variation of c with mass, and thus temperature (see
Fig. 3 of Paper I). This explains the observed invariance of the
slope. Furthermore, the observed concentration parameter is
consistent with theoretical expectations (Paper I). As a consequence,
the variation with
of the normalisation,
,
follows expectations, and the offset with respect to
simulations observed at
remains the same at all
(see also
Fig. 4, and Fig. 13 of Pratt & Arnaud 2002).
However, the quality of the power law fit decreases with decreasing
(see Table 2 and also Fig. 3). The
reduced
increases and the corresponding null hypothesis
probability for the whole sample varies from 0.32 at
to 0.07 at
.
This behaviour corresponds to an increase
of the intrinsic scatter in the observed
-T relation (see
Table 2). For the whole sample, the worst fit and largest
intrinsic scatter is observed at
.
The regression method
we used (Sect. 2.1) is strictly valid only if the intrinsic
scatter is negligible as compared to the statistical scatter. This is
not always the case (see Table 2), and we first checked if
our results could be affected, using the M200-T relation for
the whole sample (i.e., the worst case). We refitted the data using
the orthogonal BCES method (Akritas & Bershady 1996). While this is the
least-biased regression method when both measurement errors and
intrinsic scatter are present, it is less accurate that the
method when the intrinsic scatter is negligible. The best fitting values remain unchanged (within 0.5 per cent) and the standard error
estimates are only slightly larger (by
15 per cent).
The regression method we used is thus justified. Nevertheless, the
derived intrinsic scatter should not be over-interpreted. The cluster
sample is small and is certainly not representative of the entire
cluster population. In particular, it is heavily biased towards the
more relaxed clusters. Moreover, the increased intrinsic scatter at
low
may be an artifact of the method we used to derive the
various
.
These were derived from an NFW fit to the observed
mass profile, using
as a free parameter (see
Sect. 2.1). In the NFW fit, M2500 is extremely
well constrained by the data around
,
quasi-independently
of the shape of the observed mass profile. On the other hand,
at low
,
beyond the maximum radius of
observation, can be viewed as an "extrapolation'' of the NFW model best
fitting the observed mass profile. It thus depends both on the
normalisation of the observed profile (basically M2500) and on
its shape. The shape parameter (the concentration c) is very
sensitive to the data at small radii, in particular in the cooling core
region, where the mass profile is least well constrained, and where
there could be systematic errors due to the PSF/projection correction.
As a result we expect, as observed, increasing statistical errors on
as
decreases, and a corresponding increase of
the raw scatter in the
-T relation (reflecting the scatter in c,
see Fig. 3 of Paper I). The increase might be larger than that
expected purely from the increase of statistical errors due to
intrinsic scatter in c and/or systematic errors on c.
As discussed in Paper I, there is an excellent quantitative
agreement in shape between the X-ray mass profiles used in this
work and the profile predicted by numerical simulations. The observed
scaled profiles are well-described by the quasi-universal cusped
profile (NFW-type) now found in all CDM simulations, and have
concentration parameters as expected for their mass. As concluded in
Paper I, this suggests that the Dark Matter collapse is well
understood, at least down to the cluster scale. In turn, this gives us
confidence in the XMM-Newton mass estimates, not only in the observed
radial range, but also where we have extrapolated beyond it (i.e. at
). By using the best fitting NFW
model to estimate M500 and M200, we have implicitly assumed
that this model remains valid beyond
(Sect. 2.1). It would be surprising if this were not the case
since i) it is consistent with the theoretical predictions above
,
and ii) in one case (A1413), we were even able to
check the validity of the NFW profile down to
.
Strictly speaking, the good agreement between the observed and
predicted shape of the mass profiles does not mean that the absolute value of the X-ray mass is correct. It could be subject to
systematic errors. However, for the correct universal shape of the mass
profile to be recovered, this systematic error would have to be the same,
within the statistical errors at all observed
,
whatever the
cluster temperature.
One possible source of such systematic error is a departure from
hydrostatic equilibrium (HE). The recent simulations of Kay et al. (2004a)
suggest that the mass determined from the HE equation underestimates
the true mass, due to residual gas motion. The effect is about the
same at all radii up to
.
It is of the order of 15 per
cent for adiabatic models and of 10 per cent for models including cooling and
feedback, with typical variations of
per cent. Such variations would
not significantly change the shape of the X-ray mass profiles, taking
into acccount our statistical errors. Thus the measured M2500 and
M1000 values, and thus the corresponding normalisation of
theM2500-T and M1000-T relations, could well be
10-15 per cent too low. The offset would be the same for the
M500-T and M200-T relations, since they are derived
from "extrapolation'' of the NFW model. Note that this is probably an
upper limit, since we focus on particularly relaxed clusters.
