I. Barnes et al., THE TROPOSPHERIC OXIDATION OF DIMETHYL SULFIDE - A NEW SOURCE OF CARBONYL SULFIDE, Geophysical research letters, 21(22), 1994, pp. 2389-2392
In laboratory investigations of the gas-phase OH initiated oxidation o
f dimethyl sulfide (DMS: CH3SCH3) at room temperature the formation of
SO2, dimethyl sulfoxide (DMSO: CH3SOCH3), and OCS have been observed.
A yield of 0.7 +/- 0.2 % S was measured for OCS. These new results re
present a hitherto unknown and quite considerable in situ atmospheric
source of OCS. Based on the global DMS source strength as given in the
literature and provided that the results from the laboratory study ar
e valid under atmospheric conditions we estimate a contribution in the
range 0.10 to 0.28 Tg (OCS) yr-1 from the gas-phase atmospheric photo
oxidation of DMS to the global OCS budget.