The presence of intervening gas in the sightline to a high redshift QSO will cause absorption lines to be superimposed on the quasar's continuum. This relatively simple physical process allows us to study in detail the properties of gas clouds in front of QSOs, whether in the intergalactic medium or in the galaxies giving rise to high column density damped Lyman alpha Systems (DLAs). DLAs are one of the key components of the universe at high redshift because, although relatively rare, they account for most of the neutral gas available for star formation.
Measuring the redshift evolution of
(the total
amount of neutral gas traced by DLAs expressed as a fraction of the
closure density) has traditionally been seen as a tool for
probing the history of assembling galaxies and measuring the rate
at which they convert gas into stars (e.g. Lanzetta et al. 1995; Pei & Fall 1995; Storrie-Lombardi et al. 1996; Storrie-Lombardi & Wolfe 2000; Rao & Turnshek
2000). Similarly, chemical abundances in DLAs have been used to
trace the metallicity evolution of galaxies over most of the
Hubble time (e.g. Pettini et al. 1997; Pettini et al. 1999;
Prochaska & Wolfe 1999, 2000). However, the interpretation
of both DLA abundances and
as indicators of
galaxy evolution
is pivotal upon the assumption that DLAs are
representative of the bulk of "normal'' galaxies at each redshift
sampled. Therefore, it is rather surprising that, at least for
current samples of DLAs, no strong evolution of either
or metallicity (
)
has been revealed
by the above studies from
down to
.
One possible explanation is that DLAs are representative of only
a particular evolutionary stage in a galaxy's lifetime.
Alternatively, current DLA
samples may be incomplete due to a selection bias.
In this paper, we specifically investigate the possibility that
dust extinction may have produced incomplete samples of
DLAs in previous surveys based on optically-selected QSOs.
DLAs appear to remain relatively metal-poor
(
)
from
to
(Pettini et al. 1999; Prochaska & Wolfe 2000).
However, it has been noted by several authors that the
absorbers with the highest values of hydrogen column density
are all of low metallicity and dust content
(e.g. Pettini et al. 1997; Boissé et al. 1998;
Pettini et al. 1999; Prantzos & Boissier 2000; Savaglio 2001). Whilst
relatively metal-rich damped systems do exist, they tend to
have values of N(H I) towards the lower end of the range
considered for DLAs,
cm-2. Boissé et al. (1998) and Prantzos &
Boissier (2000) in particular have pointed out an apparent
anti-correlation between N(H I) and metallicity.
Since the census of metal abundances (using the column-density weighted
average) is dominated by the highest N(H I) absorbers, such an
anti-correlation could
explain the lack of metallicity evolution in the present
samples of DLAs. This anti-correlation between N(H I) and metallicity
may reflect a bias against high-column-density,
metal-rich DLAs with sufficient dust to obscure background
QSOs from the eyes of magnitude-limited optical surveys.
Further evidence that optical magnitude-limited QSO samples may be incomplete due to dust bias comes from consideration of the spectral energy distribution of quasars with and without DLAs. Fall et al. (1989) and Pei et al. (1991) found evidence that QSOs with DLAs have systematically steeper continuum slopes than quasars with no damped absorber. A similar conclusion was reached by Carilli et al. (1998) who found that a high fraction of their "red'' QSO sample had associated 21 cm absorbers compared with QSOs selected solely for the presence of Mg II absorbers. By modelling the extinction effect of dust, Pei & Fall (1995) estimated that at z = 3 between 27% and 44% of QSOs and 23%-38% of DLAs may be missing from B-band selected quasar samples.
The objective of the Complete Optical and Radio Absorption
Line System (CORALS) survey presented here is simple and
straightforward: compile a homogeneous sample of
radio-selected QSOs and obtain medium resolution spectra of
every target, regardless of optical magnitude. In this way
it should be possible to determine quantitatively the
severity of the dust bias implied by the observations
reviewed above. The present paper is the first in the CORALS
series. Here we define the sample (Sect. 3),
describe the observations and present the QSO spectra
(Sect. 4), identify the DLAs (Sect. 5), and
calculate their number density and
(Sect. 6).
We adopt an
cosmology and
use H0 = 65 km s-1 Mpc-1 throughout the paper.
Copyright ESO 2001