In this section, we describe the observed pairs of
quasars and list the absorption systems with
N(H I
cm-2 found in the 7
spectra. For each of the systems, we search the adjacent
line of sight for the presence of any absorption at the
same redshift. When a LLS or a C IV system with rest
equivalent width
Å is seen along the
second LOS within
1000 km s-1 from the former LLS,
we call this a coincidence.
The observed number densities of LLS and C IV absorption
systems with
Å are similar at
the same redshift (e.g. Steidel et al. 1988; Steidel 1990).
We can therefore assume that they trace the same kind of
overdensity.
The numbers associated with the coincidences correspond to those in Table 4 and Fig. 15.
These two QSOs (also called Q0307-195A,B) are separated
by 56 arcseconds on the plane of the sky, corresponding
to
kpc in the considered redshift
interval.
Spectra at low and intermediate resolution of this pair
have been used in the past to study the correlation of
C IV and Lyman-
forest lines (Shaver & Robertson 1983; D'Odorico et al. 1998).
1)
- there is no metal system along the LOS of UM680
corresponding to the sub-DLAS at
observed in the spectrum of UM681 (see Sect. 3.1). A weak
Lyman-
absorption,
H I
,
is observed at
(see
Fig. 1). From the observed number
density of H I Lyman-
absorption lines with column
density in the range
H I
(Kim et al. 2001), the probability for such an absorption to
fall in a velocity bin of 200 km s-1 at this redshift is
.
2)
- the coincident systems observed at
and
in the spectra
of UM680 and UM681 respectively, are two candidate LLSs
which show absorption lines due to the same ionic
transitions with a shift of
300 km s-1 (see
Fig. 5).
We detect low ionisation absorption lines due to
Al II, Si II and Fe II, together with Al III, Si III and Fe III, the latter only in UM680. The corresponding
Si IV and C IV absorption doublets are outside our
wavelength coverage, but their presence is discussed in
Shaver & Robertson (1983).
It is not possible to constrain the value of the H I column density of both systems due to the complexity of
the profile. The Lyman-
lines are in a region of the
spectrum with low signal-to-noise ratio and
probably blended.
From the equivalent width ratio of Si II and Fe II to C IV (as measured by Shaver & Robertson 1983) we derive
that the systems are likely in a low excitation state and
have N(H I
) > 1018 cm-2 (see Bergeron & Stasinska 1986).
3)
- the QSO UM681 presents a metal system at its emission
redshift (
)
with lines due to
C IV, N V, O VI and S IV and also weak
low ionisation lines (see Fig. 6).
This system, although characterized by highly ionised
transitions, has a velocity spread of less than
250 km s-1 and does not show any evidence of
partial coverage.
Furthermore, the presence of singly ionised absorption
lines and the symmetric velocity profile favour an
absorber with a dense core.
Therefore, although the system is located in the vicinity
of the quasar it is probably not associated with it.
In addition, there is a very similar absorption
system along the LOS of UM680, at
,
corresponding to a velocity
shift of
100 km s-1 (see Fig. 6).
The transverse spatial separation between the two LOSs at
this redshift is
kpc.
The latter system is located at
2000 km s-1 from the
emission redshift of UM680; the same arguments as before
are valid to reject the hypothesis that this is due to gas
associated with either of the two quasars.
The observed H I Lyman-
and Lyman-
absorption lines
for this system are consistently fitted with a main
component of column density
H I
.
Figure 7 shows the H I Lyman-
emission
region in the two QSO spectra.
The coinciding Lyman-
absorptions at
are shown, together with the associated N V
lines (the N V
transitions fall outside the observed wavelength range).
Another pair of Lyman-
absorptions is observed at
,
which shows an associated N V doublet in
the spectrum of UM680, while does not have any detected
associated metal line in UM681.
Shaver & Robertson (1983) suggest the existence of a uniform,
1 Mpc diameter, gaseous disk associated with UM681 to
explain the coincidence at
.