Another possible source of systematic error is that associated with
errors in estimated temperatures from uncertainties in the
instrument calibration. Possible errors are of the order of
10 per cent. This value is consistent with the systematic difference
observed between temperature derived with XMM-Newton and Chandra with the
former being on average
times the latter
(Kotov & Vikhlinin 2005). Since the mass derived from the HE equation scales
as
,
error in Twould translate into a systematic error on the estimate of the
`real' mass of clusters. However that would not change the
normalisation of the "observed'' M-T relation, since that depends only
on the shape of the temperature profile.
In the present study, as discussed above, an NFW profile has been used
to describe the integrated mass profile, derived, assuming HE, from the
observed density and temperature profiles. A similar approach
was used
in the Chandra study of Allen et al. (2001).
Previous ROSAT/ASCA studies also estimated the mass from the HE
equation, but assumed a
-model for the gas density profile and a
polytropic (or even isothermal) temperature profile (Castillo-Morales & Schindler 2003; Horner et al. 1999; Sanderson et al. 2003; Nevalainen et al. 2000; Xu et al. 2001; Finoguenov et al. 2001). Data were
of poorer spatial resolution and statistical quality, and had less radial
extent, thus requiring more extrapolation, particularly for low
mass clusters. This could introduce systematic errors and biases,
particularly at low
,
since a mass profile derived from an
isothermal or polytropic
-model is not consistent with an NFW
profile at large radii (see Fig. 11 of Neumann & Arnaud 1999). On the
other hand, the latest ROSAT/ASCA studies of the M-T relation
(Sanderson et al. 2003; Finoguenov et al. 2001) are superior in terms of the size of
the
cluster samples, and their wide and homogeneous coverage in
temperature. Their results are compared to ours in
Table 3.
Finoguenov et al. (2001) established the M500-T relation for 39
clusters with ASCA temperature profiles. Interestingly, their
results are consistent with ours within the uncertainties
(Table 3). This suggests that systematic errors are not
dominant over statistical errors at
in this ROSAT/ASCA study. However, our normalisation is on the upper side of their
allowed values.
The slope they find for their hot cluster subsample (
)
is,
as we have found, consistent with the expected
value. When
Finoguenov et al. (2001) included all clusters (down to
),
they found a steepening of the M500-T relation:
.
The effect is larger than in our case: we find
(although the difference is not significant).
However, our sample does not reach quite such low temperatures
and the
difference could also reflect a progressive steepening of the M-T relation toward low masses.
Table 3:
Comparison of the present results with M-T relations
from the literature.
is the logarithmic slope of the
relation and A is the normalisation at
,
in units of
for H0=70 km s-1 Mpc-1.
The same remark holds for the results of Sanderson et al. (2003), who
derived a slope of
for the M200-T
relation, which is barely consistent with our value. Their large
sample includes 66 clusters in the [0.5-15]
temperature range.
Furthermore, their normalisation at
is significantly
lower than ours (by 15 per cent, Table 3). This may
reflect the introduction of systematic errors when extrapolating
polytropic models down to
as low as 200. However, such
systematic errors could not explain the discrepancy between our
results and theirs at
.
At that density contrast, their
slope for a hot cluster (
)
sub-sample is
,
a result which is inconsistent with ours at the
95 per cent confidence level. Their normalisation at
,
,
is lower than our
value of
and is only barely
consistent with the Chandra results.
Sanderson et al. (2003) have suggested that the discrepancy (with respect to the Chandra results) might be related to the dynamical state of the clusters in the different samples. Both the Chandra study and the present XMM-Newton study focus on particularly relaxed clusters, which is not the case in Sanderson et al.'s study. However, we note that Finoguenov et al.'s sample does not discriminate in terms of dynamical state, and their results are in good agreement with ours. That said, the M-T relation could well depend on the exact dynamical states of the clusters in the sample in question, an effect which is not trivial to predict. The numerical simulations of Rowley et al. (2004) show that clusters with substructure tend to lie below the mean T-M relation, probably due to incomplete thermalisation (their Fig. 15). However, for the same reason, we would expect the X-ray mass to underestimate the true mass (Kay et al. 2004a), moving unrelaxed clusters back closer to the mean relation. A XMM-Newton study of the M-T relation for an unbiased sample of clusters is needed to assess the effect of cluster dynamical state on the measured M-T relation. The relation should ideally be compared to numerical simulations and lensing mass data. In any case, we do not confirm Sanderson et al.'s results, at least for the relaxed clusters considered here.
