Abstract
The oxidation of hydrogen sulfide in shock waves has been studied over the temperature range 1350°—2450°K by following the characteristic absorption of OH and SO2. Two different regions are apparent: below 1560°K the OH and SO2 appear together, after an induction period, while above 1700°K the SO2 appears before the OH. The oxidation at low temperatures is interpreted in terms of a branching‐chain mechanism involving the reactions: SH+O2SO+OH,OH+H2SH2O+SH,SO+O2SO2+O,O+H2SOH+SH. At higher temperatures, participation of the reaction O+H2SSO+H2 provides an additional route for the formation of SO2 and hence leads to a reduced induction time for its appearance.
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