Due to the relatively small size of the CORALS survey, it is
not possible to investigate the evolution of DLA statistics
for this sample. However, since our main objective is to
ascertain whether or not a significant fraction of gas has
gone undetected, it is sufficient for us to
restrict our determination of
to the
range
where there appears to be
little evolution. This requires us to omit two DLAs from
our sample (B1251-407a and b), and restrict our
statistical analysis to the remaining 17 DLAs.
![]() |
(1) |
![]() |
(2) |
![]() |
(3) |
![]() |
(4) |
Taken at face value, the estimate of n(z) from the CORALS
survey is 50% larger (at the
same
)
than that found in previous
surveys. For example, Storrie-Lombardi & Wolfe (2000)
deduced
n(z)=0.055(1+z)1.11 = 0.21 (no errors quoted).
However, this difference is only marginally
significant, since the two determinations of n(z)are within
1
of each other.
The mass density of neutral gas in DLAs as a fraction of the closure
density is expressed as
![]() |
(5) |
We also consider another effect. As explained in
Sect. 2, many previous surveys have included in their
statistical analyses candidate DLAs, identified on the
basis of the equivalent width of the Lyman
line rather than
by profile fitting to a damped profile. It is worthwhile
examining the overestimate of
which may
result from this approximation. For the 17 DLAs for which we
have obtained our own spectra, we measure the equivalent
width and compare the implied column density to that
determined by fitting the Lyman
line. In most cases we find
the two techniques to be in very good agreement, certainly
within the errors associated with each method. There are
only three exceptions (the DLAs in B1055-301, B1251-407a
and B2314-409) where the equivalent width determination
leads to a much higher N(H I) than the line fit. Inspection
of Fig. 2 shows that this is due to extended
absorption around the DLA. Although fits of these DLAs were
not straight-forward, this process was facilitated by higher
spectral resolution and coverage of metal lines which
provide additional guidance in the shape of the wings and
.
Had we used the values of N(H I) deduced from
the equivalent widths for the entire CORALS sample, we would have
over-estimated
by 20%. This discrepancy
would have been further increased if extended blends of
lines which do not include a DLA, such as those
present in the spectrum of B1251-407, were mistakenly included.
Nevertheless, the over-estimate is not large and, given the
increasing body of accurate measurements of N(H I) in
DLAs, we think it very unlikely that this effect could be
masking a higher degree of dust bias than that indicated by
inspection of Fig. 3.
Finally, for completeness, we calculate
in the redshift range
where
we detect two DLAs despite the fact that with CORALS we only
sample a total interval
.
The error bars
are naturally very large, but all the same it is intriguing
that
seems to remain high at
-2.37+0.24-0.59 in contrast with the slight down-turn
suggested by the work of Storrie-Lombardi & Wolfe (2000)
and Péroux et al. (2001b). It will be very interesting to
see how better statistics will impact upon the CORALS value
of
at the highest redshifts since
the present determination would suggest an
increase in the importance of dust bias with increasing redshift.
In their preliminary analysis of this sample, Ellison et al.
(2000) found tentative evidence that
was
higher towards fainter QSOs, consistent with the effect
expected from a dust bias. We re-examine this point in
Fig. 5, which shows cumulative statistics for
the CORALS DLAs as a function of the B-band magnitude of
the background QSOs. Since there are relatively few bright
QSOs in our sample, we also show the statistics for the LBQS
DLA survey (Wolfe et al. 1995) which has a limit
,
using the column densities reported by Wolfe et al.
(1995) and Storrie-Lombardi & Wolfe (2000). We confirm the
initial conclusion by Ellison et al. (2000) that
increases as fainter QSOs are observed, but
stabilises at
.
Thus, we do not find a
population of high N(H I) DLAs which is only revealed when
faint (
)
QSOs are observed.
However, closer inspection of the data emphasises the need to extend
our survey in order to fully sample the column density
distribution function, particularly at the high column
density end. The increase in
between the
and
bins is almost entirely due to
a single DLA with N(H I) =
cm-2.
Similarly, the increase between the
and
bins is caused by a single DLA with N(H I) =
cm-2. Between them, these two systems account for
over half of the neutral gas in the entire DLA sample. A K-S
test that compares the distribution of N(H I) among DLAs
towards B < 20 QSOs with those from the large sample of
Storrie-Lombardi & Wolfe (2000) provides inconclusive results, i.e.
that the samples are indistinguishable at only the 1
level.
Taken as a whole, the CORALS DLAs are inconsistent (again only at the
1
level) with the N(H I) distribution of
Storrie-Lombardi & Wolfe (2000). As found by Ellison et al. (2000)
for a sub-sample of the CORALS sample, we confirm that for
the complete sample that there is no strong correlation between
magnitude and redshift out to
.
Therefore, these
trends are not likely to be associated with the evolution
(apparent or real) of the properties of the QSOs themselves.
In addition to the cumulative values of n(z) shown in
Fig. 5, we calculate the number density of
DLAs towards QSOs with
and B < 20, and find
n(z) = 0.38+0.20-0.14 (at
)
and
0.27+0.11-0.08 (at
)
respectively. For the B <
20 subset, this value is consistent with the number density
found by Storrie-Lombardi & Wolfe (2000). Again, we see
that there is an excess of DLAs in faint QSOs, but only at
the
1
significance level.
Copyright ESO 2001