As found previously (Hatchell et al. 1998a), the fractional abundances
of various sulphur-bearing species depend rather sensitively on
depletions, hot core "age'', and grain thermal history. The work
presented here shows that the abundance ratios of HCO/H2CO and
NS/CS seem particularly well suited to infer whether a shock has
passed through a hot core. However, they are probably useful in this
way only if freeze-out during the pre-stellar phase is not total.
It should be noted that we have made some rather strong assumptions
about the role of surface reactions in the chemistry of the hot
cores. We have assumed that hydrogenation of species to form saturated
hydrocarbons dominates on grain surfaces. In fact, the use of an
approach like that of Caselli et al. (1998) might well lead us to
conclude that the grain surface reactions lead to far richer surface
compositions than we have supposed. We have also assumed that the
shock is not powerful enough to destroy the refractory material. The
release of the latter, however, would not change the conclusion of
this study as the silicon released should not significantly affect the
NS/CS nor the HCO/H2CO ratios.
At a fractional abundance of 10-10, HCO is probably too
weak to be detectable other than in the (3 mm) ground state
transitions, even in Orion and Sgr-B2 (Turner 1989) but measurements
of the NS to CS abundance ratios in hot cores should be made. NS is
not a commonly observed species but detections of NS emission towards
a number of hot cores were reported by Hatchell et al. (1998b): their
observations of NS and CS give ratios close to
0.1. The hot
cores in their sample are believed to be all at the same evolutionary
stage as the authors did not find a large variation in their
chemistry. Also, McGonagle & Irvine (1997) reported an extensive
survey for nitrogen sulfide in Giant Molecular Clouds (GMC). They
found that its fractional abundance is of the order of few
10-10. In general, this is consistent with the estimates of our
models. Their estimate for the column density of NS is, however, too
uncertain to substantiate our conclusions that the CS/NS ratio could
be a good indicator of shocks in hot cores: their observations were
performed with spatial resolution of 86, 45 and 35 arcsec for
observations of NS
,
NS
and NS
respectively, and they conclude
that much higher spatial resolution observations of NS are indeed
needed. Comparisons should be made with high resolution
(interferometric) observations for a large sample of hot cores where a
resolution of about 1 arcsec (necessary even for the nearest hot core)
can be achieved. Indeed, the low rotational and excitation
temperatures deduced from their observations suggest that NS emission
arises from extended material of relatively modest density (
cm-3).
Acknowledgements
SV acknowledges the financial support of PPARC. DAW is grateful to PPARC for the award of a Senior Fellowship. PC acknowledges support from the ASI-grants ARS-98-116 and ARS-78-1999, and from the MURST research program "Dust and Molecules in Astrophysical Environments''. The authors thank A. G. Gibb and M. G. Hoare for useful discussions.
Copyright ESO 2001