R. Bandiera1 - E. Corbelli2
1 - INAF - Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5,
50125 Firenze, Italy
2 -
INAF - Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5,
50125 Firenze, Italy
Received 27 July 2004 / Accepted 20 December 2004
Abstract
Murphy et al. (2003a, MNRAS, 345, 609) claim to find evidence of cosmological variations of the
fine structure constant
in the spectra of intervening QSO absorption
line systems.
We find that this result is affected by systematic effects.
The
values estimated in individual line systems depend on the set of
atomic transitions used and therefore the quoted dependence on the cosmic age
may reflect the fact that different sets of transitions are used at different
redshifts.
A correlation between line shifts and relative optical depths of the atomic
transitions is also present.
This correlation is very tight for a high-redshift subsample and accounts for
the anomalous dispersion of the
values found by Murphy et al. (2003a)
in this subsample.
The above correlations are consistent with a scenario in which gravitational
redshift, caused by the gravity of the dark halo, contributes to the shift in
frequency of individual components.
Gravitational redshift causes differential spectral shifts of the same order as
magnitude of those measured.
In the presence of line misidentification, these shifts can be interpreted in
terms of a variable
.
In order to verify the gravitational redshift hypothesis, a direct access to
Murphy et al. (2003a) data, or to a large amount of new high resolution data,
is necessary.
Key words: quasars: absorption lines - galaxies: halos - cosmology: miscellaneous
A recent work by Chand et al. (2004), based on more accurate measurements in high
quality data relative to a smaller sample objects, uses the MM method with
well-defined selection criteria.
No cosmological variation of
is found, with a 1-
uncertainty of
(namely an order of magnitude below the values quoted by MWF).
Chand et al. (2004) avoid very weak and blended lines and point out that when one
does not do so, spurious detections are frequently seen.
Using a different but very robust method, Bahcall et al. (2004) also do not find any
relevant time dependence of the fine structure constant.
Bahcall et al. (2004) point out several inconsistencies in the results of MWF which
imply that systematic uncertainties due to misidentification of lines might be
significant in the MM method used by MWF.
In order to directly test the hypothesis of component misidentifications, one
needs to investigate in detail the original data and the routines used by MWF
in their analysis: this information is, however, not accessible to the
community.
As emphasized by Chand et al. (2004) and by Bahcall et al. (2004), MWF have not described
their algorithm of line identification, the confidence level adopted and the
physical assumptions made.
So, line misidentifications cannot be excluded in their results.
Given the overwhelming consequences in the fundamental physics and
cosmology of the variability of the fine structure constant (see
e.g. Uzan 2003; Martins 2003; Uzan 2004), any newly suggested potential source of bias in the
determination of
must be examined in detail.
Direct access to MWF data and analysis would facilitate this process.
At the moment, however, we are forced to approach the problem in different
ways.
In the present paper we investigate the statistical properties of the data
presented by Murphy et al. (2003a, their Table 3), and we find correlations that can
be explained only in terms of a systematic effect, not accounted for by MWF
(Sect. 2).
In Sect. 3, we put forward the hypothesis that differential gravitational
redshift (hereafter GRS), within absorption systems, may be responsible for the
correlations found and of the non-zero value of
.
An important feature of GRS, with respect to other effects, is that symmetry
between red- and blueshifts is broken, and therefore a systematic effect on the
average values of the spectral shifts may be accounted for.
This effect is very tiny, and it can be detected only under particular
conditions.
In the MM analysis, GRS appears in only if misidentifications of some components
are present.
In Sect. 4, we search for correlations between
and some indicator of
the gravitational potential, for various absorption systems: the presence of
such correlations represents a strong clue that some differential redshift is
of gravitational origin.
Our last section summarizes and concludes that GRS is a possible candidate for
the origin of the measured differential redshift.
The central working hypothesis of MWF for evaluating
is the
proportionality between the line shift and the atomic relativistic correction
for all atomic transitions detected in the spectrum of each component of an
absorption system.