Finally, it is of interest to compare the present results with those
of Ettori et al. (2002), who also use an NFW model to estimate
masses
. Their M-T relation for a
relaxed sub-sample of 12 clusters with
can be directly
compared with our relation for hot clusters. At
,
they
found
,
which is marginally consistent with our
value, and
at
,
a value clearly
rejected by our data. However, there is a large scatter in their M-T relation at
,
which becomes dramatic at
(their Fig. 5). We do not observe such a scatter. It may reflect
systematic errors connected to the extrapolation of the NFW model. As
we discussed above in Sect. 3.2, the precision on
extrapolated mass depends on the precision on the concentration
parameter (i.e., the shape of the mass profile, especially in the
center), which is more difficult to constrain with BeppoSAX than
with XMM-Newton, in particular due to the larger BeppoSAX PSF.
The temperature structure of the ICM in a cluster is the result of the complex interplay between gravitational processes (i.e., the evolution of the gas in the Dark Matter potential), and of any other process that can affect the gas entropy (e.g., radiative cooling and heating from galaxy feedback). The theoretical M-T relation - which should be viewed rather as a T versus M relation when predicted from theoretical studies - depends on the exact modelling of all these processes. Moreover, as we discuss below, comparison of observations and theory also depends on the exact definition of the "average'' temperature, since the gas is never perfectly isothermal.
The normalisation of the M-T relation is particularly well
constrained by our study, the statistical error now being less than
5 per cent at
.
The value of the normalisation depends
on the (sub)sample considered because it is correlated with the slope.
However by choosing a reference temperature of
,
close to the
median temperature, we minimize the effect, and the difference is of
the order of the statistical error. We can thus first compare our
results with the predicted values, quasi-independently of the slope
issue.
![]() |
Figure 4:
The normalisation of the
|
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The difference with the prediction from adiabatic models is not dramatic, particularly when the dispersion among various adiabatic simulations is taken into account. The normalisation is 30 per cent below the prediction of Evrard et al. (1996), compared to typically more than 50 per cent difference in the normalisation derived from different adiabatic simulations (Table 3; Henry 2004). However, as discussed by Muanwong et al. (2002), higher resolution simulations tend to predict higher normalisation, thus exacerbating the discrepancy with our results. Adiabatic simulations probably fundamentally fail to predict the correct normalisation of the M-T relation. The observed discrepancy could in principle be due to incorrect modelling of the dark matter component itself, since it is this which drives the potential. However, we have already argued that this is not the case from the excellent agreement between the observed and simulated mass profiles (Paper I and Sect. 4). A more likely explanation is that non-gravitational processes affect the M-T relation, as they affect all other scaling relations.
From theoretical arguments and from observations of the gas entropy,
it is now clear that both cooling and galaxy feedback have to be taken
into account when discussing relations
involving the ICM (Pratt & Arnaud 2005; Voit & Ponman 2003). We thus focus on published
theoretical studies that
include both phenomena. Their predictions are compared with our
results in Table 3 and in Fig. 4. All of
the quoted simulations are made in the "concordance''
CDM
cosmology, and use the same definition of
as in the
present work. However, they do not always use the same definition
of the temperature (see below).
At a given mass, cooling and galaxy feedback increase the gas
entropy
as compared to the value attained by pure gravitational heating.
In many scenarios, these processes increase the
temperature and, as expected, a lower normalisation is
found when these processes are included in a given numerical
simulation (Thomas et al. 2002; Muanwong et al. 2002) or analytical model
(Voit et al. 2002).
Recent non-adiabatic simulations seem to be quite successful at
reproducing the observed M2500-T relation. The normalisation
derived by Borgani et al. (2004), for a sample of simulated clusters with
temperatures T > 2 keV, is in perfect agreement with our value (see
also
Fig. 3),
while the normalisation derived by Kay et al. (2004b, see also
Thomas et al. 2002) is only
10 per cent too high. These works
used the mass weighted temperature,
,
estimated within
R2500, which is directly linked to the thermal energy. As
discussed in Sect. 2.2 our spectroscopic temperature,
,
should be close to the mass weighted temperature in that region. Thus,
the good agreement between the observed M2500-
and
predicted M2500-
relations is encouraging, and suggests
that the thermal energy content in this central region is roughly
correctly modelled.
Up until recently, the standard temperature definition used to mimic
X-ray observations in numerical simulation studies was the
emission-weighted temperature
.
