With the present STIS spectra of HE 0515-4414 the redshift range
has been covered for the first time at
sufficiently high resolution to undertake a sensitive search for
O VI absorbers. We have detected 6 O VI systems. Two
of them (z = 1.697, 1.736) are either associated with the QSO or
in the proximity zone of the extremely luminous QSO. The system z
= 1.416 is marginal, since only the 1031Å line is detected.
Including the latter, we have 4 detections in the range z = 1.21to 1.67 which yield a number density of O VI absorbers with
25mÅ of
.
Compared with the findings by Tripp et al. (2000) of
at
,
the number density at
is roughly a factor of 5 lower. Tripp et al.
(2000) compared their finding of a high number density of
weak O VI absorbers (
30 mÅ) in
H 1821+643 and PG 0953+415 with other classes of absorbers and
found that the weak O VI number density is more comparable
to that of the low z weak Ly
absorbers - which have
for
50mÅ - than to other types of metal absorbers like Mg II. In
HE 0515-4414 we have at least 42 Ly
systems (the exact
number being unknown due to the line blending problem) with
50mÅ in the range
which yields roughly
. Among these, roughly half of them are strong,
saturated Ly
lines with a detected Ly
line.
Again, while our STIS spectrum of HE 0515-4414 confirms the number
density of Ly
absorbers found previously (see Weymann et al.
1998), the number of O VI absorbers with
mÅ is lower than the number of Ly
absorbers
with
mÅ by a factor of 10. It is
noteworthy that, except the z = 1.674 system, O VI is
detected in lower column density Ly
absorbers (log
). Following the calculations by Tripp et al.
(2000) and earlier work by Storrie-Lombardi et al. (1996) and
Burles & Tytler (1996), the mean cosmological mass-density of
O VI absorbers can be written in units of the critical
density
as
![]() |
(3) |
Over the redshift interval z = 1.21 to z = 1.67 we have
for
q0 = 1/2.
is
(Table 1).
Assuming
,
following Tripp et al. (2000)
and Tripp & Savage (2000), which is close to the maximum for both
collisional ionization and photoionization, we obtain a lower
limit
(O VI)
.
The only reliably
measured heavy element abundances at
are from
DLAs. Typically the metal abundance (e.g. from Zn) is 1/10 solar
(Pettini et al. 1999; Vladilo et al. 2000). There is, however,
no guarantee that these abundances apply also to the O VI
absorbers among the low column density systems. Assuming 1/10
solar for the oxygen abundance, we have
.
With the same
assumptions Tripp et al. (2000) derived a value
.
Using a somewhat different formalism for
the derivation of
,
namely Eq. (6) from
Tripp & Savage (2000), we get with the same assumptions
(O VI)
.
Both from the number counts of the O VI
systems and the estimate of the mean O VI density the
unavoidable conclusion seems to be that at
,
the
baryon content of the O VI phase contains a factor of
less material than at
.
Copyright ESO 2001