![]() | Annu. Rev. Astron. Astrophys. 1999. 37:
487-531 Copyright © 1999 by Annual Reviews. All rights reserved |
3.4. Narrow Absorption Line Results
In contrast to the BALs, intrinsic NALs might be the best abundance probes
we have for QSO environments. Resolved measurements of NAL multiplets allow
us to measure both the coverage fractions and true column densities
(Section 3.2.2). The NALs also allow
separate measurements of important
lines that are often blended in BAL systems, such as NV
1239,
1243-Ly
, OVI
1032,
1038-Ly
, and
many others. We therefore have
potentially many more constraints on both the ionization and abundances.
Early NAL studies did not have the quality of data needed to derive column
densities and abundances, but several groups noted a tendency for
larger NV/CIV line strength ratios in za
ze
systems compared with za << ze
(Weymann et al. 1981,
Hartquist & Snijders
1982,
Bergeron & Kunth
1983,
Morris et al. 1986,
Bergeron &
Boissé 1986).
This trend is probably not caused simply by higher ionization in
za
ze
absorbers, because recent studies show that za
<< ze systems typically have strong OVI lines
and therefore considerable high-ionization gas; NV appears to be weak
relative to both CIV and OVI at za <<
ze
(Lu & Savage
1993,
Bergeron et al. 1994,
Burles & Tytler
1996,
Kirkman & Tytler
1997,
Savage et al. 1998).
The lower NV/OVI and NV/CIV line
ratios at za << ze could be
caused by an underabundance of nitrogen (compared with solar ratios) in
metal-poor intervening gas
(Bergeron et al. 1994,
Hamann et al. 1997d,
Kirkman & Tytler
1997). This
would be the classic abundance pattern involving secondary nitrogen
(Vila-Costas &
Edmunds 1993).
Relatively higher
N abundances and thus stronger NV absorption lines should occur
naturally in metal-rich environments near QSOs (see
Section 2.6 above and
Sections 6
and 7 below).
The first explicit estimates of za
ze
metallicities were by
Wampler et al.
(1993),
Möller et al.
(1994),
Petitjean et al.
(1994),
Savaglio et al.
(1994)
for QSOs at redshifts of ~ 2-4. These studies
found that za
ze
systems often have Z
Z
, which
is at least an order of magnitude larger than the za
<< ze systems measured
in the same data. Several of the metal-rich za
ze
systems have doublet
ratios implying partial coverage and thus, very likely, an intrinsic origin
(Wampler et al. 1993,
Petitjean et al.
1994).
The location of the other za
ze
absorbers is not known, but
Petitjean et al. (1994)
noted a marked change from [C/H]
-1 to
[C/H]
0 at a
blueshift of ~ 15,000 km s-1 relative to the emission
lines. If high abundances occur
only in intrinsic systems, then these results suggest that most
za
ze
NALs are intrinsic (see also
Möller et al.
1994).
More recent studies support these findings.
Petitjean & Srianand
(1999)
measured Z
Z
and
[N/C] > 0 in an intrinsic (partial-coverage) za
ze
absorber. For za
ze
systems of unknown origin,
Savage et al. (1998)
estimated roughly solar metallicities and
Tripp et al. (1997)
obtained [N/C]
0.1 and, very conservatively,
[C/H]
-0.8. (The
lower limit on [C/H] for the latter system
is -0.2 when more likely ionizing spectral shapes are used in the
calculations.)
Savaglio et al.
(1997) revised the metallicities downward slightly
from those in their 1994 paper to -1 < [C/H] < 0, based on better
data. Those systems are of special interest because of their high redshift
(za
4.1).
Wampler et al. (1996)
estimated Z ~ 2
Z
(based
on a tentative detection of OI
1303) for the only
other za
ze
systems studied so far at z > 4.
Hamann (1997),
Hamann et al. (1995,
1997b,
1997e, 1999b)
used the analysis outlined in Section 3.2
to determine metallicities or establish lower limits for several
za
ze
systems, including some mentioned above and some that are clearly
intrinsic by the indicators in Section 3.1.
The results generally confirm the
previous estimates and show further that, even when there are no
constraints on the ionization (for example, when only
Ly
and CIV
lines are measured), the column densities can still require Z
Z
. A
quick survey of those results suggests that bona fide intrinsic
systems and most others with Z
Z
have
[N/C]
0.0.
3.4.1. Uncertainties and Conclusions
Most of the NAL studies mentioned above would benefit from better data
(higher signal-to-noise ratios and higher spectral resolutions) and more
ionization constraints (wider wavelength coverage), but the frequent
result for Z
Z
is
convincing. Unlike the BALs, there are no obvious systematic effects
that might lead to higher abundance estimates for za
ze
systems compared with za <<
ze. The possibility of ionization-dependent coverage
fractions presents an uncertainty for those systems with partial
coverage, but we do not
expect that to cause systematic overestimates of the metallicities
(Section 3.2.2). We conclude that
many za
ze
NALs and, more importantly, all of the
confirmed intrinsic systems have Z
0.5
Z
and
usually Z
Z
. The
upper limits on Z are uncertain. The
largest estimate for a well-measured system is Z ~ 10
Z
(Petitjean et al.
1994), but
those data are also consistent with metallicities as low as solar
because of ionization uncertainties
(Hamann 1997).
There are mixed and confusing reports in the literature regarding
metal-to-metal abundance ratios, most notably N/C. In contrast
to Franceschini &
Gratton (1997), we find no
tendency for subsolar N/C in za
ze
systems. In fact, there is the general trend for stronger NV
absorption at za
ze
compared with za << ze
systems, and the most reliable abundance data suggest solar or higher
N/C ratios whenever Z
Z
.
The only serious problem is in interpreting the abundance results for
absorbers of unknown origin. High metallicities might correlate strongly
with absorption near QSOs, but the metallicities cannot define the
absorber's location. For example,
Tripp et al. (1996)
estimated Z
Z
and
[N/C]
0 for a
za
ze
system in which the lack of excited-state absorption in
CII*
1336 (compared with the
measured CII
1335)
implies that the density is low,
7
cm-3, and thus the distance from the QSO is large,
300 kpc. [The
relationship between density and
distance follows from the flux requirements for photoionization
(Section 2.5.1.)] Super-solar
metallicities at these large distances are surprising. At
300 kpc
from the QSO, we might
have expected very low intergalactic or halo-like abundances. The
solution might be that the absorbing gas was enriched much nearer the
QSO and then ejected
(Tripp et al. 1996).
Unfortunately, the excited-state lines used for density
and distance estimates are not generally available for
za
ze
systems (because they have low ionization energies, e.g.
CII* and SiII*). Of the six
za
ze
absorbers known to be far
(
10) from QSOs
based on these indicators, three of them clearly have
za > ze and are probably
not intrinsic for that reason
(Williams et al.
1975,
Williams & Weymann
1976,
Sargent et al. 1982,
Morris et al. 1986,
Barlow et al. 1997).
Only one has a metallicity estimate - the system with Z
Z
at
300 kpc distance
studied by
Tripp et al. (1996).