From observations of sulphur-bearing and other molecular species and chemic
al models it has been established that elemental sulphur is roughly two ord
ers of magnitude more depleted in the detectable parts of such regions than
are elemental carbon, nitrogen and oxygen. It seems surprising that sulphu
r is so depleted but not entirely depleted. We suggest that the fact that m
uch of the sulphur is in S+ in translucent clumps with hydrogen number dens
ities of less than 10(3) cm(-3) plays a significant role in determining why
it is so depleted in denser sources. Ions collide more rapidly with grains
and may stick more efficiently to them than neutrals; so, as a clump colla
pses, sulphur may become depleted in it more rapidly than elements that are
not primarily ionized in translucent material. Eventually in the collapse,
gas-phase sulphur will become contained mostly in neutral species, which i
n our picture leads to a large decrease in its depletion rate and a remnant
gas-phase elemental fractional abundance high enough for sulphur-bearing s
pecies in dense cores to be detectable.