In the framework of the MM method, one expects the following relation to hold
for each atomic transition i:
![]() |
(1) |
We start with the working hypothesis that there is a primary correlation
between the relative optical depth of a transition and
,
i.e. that the
primary correlation is not that between Qi and
.
A preliminary step is to estimate, for a "typical'' absorber, the relative
optical depths of all transitions used by MWF.
We define the relative optical depth of the ith transition,
,
as the
optical depth scaled to that of a reference transition (from now on we
skip, for simplicity, the index i).
In this paper we will use Fe II at 2382 Å as the reference transition.
We take a sample of low-z absorbers (Churchill & Vogt 2001; Churchill 1997) to determine the column
density of Mg I and Mg II relative to that of Fe II , and a sample of high-zabsorbers (Prochaska et al. 2001; Prochaska & Wolfe 1999) to determine the column density of Al II , Al III ,
Si II , Cr II , Ni II , and Zn II relative to that of Fe II .
We have linked the low and high-z sets of data to derive the
relative optical depths of all transitions of interest.
Table 1 gives the decimal logarithm of the relative optical depth,
,
the logarithm of the relative column density,
,
the Q coefficient, and some other basic data (ionic species, wavelength, and
oscillator strength f, as given by Prochaska et al. 2001) for all transitions used.
Table 1: Atomic data.
Table 2: High-contrast absorption line systems.
We define the standard deviation in ,
and the linear correlation
between
and Q as:
s | = | ![]() |
(2) |
![]() |
= | ![]() |
(3) |
The values of s and
may change from one absorption system to another,
but there are absorption systems with equal values of s and
.
In principle, spectral lines should be weighted with their specific relevance
to the fit; however, in our simplified analysis we assume that all transitions
used for an absorption system are equally relevant.
The use of
,
instead of
,
has the advantage of limiting the
dispersion, even though the resulting correlations are qualitatively similar to
those obtained using
.
If
correlates with Q, the primary correlation between
and the measured
induces a spurious correlation between Q and
.
In the MWF analysis this leads to a
different from zero.
Our complete sample is that listed in Table 3 of Murphy et al. (2003a).
We subdivide this into low-z and high-z subsamples, using a spectroscopic
criterion: an absorber is included in the high-z sample only if it has been
observed in at least one transition at wavelengths shorter than 2300 Å.
Murphy et al. (2003a) have noticed that a subsample of systems (called the
"high-contrast
sample''), observed in many transitions with very different relative optical
depths, has a statistical spread in
much larger than the average
nominal uncertainty of each absorber.
The authors ascribe this discrepancy to uncertainties not accounted for in
their analysis, but they exclude that this may lead to systematic effects in
the determination of
.
We shall reach a different conclusion.
![]() |
Figure 1:
a) Distribution of the data in the s-z parameter plane and b) in the s-![]() |
Open with DEXTER |
Figure 1 shows the complete set of data in the s-z plane, and in
the s-
plane.
Figure 1a shows that our criterion, although purely based on
the set of transitions used, effectively separates lower and higher-zabsorbers, with a shallow cut around
.
Values of s for low-z absorbers are limited to the range (0.3, 0.7);
values of s for high-z objects lie in the range (0.3, 1.2).
High-contrast absorption systems typically correspond to higher values of s(say, above 0.8): this indicates that, at least on average, the quantity
s accounts reasonably well for the spread in relative optical depth of the
atomic transitions used.
Because different sets of transitions are used for different redshifts, any
cosmological implication of measured variations of
with redshift
should be taken very cautiously.
Notice that, in addition, the low-z and high-z samples given by
Murphy et al. (2003a) correspond to different kinds of absorbers.
The low-z sample is mostly composed of absorption-line systems selected by
the Mg II lines,
and have moderate HI column densities; while a large fraction of the
high-z sample is made up of damped Ly
absorption systems.