Using this temperature
definition at
,
the normalisation of Borgani et al. (2004) is
now too high by about 12-20 per cent, the normalisation found by
Voit et al. (2002) is marginally too low and the normalisation found by
Muanwong et al. (2002) at
is 30 per cent too high (Fig. 4). It is likely that the variabality of these
results is linked to differences in the various physical models used.
Independent of the physics, a crucial point seems to be the exact
definition of the temperature. Recently, Mazzotta et al. (2004) introduced
the spectroscopic-like temperature (
)
in order to better
reproduce the temperature obtained from spectral fits when the ICM is
multi-temperature. Mazzotta et al. show that
is biased
towards the lower values of the dominant thermal component, and that
in general
overestimates
.
Unfortunately, this
exacerbates the disagreement between observed and simulated
M500-T normalisations. Using
,
Rasia et al. (2005)
over-predict a normalisation, relative to our values, by a factor as
large as
1.8. Note that Rasia et al. use the same
physical model as Borgani et al. (2004) and yet their normalisation is
50 per cent higher (see Table 3 and also their Fig. 2).
We note that the earlier work of Mathiesen & Evrard (2001), based on
spectroscopic temperatures of adiabatic numerical simulations, showed
a smaller effect.
Strictly speaking these temperatures were estimated with R500,
whereas our spectroscopic temperature measurement
is interior to
R1000). A1413 is the only cluster for which we have
data up to
.
The spectroscopic temperature within
,
is only slightly smaller (by 3 per cent) than
.
This would increase the normalisation of the M500-Trelation by less than 5 per cent if we used
(assuming the
same correction factor for all clusters).
It thus appears that there is a genuine disagreement between observed
and predicted normalisation of the M500-T relation. One
interpretation, as proposed by Rasia et al. (2005), is that the X-ray mass
underestimates the "true'' mass (see
also Borgani et al. 2004; Muanwong et al. 2002). Using
temperatures, they estimated the value of M500that an X-ray observer would derive from their simulation using the HE
equation and a polytropic
-model. The resulting M500-
is indeed now in good
agreement with our observation (Table 3 and
Fig. 4). However, the normalisation is
,
as compared to
when
using the "true'' theoretical mass. This corresponds to a very serious
underestimate of the mass by X-ray observations: the "true'' M500 mass of clusters would be a factor
7.2/4.2= 1.7 higher than
the X-ray mass. We think this is very unlikely, at least for the
masses estimated as in the present work. Firstly, our approach - fitting
an NFW
model and extrapolating the mass profiles - is more sophisticated than
the simple polytropic
-model approach.
Secondly, we note again the
excellent quantitative agreement of our mass profiles with theoretical
predictions.
If we have underestimated the "true'' M500 by a
factor of 1.7, we should also have underestimated the "true'' M2500by the same factor. This is unlikely: from combined lensing/X-ray
studies, Allen et al. (2001) conclude that systematic uncertainties are
less than 20 per cent
. Conversely, for the X-ray
mass profiles to have the correct universal shape, as we have
observed, the predicted difference between the X-ray mass estimates
and the true mass should be roughly constant with radius. This is not
what is expected if the difference is important at
:
it is
linked to differences between the temperature profile derived from
projected
values and the true profile, which depends on the
ICM structure along the line of sight (Rasia et al. 2005; Mazzotta et al. 2004), and
thus a priori on radius. It would be interesting to check this
point
with numerical simulations.
A more likely explanation is that numerical simulations do not
correctly describe the gas thermal structure at large scale, at least
for relaxed clusters considered here.
We note that numerical simulations predict temperature profiles
decreasing with radius, by nearly a factor 2 at
(Borgani et al. 2004, Fig. 6), while the observed profile is flatter
(Fig. 1). This would bias low the
as compared to
the X-ray temperature of real clusters, and thus increase the
normalisation of the M500-
relation
. It would be interesting to
compare the theoretical M2500-
and M2500-
relations, and investigate if there is continued good agreement with
observations. We expect this to be the case since the predicted
temperature variations are not dramatic - less than 20 per cent variations
within
(see Fig. 6 of Borgani et al. 2004 and Fig. 9 of
Kay et al. 2004a), so that
should be close to
.
The observed M-T relation slope is consistent with the self-similar
expectation for the sub-sample of hot clusters (
):
at
,
where it is best constrained.
The slope is significantly higher when the whole sample (T>2 keV) is
considered:
.
