In the case of the obvious outflow sources, NGC 2071 and Orion A, a broad
Gaussian component has been subtracted from the line profile map. This is
examplified in Fig. 9 for the centre positions. In the centre
position of Orion A we fitted three Gaussian components to the SO line profile,
a broad outflow, the hot core, and a quiescent cloud component. We obtained
essentially the same result as Friberg ([1984]) although he
used an additional component to describe the quiescent component. In positions
adjacent to the centre position both the outflow and hot core components were
removed. In the other positions, further off the centre, only a weak broad
outflow component was removed when visible. The hot core component cannot be
discerned in the CS spectrum (Fig. 9). Total and residual integrated
intensity maps are shown for both sources in Figs. 4 and
8, respectively. These two sources were the only ones where we
found prominent kinematical evidences of outflow activity in their SO and CS
line profiles. In several other sources, e.g. G34.3+0.2, NGC 2264IR, and
NGC 7538, there are
The main isotopomer data will be used in Paper II to derive SO/CS integrated intensity ratio maps. To be able to estimate eventual SO/CS abundance ratio variations we then have observed the 34SO(32-21) and C34S(2-1) lines in critical positions i.e. where the SO/CS integrated intensity ratio is very high or very low. Since the SO/CS abundance ratio is estimated from the rare isotopomers we can avoid, to a large extent, effects from optical depths and possible outflows. The observed SO, 34SO, CS and C34S spectra are shown in Figs. 10-14 and the corresponding integrated intensities are given in Table 2. In Figs. 10-14 the C34S and 34SO spectra have been multiplied with a factor 5. In the cases of NGC 2071 and Orion A the residual integrated intensity is tabulated in Table 2.
In order to check the consistency of the data further we have used those
entries in Table 2, for which we have reliable detections in all four
isotopomers, to plot the integrated intensity ratio
as function of the ratio
,
see
Fig. 15. Here we see a clear correlation between the two ratios (as
would be expected). Also shown in Fig. 15 (as dotted lines) are limits
for SO/CS abundance ratios in the range 0.25 to 4.5. All data points, but one,
fall in the region spanned by this range if we allow the ratios to vary within
their
errors. The error estimation of the ratios is discussed
thoroughly in Paper II (Sect. 2.1) in conjunction with the ratio maps. The
limits have been calculated assuming a 32S/34S ratio of 22 (Wilson &
Rood [1994]) and that the SO optical depth is a factor of
three lower than the optical depth of the CS line if the SO and CS abundances
are equal (due to the threefold spin multiplicity of SO, see Paper II).
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