Therefore, we should not be surprised if, in our analysis, different results
are found for the two sets of systems, since they have been analyzed in
different sets of transitions, and furthermore are associated with different
types of cosmic structures.
In the two subsections below we will search for whether individual values of
depend on
.
A significant correlation would prove that our working hypothesis is
correct; if instead the MWF results correspond to a true variation of
no correlation should be found.
For
positive, the (spurious) correlation between
and Qwill have the same sign as the primary correlation between
and
.
For
negative the correlation will have the opposite sign.
In order to obtain a negative
when
is positive,
must decrease for increasing
.
When
is negative
must increase for increasing
.
According to our working hypothesis, the closer the
value is to
,
the larger the displacement from zero of the
value for each system.
Therefore we expect a correlation between
and
.
The average value of
over the whole sample will be different from
zero, provided that the
distribution is not symmetric around zero.
Figure 1b shows that negative values of
are mostly
associated with low-z objects (64 objects).
A weighted linear regression between
and
results in a
positive slope, although at a low significance level:
,
with a reduced
of 1.10 (assuming a functional dependence
).
A tighter result (
)
is obtained assuming a functional dependence
:
,
with a reduced
of 1.09.
Below we again will use the symbols m and m0 to indicate the best fitting
slope leaving q free, or setting q=0.
As can be seen in Fig. 1b, low-z objects present a
bimodal distribution, consisting of one component with
in the range
(-0.92, -0.80), and of another one with
in the range
(-0.52, 0.01).
The former component is highly uniform in
(39 objects with an average
value of -0.85) and the average
is
.
For the other component (25 objects with an average
value -0.35) we
have instead
.
A comparison of the two subsamples again suggests that
increases with
.
However, as already obtained from the linear regression, the significance of
this trend becomes compelling only if we assume that
vanishes when
.
It is worth investigating another recently published work (Chand et al. 2004), which
analyzes the spectra of a sample of low-z absorption systems.
The authors do not find any evidence of a VFSC and give an upper limit of
to
.
This is about one order of magnitude smaller than the signal claimed by MWF.
The sample of Chand et al. (2004) is smaller than that of Murphy et al. (2003a) but the
quoted errors of
are smaller because high resolution observations
allowed them to select only systems with all individual components identified
unambiguously.
The decision of applying a severe selection of the systems could either render
the approach cleaner than that of MWF, or potentially more subject to biases.
Here we check whether the correlation between
and
,
found
in the MWF low-z sample, is also present.
Values of
in Chand et al. (2004) were obtained using all transitions listed
for each of the 23 absorption systems in their Table 3 (even if some components
were analyzed by Chand et al. (2004) using a subsample of these transitions).
The estimated slope for the
-
linear regression is
,
with a reduced
of 0.94; in the case of a pure
linear proportionality we have
,
with a reduced
of 0.91.
This result is consistent with no correlation between
and
,
down
to a 1.1-1.5
level, namely at a level 5-8 times smaller than the
correlation found in the Murphy et al. (2003a) results.
We have also used different methods of object selection, such as limiting our
choice to systems in which both Fe and Mg transitions are detected in all
components (12 objects) or to systems in which the same set of transitions has
been used for all components (8 objects).
The conclusion, to a rather high level of confidence, is that the correlation
is not visible in the Chand et al. (2004) results.
Their method does not seem to be affected by the unwanted systematic effects
found in Murphy et al. (2003a).
Figure 1b shows that high-z absorbers are distributed more
continuously over a wider range of ,
namely (-0.6, +1.0).
With respect to the low-z sample, the high-z sample shows a much larger
dispersion in s (see Fig. 1), and therefore it may be better
suited for searching for effects which arise when using transitions with a wide
range of relative optical depths (i.e. cases with large s values).
Figure 2 shows how the measured values of
depend on s in
this sample.
While no apparent trend is present for s<0.8, for larger s values there is
a clear trend of decreasing
with s.