A value of
is expected from the virial theorem if clusters
obey self-similarity. All adiabatic simulations confirm this value
(Bryan & Norman 1998; Yoshikawa et al. 2000; Evrard et al. 1996; Eke et al. 1998; Pen 1998; Thomas et al. 2001), including
when a wide bandpass spectral temperature, as measured with Chandra or XMM-Newton, is used to establish the M-T relation (Mathiesen & Evrard 2001).
Numerical simulations including cooling and feedback do predict a
slightly higher slope. However, the effect is smaller than we observe
(
-0.1) and is generally not significant
(Table 3). The only exception is the M500-
relation derived by Rasia et al. (2005):
;
however the
normalisation is then much too high (see above). It is also worth
noting that the phenomenological analytical model of Voit et al. (2002)
yields a steeper slope. We obtained
by fitting their
relation (their Fig. 22) in our temperature range. This is in good
agreement with the observed value; however, in this case the
larger slope is mostly due to the variation of the concentration of
the Dark Matter with mass in their model (Voit et al. 2002), which is
larger than we observe (Paper I).
As a final remark, we want to emphasise that the observed discrepancy
with the standard self-similar value is actually small. The slope
increase, observed when including cool clusters, is significant at most
at the
85 per cent confidence level. Furthermore, at
,
the
limiting temperature of our sample, this corresponds to only -20 per
cent difference in mass as compared to the extrapolation of the best fitting
M-T relation for hotter clusters (see also Fig. 3). There
is scatter in the M-T relation, and our sample comprises only 4 cool
clusters. We thus cannot exclude that the steepening is an artefact of
our particular choice of clusters. We also note that the quality
of the power law fit decreases when including low mass systems. This
may indicate that the M-T relation is actually convex in the log-log
plane, either across the entire temperature range, or below a "break''
temperature. We lack clusters in the intermediate temperature range to
assess this issue. Clearly, a possible discrepancy between predicted
and observed slopes needs to be confirmed and better specified by
considering a larger cluster sample.
Using a sample of ten relaxed galaxy clusters observed with XMM-Newton, we
have calibrated the local
-T relation, in the temperature range
[2-9]
,
at four density contrasts,
.
We used the spectroscopic temperature
estimated within
0.5R200 (
), excluding the cooling
core region, and derived the masses at various
from NFW
profile fits to precise mass profiles measured up to at least
.
We argue that our measured masses are particularly
reliable. The logarithmic slope of the
-T relation is the same at
all
,
reflecting the self-similarity of the mass profiles. The
slope is well constrained and is consistent with the standard
self-similar expectation,
,
for the sub-sample of hot
clusters (
). The relation steepens to
when
the whole sample (T>2 keV) is considered. The normalisation of the
M-T relation is measured with a precision better than
per cent and is 30 per cent below the value predicted by the adiabatic
numerical simulations of Evrard et al. (1996).
Models that take into account radiative cooling and galaxy feedback
are now in good agreement with the observed M2500-T relation.
We argue that remaining discrepancies at
and lower are
more likely to be due deficiencies in models of the ICM thermal
structure, to which the spectroscopic-like temperature seems to be
very sensitive, rather than to an incorrect estimate of the mass from
X-ray data.
More detailed comparisons are needed to understand the origin of the discrepancies between the predicted and observed M-T relations. Our directly measured M1000-T relation now provides the most direct constraint at large scale for numerical simulations. Simulations of mass profiles, as would be determined by an X-ray observer using modern Chandra and XMM-Newton techniques, are also needed. This would be particularly interesting for relaxed cluster sub-samples, and using better representations of observed temperatures (e.g. as proposed by Mazzotta et al. 2004). Such data could be directly compared to observed mass profiles. This would provide information on i) possible overall systematic errors in X-ray mass estimates, and ii) further test the reliability of simulations to correctly reproduce the ICM structure.
On the observational side, study of a much larger, unbiased, sample is needed to i) determine the exact shape of the local M-T relation; ii) study its intrinsic scatter, and iii) assess the effect of cluster dynamical state on the M-T relation.
Acknowledgements
We thank A. Evrard for useful comments on the manuscript. We thank M. Bershady for providing the BCES software and for useful discussions on the statistical analysis. We are grateful to J. Ballet and H. Bourdin for further useful discussions on statistical analysis. The present work is based on observations obtained with XMM-Newton an ESA science mission with instruments and contributions directly funded by ESA Member States and the USA (NASA). E.P. acknowledges the financial support of CNES (the French space agency). G.W.P. acknowledges funding from a Marie Curie Intra-European Fellowship under the FP6 programme (Contract No. MEIF-CT-2003-500915).