Astron. Astrophys. 342, 395-407 (1999)
3. Continuum definition and emission lines in the UV
First of all the UV data of HS 1103+6416 were corrected for
interstellar reddening according to Seaton's law (1979) with
corresponding to
N(H I )=1.03 1020 cm-2
(Reimers et al. 1995b). This value is from the Stark HI survey (Stark
et al. 1992)
We searched for regions in the data apparently free of absorption
lines, where we calculated the mean flux and the error of the mean
flux to check for consistency with the noise. The continua were then
constructed by fitting cubic splines to the sample of mean flux
values.
The data show one strong and one weak Lyman edge at
and 1800 Å, respectively (see
Fig. 1). Due to blending of the highest Lyman series lines the
continuum flux level is poorly defined at these edges and we manually
modified the continuum in these regions. By modelling the Lyman edge
and H I absorption lines calculating Voigt profiles for
the first 39 Lyman series lines we find
log N(H I )=17.46 cm-2 and
km -1 for the LLS at
and log N(H I
)=16.6 cm-2 and
km s-1 for the LLS at
, respectively.
![[FIGURE]](img23.gif) |
Fig. 1.
Observed fluxes in 10-15 erg s-1 cm-2 Å-1 of HS1103+6416 obtained with the FOS and GHRS onboard the HST. Data have been rebinned for presentation purposes only.
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The decrease in flux at Å
and Å cannot be explained
by further Lyman edges since the corresponding Lyman series lines are
missing.
Since there is a large time gap between FOS and GHRS observations
(8 months) we cannot decide if the observed flux increase at
Å is intrinsic to the QSO
continuum or due to flux variations of the QSO. In the fitted
continuum broad emission at Å
is apparent which might be due to Ne VIII 774 and/or
N IV 765 and/or O IV 788.
3.1. Spectral energy distribution
Ultraviolet spectra of QSOs are
still strongly influenced by absorption of intervening absorbers. In
order to find the intrinsic spectral energy distribution of the QSOs
corrections have to be applied to the observed data. First, the
dereddened spectra were corrected for continuum absorption by neutral
hydrogen in the identified LLSs.
Corrected fluxes were transferred to luminosities using
![[EQUATION]](img30.gif)
for q (Weedman 1986) and
H km s-1 Mpc-1.
Fig. 2 shows the spectral energy distributions
log versus frequency in the rest
frame of HS 1103+6416.
![[FIGURE]](img44.gif) |
Fig. 2.
Spectral energy distributions log versus frequency in the rest frame of HS 1103+6416. Optical data were obtained at the Calar Alto 2.2 m telesope. In the UV the continua derived for the dereddened spectra were corrected for the neutral hydrogen continuum absorption of the LLSs and transferred to luminosities adopting q and H km s- 1 Mpc-1. An additional correction for the cumulative hydrogen continuum absorption of the numerous Ly clouds with log N(H I ) cm-2 leads to higher luminosities and to changes in the continuum slopes (dotted lines).
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Monte Carlo simulations were performed in order to estimate the
depression of the quasar spectrum due to the cumulative hydrogen
continuum absorption by the numerous
Ly clouds. The incidence of LLSs, i.e.
absorber clouds with neutral hydrogen column densities greater than
log N(H I
) cm-2, is easily detected
by their Lyman edges. Thus only clouds with
log N(H I
) cm-2 are considered.
The distribution in redshift and column density of
Ly clouds can be described by
![[EQUATION]](img48.gif)
We chose A ,
and
for
Ly clouds with
H I
) (see e.g. Madau 1995 and references
therein). Most absorption from Ly
lines occurs at column densities of
log N(HI) = 14. Five thousand simulations were performed to calculate
the mean transmission exp( ) at the
observed wavelengths with given
by
![[EQUATION]](img56.gif)
and
![[EQUATION]](img57.gif)
for Å. This additional
correction leads to higher luminosities and - even more important - to
changes in the continuum slope (see dotted lines in Fig. 2).
In contrast to HS 1307+4617 and HS 1700+6416 the continuum shape of
HS 1103+6416 is much flatter in the optical, but steeper in the
ultraviolet range (see Reimers et al. 1998) and compatible to the
common assumption of for
Å.
© European Southern Observatory (ESO) 1999
Online publication: February 22, 1999
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