A difference between these two subsamples is present also in the measured
values of
:
the average of
for s<0.8 (38 objects) is
,
for s>0.8 (26 objects) is
.
The discrepancy between these two values is at a
level.
A result similar to the s>0.8 sample, namely
,
is
obtained for the high-contrast sample: this is a rather obvious result, since
the two samples are partially overlapping.
In the remaining part of this section, we concentrate on a statistical
analysis of the high-contrast subsample.
![]() |
Figure 2:
Dependence on the spread in the relative optical depths s of the
![]() ![]() ![]() |
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The high-contrast sample is made of 22 objects for which Murphy et al. (2003a) have
measured an excess dispersion of
.
We propose that this excess dispersion results from the presence of hidden
variables, one of which is
.
A simple way to derive how
varies with
is to evaluate the
average
for systems with negative and positive
:
we obtain
equal to
and
respectively,
two values which are
apart.
A weighted linear regression between
and
on the high-contrast
sample gives a slope
(
level).
Assuming that
vanishes at
,
the slope is
(
level).
In spite of the good significance level of
-
regressions for the
high-contrast sample, their reduced
values are still large, of the
order of 3.
A possibility is that the Murphy et al. (2003a) hypothesis applies mostly to heavily
damped systems, because they are complex systems, containing many saturated
lines, while our conjecture of the presence of hidden variables may better
apply to absorption systems below a critical column density,
.
![]() |
Figure 3:
Correlations between
![]() ![]() ![]() ![]() |
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In Table 2 we list all high-contrast systems, and we indicate the
H I column density whenever this can be found in the literature (the relative
references are listed in the last column).
For a few cases the H I column density is unknown: we assume for those that the
H I column density is below
.
In Fig. 3a we show the data of Table 2 for
.
A weighted linear regression for these systems gives a slope
(with a reduced
of 3.62); or alternatively
(with a reduced
of 3.37).
Therefore there is no evidence of correlation in this subsample.
For
instead a weighted linear regression gives
a slope
(with a reduced
of 0.91);
Fig. 3b displays this result.
Alternatively,
(with a reduced
of 1.87).
Here both regressions determine the slope at a significance level of about
.
The result we find is striking: the correlation between
and
is
very tight for low column density systems and it loses its significance for
heavily damped systems.
One worry about choosing
as low as
might be the 3
unknown H I column densities of Table 2.
These can turn out to be higher than
.
However, we have checked that as soon as
the
significance of the correlation stays above
for
(even though the dispersion increases) and stays below
for
.
For
for example, our last two statements are true not
only if all the unknown H I column densities are below
but also if we
do not consider for the correlations the two entries relative to the (C02)
reference of Table 2, or if we consider one or both of them to be higher than
.
In this section we discuss GRS in absorption systems, and its possible influence on the quoted variation of the variable fine structure constant. GRS can be detected in many types of bound systems such as stars, galaxies and clusters of galaxies (e.g. Broadhurst & Scannapieco 2000; Stiavelli & Setti 1993), and has been used to infer physical parameters like the total mass. It is likely that absorption systems are localized in dark matter halos of galaxies, but since they can be observed only along one line of sight, whose position with respect to the system barycentre is unknown, it is not easy to quantify the magnitude of GRS in observable quantities. To check explicitly if and how GRS plays a role in the MWF analysis is even more difficult because their data and procedure are not available to the public.
In order for GRS to be responsible for the fine structure constant variations measured in absorption line systems with the MM method, three conditions are required:
In the rest of this section we examine these conditions in more detail.
In Sect. 4, we test in a more quantitative way the GRS hypothesis, by
searching for correlations between the estimated
and indicators of the
gravitational potential in the absorption system.
The aim of this subsection is to evaluate, for typical gaseous systems embedded
in dark matter haloes, the magnitude of the differential GRS.
