The disappearance rate of S2, which was produced from the pyrolysis of COS, was measured behind incident shock waves by monitoring the UV emission in the temperature range of 4500–6000 K and in the pressure range of 0.32–0.5 atm. It was found that two processes could possibly account for the disappearance of S2: S_2+Ar→2S+Ar\ ag3 and (Remark: Graphics omitted.) and the following rate equation was obtained: -d[S_2]/dt=k_II[S_2][Ar]mol cm^-3s^-1 where k_II=10^13.68exp(-77kcal/RT)cm^3mol^-1s^-1.
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Higashihara et al. (1980) studied this question.
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