The
presence of a further coincidence at
2000 km s-1 from this one, favours the thesis that
the absorptions are due to a coherent gaseous
structure embedding both quasars and possibly small
galactic objects.
Deep imaging of the field could possibly shed light on
the nature of the absorbers and of the ionising processes
at work in the gas.
The first spectra of this QSO pair were presented by
Sargent et al. (1988), the two objects are separated by 5
arcmin on the plane of the sky, corresponding to a
transverse spatial separation of Mpc
in the considered redshift range.
The remarkable feature is the presence of
a DLAS in each of the LOS (see Sect. 3).
![]() |
Figure 8:
H I Lyman-![]() ![]() ![]() ![]() ![]() ![]() |
The emission redshift of Q2343+1232 reported by
Lu et al. (1998),
,
is consistent
with the position of the emission lines observed in the
Sargent et al. (1988) spectrum (Si IV+O IV] and C IV) and
with the O I emission in our spectrum (marked in
Fig. 8), when the shifted rest wavelengths
computed by Tytler & Fan (1992) are used.
Likely, the peak observed at
Å is
partly due to the N V emission, while the maximum of the
Lyman-
emission is strongly absorbed.
We identify two absorption systems at
:
a N V doublet and the corresponding Lyman-
absorption at
(
km s-1), together
with another possible Lyman-
line at
(
km s-1).
They do not show any signature of partial coverage and
they could be explained by the presence of a cluster
of galaxies of which the QSO itself is a member
(e.g. Weymann et al. 1979).
5)
- in the spectrum of Q2343+1232, the DLAS at
(see Sect. 4.2) coincides with a metal
system at
(redshift of the
Si IV main component) in the companion
LOS, showing only high ionisation lines (C IV was
detected by Sargent et al. 1988)
and a strongly saturated Lyman-
(
Å) (see Fig. 10).
The H I absorption is likely not a LLS
since singly ionised lines are not detected (like Mg II
and Fe II). An acceptable fit of the profile is
obtained with two main components at N(H I
and
cm-2, which however
should be considered as lower limits.
6)
- the DLAS at
in
the spectrum of Q2344+1228 (see Sect. 4.1) does not have a
corresponding metal system on the LOS to Q2343+1232, but
it is indeed at
940 km s-1 from the H I Lyman-
emission at the redshift of this quasar (see
Fig. 8).
The quasar Q2139-4434 (
)
was
observed at intermediate resolution together with its
companion Q2138-4427 (
)
by
Francis & Hewett (1993).
They are separated by
8 arcmin on the plane of the sky. Francis and
Hewett observed common strong Lyman-
absorptions at
and
and further imaging of the
field revealed the presence of a cluster of galaxies at
(Francis et al. 1996, 1997, 2001a).
Wolfe et al. (1995) confirmed the damped nature of the
system at
in the spectrum of Q2138-4427.
We obtained high resolution spectra of Q2138-4427,
Q2139-4434 and of Q2139-4433 (
,
R = 19.97; Hawkins & Véron 1996). The latter two
QSOs are separated by 1 arcmin on the plane of the sky.
7)
- the strong Lyman-
absorption at
in
the spectrum of Q2138-4427 has at least
one visible damped wing in the velocity profile (see
Fig. 11) implying a column density N(H I
cm-2.
Unfortunately, the spectra of Q2139-4433 and Q2139-4434
do not cover the wavelength region where the
corresponding H I Lyman-
lines should fall, while the
spectrum of Q2138-4427 does not cover
that of the C IV doublet at this redshift. In
the low resolution spectrum of Q2139-4434 by
Francis & Hewett (1993), an absorption line with equivalent
width
20 Å is present at this redshift, which
would correspond to a Lyman-
line with N(H I
cm-2.
We do not detect C IV absorption at this redshift in the
spectra of Q2139-4433 and Q2139-4434 but we identify
neutral and singly ionised transition lines (C II,
O I, Si II and Fe II) with a simple
two-component velocity profile in Q2139-4434.