Photons of frequency
emitted in a gravitational potential
are
observed at infinity to be redshifted by an amount
![]() |
(4) |
Let us consider gaseous systems embedded in dark matter haloes whose density
profile is described by the formula proposed by Navarro et al. (1997,1996):
![]() |
= | ![]() |
|
![]() |
![]() |
(6) |
An interesting result of Fig. 4 is that the velocity shifts are of the same order of magnitude as those found in the analysis of Murphy et al. (2003a, see their Table 4) and used to claim a VFSC. The estimate of differential GRS presented above refers to the whole absorption system; differential GRS within individual clouds (detected as individual components in the line profile) is much smaller.
![]() |
Figure 4:
GRS in
![]() ![]() |
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We outline here the most appropriate conditions to detect GRS effects in QSO
absorption systems.
In principle, GRS could be detected using even a single transition, if the
available sample of absorption lines is large enough to justify a statistical
approach.
In fact, isotropy arguments show that, in the absence of GRS, kinematic
redshifts of individual spectral components should average to zero with a
symmetric distribution in the whole sample.
GRS, instead, induces skewness in the spectral distribution of the absorption
components, because absorption lines located more deeply in the potential well
are those more strongly redshifted.
In this kind of analysis, the main practical difficulty is to cope with the
smallness of this effect, compared to both instrumental and statistical
uncertainties.
Even in the absence of instrumental uncertainties, there is a minimum number of
spectral components below which it is impossible to extract the gravitational
shift from the statistical dispersion due to kinematic motion.
The problem is qualitatively similar to that of determining, with accuracy
,
the average shift for a sample of components whose distribution shows a
dispersion
:
in this case at least
different components are required.
If we aim at detecting
,
while the dispersion of the
individual absorption components is
,
at least
106components are required, a number far beyond that available in the present data
sets.
This argument, even though in a more complex formulation, should apply also in
a multi-line approach.
A smaller number of components may be required if the velocity pattern of the
material changes smoothly with position.
For illustration, we present here a reasoning based on the
assumption that all blobs move in circular orbits, seen edge-on, in a
potential consistent with the profile given in Eq. (5).
In this case, at a given radius R, the orbital velocity and the gravitational
redshift (expressed as a velocity) are given respectively by:
![]() |
= | ![]() |
|
![]() |
(7) | ||
![]() |
= | ![]() |
(8) |
We consider a path along a line of sight with impact parameter d with respect
to the centre of the system:
,
where l is the coordinate
along the line of sight.
We then compute
and the radial component of
(
).
Results are displayed in Fig. 5 for different values of d.
While by a pure dimensional argument one would always expect values of the
order of
,
Fig. 5 shows that there may be
conditions in which this ratio can be one, or even two orders of magnitude
higher.
In addition, in the case of orbits tilted by an angle
,
a further
factor should be included.
This shows that, under favorable conditions, a sample of
100 components,
spread over a set of absorption line systems, may be sufficient to get a
statistically significant detection of GRS.
![]() |
Figure 5:
Relative change of
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MFW aim at comparing components, in different transitions, which are attributed
to the same cloud, i.e. to the same physical region within the absorption
system.
Of course, if this goal is reached, no GRS would be detected.
Let us examine instead the case of "component misidentification'', namely the
case in which two components, identified in the line profile of two or more
different transitions, are erroneously attributed to the same cloud.
There may be different reasons why a given transition effectively samples inner
region clouds compared to another transition.
This may happen, for instance, if chemical or ionization radial gradients are
present in the absorption system.
There is some evidence of chemical and ionization inhomogeneities in high
column density absorbers, for example, which are very numerous in our high-zsample (Petitjean & Srianand 1999; Petitjean et al. 2002).
But even in the absence of such gradients, inner regions are usually denser
than outer regions, and absorption lines of different relative optical depth
saturate at different distances from the centre and lines.
For this reason, lines with different
might effectively sample different
regions in the potential well, and therefore may be subject to different levels
of gravitational redshift.
