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Astron. Astrophys. 356, 23-32 (2000) 2. Observations of C IV (and Ly
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Fig. 1. An expanded plot of the Ly![]() ![]() ![]() ![]() |
With the objective of providing constraints on the abundances and
kinematics of the gas in 0943-242, sensitive high-resolution
spectroscopic observations centered at the C IV and
lines were performed at the Anglo
Australian Telescope (AAT) on 1995 March 31 and April 1 under
photometric conditions and with a seeing which varied from 1" to 2".
The RGO spectrograph was used with a 1200 grooves mm-1
grating and a Tektronix 10242 thinned CCD, yielding
projected pixel sizes of
Å. The
projected slit width was 1.3", resulting in a resolution as measured
from the copper-argon calibration spectrum of 1.5Å FWHM; the
slit was oriented at a position angle of 74o, i.e. along
the radio axis (as in RO95).
The total integration time of 25000s was split into
22000s and
7
3000s exposures in order to
facilitate removal of cosmic rays. Exposure times were chosen to
ensure that the background was dominated by shot noise from the sky
rather than CCD readout noise. Between observations the telescope was
moved, shifting the object slit by about 3 spatial pixels, so that for
each exposure the spectrum was recorded on a different region of the
detector. The individual spectra were flat-fielded and sky-subtracted
in a standard way using the long-slit package in the NOAO reduction
system IRAF. The precise offsets along the slit were determined using
the position of the peak of the spatial profile of the
C IV and
lines. Using
these offsets, the images were registered using linear interpolation
and summed to obtain the two-dimensional spectrum. The resultant
seeing in the final two-dimensional spectrum, measured from two stars
on the slit, was 1.5" FWHM. The corresponding FWHM of
C IV emission along the slit was 2.2", giving a
deconvolved (Gaussian) width of 1.6" or 12 kpc. Within the errors,
this is the same as that found for Ly
emission by RO95.
The two-dimensional spectrum was weighted summed over a 7 pixel (5") aperture to obtain a one-dimensional spectrum. In Fig. 2 we show the AAT data in the form of a full-resolution spectrum.
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Fig. 2. The full-resolution AAT spectrum showing the C IV ![]() ![]() |
One deep trough is observed in the
Ly emission line (Fig. 1) which
was interpreted as a large scale H I absorber by RO95.
In addition there are a number of weaker troughs, presumably due to
weak H I absorption. Fitting the emission line by a
Gaussian and the H I absorption by Voigt profiles, RO95
infer a column density
of
for the deep trough, a redshift
and a Doppler parameter b of
km s-1. For the three
shallow troughs, they find
ranging
from
to
and b ranging from 7 to 100 km s-1. The redshift
difference of the absorbers relative to systemic velocity when
converted into inflow/outflow velocities indicate values not exceeding
800 km s-1. Because at the bottom of the main trough no
emission is observed, the covering factor of the absorbing gas must be
equal or larger than unity over the complete area subtended by the
Ly
emission, indicating that the
spatial scale of the absorber exceeds 13 kpc. This work will concern
only the deep absorption trough.
To parameterize the C IV profile we have assumed that the underlying emission line is Gaussian, with Voigt profiles due to the C IV doublet absorption superimposed. We used an iterative scheme that minimizes the sum of the squares of the difference between the model and the observed spectrum, thereby solving for the parameters of the model (e.g. Webb 1987, v097). Initial values were assumed for the shape of the Gaussian profile and the redshift of the absorber.
In Fig. 3 we show a portion of the spectrum with the model
fits superimposed. The Gaussian fitted to the C IV
emission line peaks at and has a
FWHM of
Å. We have corrected
all wavelengths to the vacuum heliocentric system
(
+1.13 Å) before computing the
redshifts. The two troughs in this figure correspond to the
C IV
1548, 1551
doublet produced by the same absorption system. Therefore, within the
fitting procedure, the wavelength separation and the ratio of the two
profiles' depths are fixed by atomic physics while the two values for
b are set to be equal. The fit gives for the location of the
bottoms of the two troughs
6068.2
and 6078.3Å resulting in a redshift of 2.9202
0.0002. Within the errors this
redshift is equivalent to that of the main H I absorber
and in the subsequent analysis we will assume that the
Ly
and C IV
absorption gas belongs to the same absorber. We derive a
Doppler parameter b for the doublet of
km s-1 and a column
density
of
as summarized in Table 1.
![]() | Fig. 3. An expanded plot of the full-resolution spectrum with the fit superimposed (solid line). |
Table 1. Parameters for the Gaussian and Voigt profile fits
As expected, appears only in
emission without any absorption since it is not a resonance line.
Parameters for the
emission profile
were obtained by fitting a Gaussian using the same iterative scheme
(see Fig. 1 in Röttgering & Miley 1997). The peak is
positioned at
and has a FWHM of
Å. The fitted parameters of the
emission and absorption profiles are presented in Table 1. We
recall that the FWHM of the Ly
emission profile is
km s-1 (v097),
significantly larger than that of
(see Table 1). Inspection of the various profiles in Fig. 1
and Fig. 2 (or Fig. 3) suggests the presence of an excess
flux on the blue wings of all the emission profiles. Combining
information from all the emission lines, our best estimate of the
emission gas redshift is
.
To investigate whether there is any velocity shear in the
C IV emission profile we fitted spatial Gaussian
profiles to the emission line as a function of wavelength. In
Fig. 4 we show the wavelength maxima of these spatial profiles
and a line fitted through these points. The spatial profile of the
C IV emission spectrum is displaced by 0.2",
corresponding to a displacement of 1.5 kpc, over a wavelength range of
50Å. RO95 measured a comparable shift for
Ly of 1.8
kpc 2 although it
appears that the latter displacement is due to a far more pronounced
and abrupt difference in locations of the
Ly
peak on both sides of the
absorption trough. As Fig. 4 shows, the peaks of
C IV emission form a wavy line. We believe the velocity
shear in the CIV profile to be less significant than
the shear in the Ly
profile. We cannot
rule out that the small velocity shear might be masking a possible
break up of the absorption regions into a few saturated absorption
components of smaller b.
![]() | Fig. 4. The relative location of the peak of the C IV emission at constant wavelength as a function of wavelength. The line is a weighted fit to these peaks. The zero offset is arbitrary. |
A concern about the determination of
is the possibility that that there
exist subcomponents in the absorption systems that have high column
densities but low b values and are, therefore, not acounted for
whenever individual velocity subcomponents are not resolved. Although
we cannot strictly exclude this possibility, we adopt the stand of
Jenkins (1986) and Steidel (1990a) who, using extensive absorption
line studies, argue that this is unlikely to be the case, at least for
C IV , and that a single-component curve-of-growth
analysis can be used to infer total columns although the inferred
effective b value has no physival meaning in terms of
temperature. It is interesting to note that the physical conditions
inferred from the C IV fit are fully consistent with
the observed ratio of the doublet (since both troughs are equally well
fitted). If the underlying continuum was flat, the
column and the b value we
infer would imply a theoretical ratio of equivalent widths of
, which is where the curve of growth
just begins to leave the linear part (Steidel 1990a). Clearly the
column might be susceptible to a
larger error since Ly
is saturated.
With these caveats in mind, we will assume in the following analysis
that the adopted columns do not lie far off from reality.
© European Southern Observatory (ESO) 2000
Online publication: March 28, 2000
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