Figure 12 shows two coincident transitions in
Q2138-4427 and Q2139-4434, they have a minimal velocity
separation of around 150 km s-1, while the two LOSs are at
a transverse separation of
Mpc.
8)
- the system at
in the spectrum
of Q2139-4434 is again a candidate LLS on the ground of
the observed ionic transitions. No metal lines are
detected within
3000 km s-1 of this absorption
redshift along the LOS of Q2139-4433 and of Q2138-4427.
On the other hand, the velocity profile of the observed
H I Lyman-
absorptions follows that of the
C IV absorption associated to the LLS (see
Fig. 13).
Unfortunately, we cannot disentagle the velocity
structure of the LLS Lyman-
absorption since our spectrum
does not extend to the region where the higher lines in
the Lyman series are located.
![]() |
Figure 14:
![]() ![]() ![]() ![]() ![]() |
9)
- the DLAS at
in the
spectrum of Q2138-4427 coincides with a complex H I Lyman-
absorption in the spectrum of Q2139-4434, with no
detectable associated metal transitions.
On the other hand, we identify a saturated
Lyman-
absorption (
Å) and a C IV doublet at
in the spectrum
of Q2139-4433 (see Fig. 14), partially
superposing in redshift upon the C IV absorption
associated to the DLAS.
The transverse spatial separation between the two LOSs at
this redshift is
Mpc.
This correlation could be interpreted as due to a gaseous
structure perpendicular to the LOSs and extending over
several Mpc in the direction defined by the three quasars.
Objects | Ident. | Redshifta |
![]() |
![]() |
log N(H I) |
![]() |
log N(Fe II) |
(h-1 Mpc) | (km s-1) | Å | |||||
1 | 1.7874 | 0.87 | 13.8 | out | <11.8 | ||
1.78865 | >3000 | 19.0 | out | 14.5 | |||
UM680 | 2 | 2.0352 | 0.92 | 300 | >18 | 0.4d | 12.8 |
UM681 | 2.03215 | >18 | 0.7d | 13.4 | |||
3 | 2.12312 | 0.94 | 100 (Si II) | >17.3 | 0.5 | <12.7 | |
2.12209 | >17.3 | 0.44 | <12.6 | ||||
4 | 2.17115 | 5 | >3000 | >17.3 | 0.34 | 13.1 | |
2.167 | <0.01 | <11.8 | |||||
Q2343+1232 | 5 | 2.43125 | 5.3 | 110 (Si IV) | 20.35 | 1.1e | 14.7 |
Q2344+1228 | 2.4271 | >15.9 | 0.7e | <12.5 | |||
6 | 2.549f | 5.3 | |||||
2.53788 | 20.4 | out | 14.1 | ||||
7 | out | 1 | <0.014 | <12.3 | |||
2.37977 | 9 | 150 (Fe II) | 20 | <0.008 | 13.4 | ||
2.38279 | 8 | >19 | out | e.w. 1.2h | |||
Q2139-4433 | 8 | 2.73258 | 16.5 | <0.03 | <12.9 | ||
Q2139-4434 | 2.73557 | >3000 | >17.3 | 0.6 | 13 | ||
Q2138-4427g | 2.7323 | <0.005 | <11.9 | ||||
9 | 2.85262 | 0 (C IV) | 0.5 | <13 | |||
2.85378 | 14.8 | <0.007 | <12.6 | ||||
2.85153 | 20.9 | 0.8 | e.w. 0.2h |
a The reported redshifts correspond to the main
component of the associated metal absorption, if present;
or to the strongest H I Lyman-![]() b Transverse spatial separation between the lines of sight; in the case of the triplet it refers to the distance to the following object in the list. c Minimal velocity separation between metal absorption lines of the same ionic species in the coupled lines of sight. d C IV ![]() e C IV ![]() f Emission redshift of the paired QSO. g Precise column density determination for the metal lines in the spectrum of Q2138-4427 will be reported by Ledoux et al. (in preparation). h Rest equivalent width in Å. |
Copyright ESO 2002