From this scenario it naturally follows that one should find a correlation
between
and
for different transitions, and therefore a
correlation between
and
(see Sect. 2).
Therefore our working hypothesis of Sect. 2 (a primary correlation between
and
)
is derived naturally from the idea that GRS and
component misidentification may play a role in some determination of
.
In our framework, if transitions of different relative optical depths sample
different regions of an absorption system, high-contrast absorption systems
should in fact be the most appropriate ones to reveal effects of differential
gravitational redshift.
The correlations we discuss in Sect. 2.2 indicate indeed that strong
systematic effects are present in this subsample.
Table 3: Fe II -selected absorption line systems.
In the presence of component misidentification, if clouds seen in absorption
in two different transitions are typically located at different distances from
the centre, their frequency ratio is affected by the different radial
velocities as well as by the different halo gravitational potential felt by the
two clouds.
Symmetry arguments imply that spurious deviations caused by the different
kinematic properties of the clouds average to zero in a suitably large sample.
Therefore only GRS can reasonably account for any residual systematic shift in
the average value of
.
In Sect. 2 we have shown that the concept of is very effective in searching for hidden correlations.
This does not necessarily imply that GRS plays a role in generating
systematic effects, even though some working hypotheses suggest that it
might.
In this section we assume that, for a uniform sample in
,
the derived
value of
is roughly proportional to the level of GRS.
Since GRS is a function of the galactic potential, we investigate whether
correlates with indicators of the gravitational potential strength.
The gravitational potential depends on the total mass associated with the
absorption system and on the radial distance of the absorbing material from the
centre of mass, but unfortunately none of these physical quantities is directly
measurable from absorption data.
A way out is to identify observable quantities, which correlate with total mass
and radius.
A quantity that can correlate with the strength of the gravitational potential is the metal column density. In fact, for constant metal abundances, more massive absorption systems have higher gas column density (and therefore higher metal column densities). In addition, metals are expected to be overabundant towards the centre of the potential well or in more massive systems because of the longer star formation history.
In this section we examine two samples of objects, both with known Fe II column
densities (hereafter
).
The first one contains low-z absorption systems (as listed in Table 3
of Murphy et al. 2003a) that have well documented
along the line of sight.
Most of these objects have been analyzed by Churchill (1997, C97), or by
Churchill & Vogt (2001, CV01).
In order to obtain a uniform sample, we have limited our selection to these two
references.
The resulting sample contains 24 absorbing systems at redshifts
,
and their
is listed in Table 3.
This sample is statistically consistent with the larger low-z sample analyzed
in the previous section.
Our second sample contains high-z, damped Ly
absorption systems (with
cm-2 and
).
In order to have a nearly uniform sample we select 22 of them with
,
and published values of
in at least one of the
following references: (L96) Lu et al. (1996), (PW96) Prochaska & Wolfe (1996), (PW97)
Prochaska & Wolfe (1997), (PW99) Prochaska & Wolfe (1999), (P01) Prochaska et al. (2001).
The sample is listed in the last 21 entries of Table 3.
In order to estimate the dependence of the measured values of
on
,
we will use a linear regression, adopting the functional dependence
.
In this way, for the whole low-z sample of Table 3, we obtain
and
,
with a reduced
of
0.90: the value obtained for the slope m is not statistically significant
(
).
For the high-z sample of Table 3, instead, we calculate
and
,
with a reduced
of
2.65: a reasonable (
)
significance level is obtained here, but the
reduced
is anomalously high.
We attribute this result to the fact that some of the quoted uncertainties on
,
which are relative to high-contrast damped systems, are
underestimated (see Fig. 3a, and the discussion in
the previous section).
In fact, if we compute a linear regression on the high-z sample, assigning
the same uncertainty to all measurements of
,
we obtain
and
:
therefore, also in this
case the slope m is not statistically significant.
We attribute the low significance of these correlations to the fact that none
of the two samples is uniform in
.
Luckily, 18 out of the 24 objects of the low-z sample lie in a narrow range
of ,
namely
(-0.92,-0.79).
The correlation becomes more significant if we select only absorbers with high
values in this
range.
Taking
(12 objects) we obtain
(
)
and
,
with a reduced
of 1.14.
For
(6 objects)
(
)
and
,
with a reduced
of 0.92.
This result is consistent with a
that deviates significantly from zero
only for
larger than about 13.5.
The
deviation is towards more negative values as
increases.
Although the statistical significance is not high (only 2.8
in the best
case), one should notice that negative deviations of
for negative
are consistent with the increase of
with increasing
,
obtained in the previous section for the low-z sample.
This can be explained in terms of an effective line segregation, with weaker
lines sampling effectively regions closer to the centre of the potential well.
GRS is a reasonable candidate to explain the decrease in
with
increasing
,
because systems with higher metal column density are
either closer to the centre of the potential well, or located in more massive
systems or both.
There have been other proposals to explain the VFSC result.
Of particular interest is the consistency of the VFSC values with a non-solar
isotopic ratio of
occurring at large
redshifts.
If this isotopic ratio increases at large redshifts, small apparent shifts
would be introduced in the absorption lines (Ashenfelter et al. 2004).
These shifts mimic a VFSC if instead a solar isotopic ratio of magnesium is
used, as in the MWF analysis.
The large uncertainty about this proposal lies in the magnesium isotopic ratio
variations with metallicity.
Ashenfelter et al. (2004) show that an Initial Mass Function (IMF) particularly rich in
intermediate mass stars is needed for an increase of the magnesium isotopic
ratio with decreasing metallicity (in the range [Fe/H] =0, -1.5).
Analyses of low metallicity star data (Gay & Lambert 2000) show instead an opposite
trend of the magnesium isotopic ratio variations with metallicity.
If the data by Gay & Lambert (2000) reflect the situation in QSO absorbers, which have
lower metallicity than solar, then magnesium isotopic ratio variations cannot
explain the negative
reported by MWF.
In this case metallicities lower than solar would correspond to lower magnesium
isotopic ratios and to positive value of
.
If one assumes instead that the results of Ashenfelter et al. (2004) apply to gas in QSO
absorbers, then magnesium isotopic ratio variations can explain the MWF
results.
The correlation between
and metallicity should in this case be
positive for a certain range of [Fe/H] (which depends on IMF and yields).
For the GRS hypothesis instead large variations of
should be
associated with large potential wells.
Since more massive galaxies have had a longer star formation history, a negative
correlation between metallicity and
should appear.
The results of this Section seem to favour the GRS hypothesis, but accurate
metal abundances, higher significance in the outlined correlations and more
information on earlier IMF are needed to draw any conclusions on the magnesium
isotopic ratio variation hypothesis.
Even though we cannot disprove completely the VFSC hypothesis of Murphy et al. (2003a),
in
this paper we have discovered systematic effects which can mimic a non-zero
.
Often
depends on
,
the correlation coefficient between two
atomic quantities: the relative optical depth and the relativistic correction
coefficient Q.
For the atomic transitions used in the MWF analysis for each absorber, we
evaluate
and notice that the
distribution is not symmetric around
zero: this justifies the net displacement of the average
from zero.
In particular, the correlation between spectral shifts and the relative optical
depth of the various transitions seems to be the origin of correlations between
spectral shifts and Q, used by MWF as evidence for a VFSC.
Non-zero values of
may then be the result of GRS if lines of different
relative optical depth effectively sample regions at different distances from
the centre of the potential well.
We have examined the low-z and the high-z samples of Murphy et al. (2003a)
separately, since they have been analyzed in different sets of transitions and
furthermore are associated with different types of cosmic structures (see
Sect. 2 for more details).
In the low-z sample the correlation between
and
can be
interpreted in terms of a primary positive correlation between
and
the relative optical depth: that means that relatively weaker lines are more
redshifted than others (i.e.
more negative).
This is in agreement with what one would expect from GRS, under the hypothesis
that intrinsically weaker lines are visible only through dense regions, located
closer to the centre of the absorption system.
Since for this sample most of the systems lie in a restricted
range, and
we know the metal column densities, we compare
with the derived
values.
Systems with higher
values have more negative
values.
This again confirms the GRS hypothesis since more negative
can be
interpreted as more heavily gravitationally redshifted lines.
High
values are in fact expected when the gas lies in regions of
strong gravitational potential.
If future data prove a positive correlation between
and metal
abundances, this will support GRS-related studies and weaken other
proposals, such as the magnesium isotopic ratio variations, for explaining the
non-zero value of
derived in the MWF analysis.
For the "high-contrast'' subsample of the high-z systems, for which
Murphy et al. (2003a) have reported an anomalous statistical dispersion in
,
we
find instead a systematic effect that can be interpreted in terms of a primary
inverse correlation between
and the relative optical depth.
Further dividing this subsample into heavily damped systems, with
,
and systems with
,
we have discovered that the
latter subsample shows a striking inverse correlation, at a level higher than
for
.
No correlation is present for
.
So, while for the heavily damped systems the MWF interpretation of the
anomalous statistical dispersion might be correct, for lower column density
systems we believe that the anomalous statistical dispersion is indeed the
effect of an underlying correlation.
Note that the sign of the correlation between
and
for the
high-contrast (high-z) sample is opposite to that obtained for the low-zone.
If this correlation is interpreted in terms of GRS, stronger transitions should
be associated with innermost regions of the absorption system.
This is opposite to what is inferred for the low-z sample, and requires the
presence of physical inhomogeneities within the system (as actually found
in some cases. e.g. Petitjean & Srianand 1999; Petitjean et al. 2002).
However, one cannot exclude that the opposite trends simply arise because the
bias comes out differently in the MWF procedure used to estimate
:
this is because the data and the characteristics of the absorption systems in
the two samples are very different.
As already pointed out, a more detailed analysis can be carried out having
access to the original data.
For instance, it would be useful to obtain subsamples analyzed uniformly, using
the same set of transitions.
Conversely, one could also investigate how
changes with different
choices of the fitted transitions, in the same absorption system.
More generally, instead of determining how
correlates with Q(from which
is determined), one should search for correlations of
with other quantities, such as the relative optical depth.
Notice that any quoted variation of
with cosmological time should be
taken very cautiously, because different sets of transitions are used for
different redshifts.
In a recent work, Chand et al. (2004) found no variation in the fine structure
constant for a sample of low-z absorption systems.
They obtained this result avoiding both weak and saturated lines, as well
as heavily blended spectral regions.
In this way they restricted their analysis mostly to intermediate
"satellite components'', avoiding the ones relative to central or outermost
regions.
Therefore they reached a better accuracy in positioning the
subcomponents.
A contamination of GRS on
is possible only in the
presence of some bias in the spectral analysis.
We do not find any significant correlation between
and
in
the Chand et al. (2004) results.
Their work further supports the idea that biases may originate from the fit of
weak spectral components or of the saturated and complex parts of a line
structure.
Moreover, GRS effects are harder to detect in a sample which avoids the
centremost and outermost regions since this choice effectively restricts the
range of the potential well tested.
We would like to encourage any future GRS experiment over cosmological distances since the results can be unique tools to test structure formation scenarios in the context of several cosmological models. For example if at redshifts as high as 4-5 the Universe is still dominated by small mass objects (Cold Dark Matter scenario), GRS-induced line frequency shifts in absorption systems at such redshifts should be smaller than the ones detectable at more recent times. Also theoretical models of possible variations of the fine structure constant, which take into account the observational state of the art are needed (see e.g. Steinhardt 2003), in order to check the consistency of different results.
Acknowledgements
We are grateful to the referee and to Charles Steinhardt for many valuable comments to the original version of this manuscript.