Abstract

The reaction of IO radicals with dimethyl sulfide was studied using cavity ring-down laser spectroscopy. The reaction rate constant shows both a temperature and pressure dependence. At 100 Torr total pressure, the reaction has reached its high-pressure limit and has a rate constant of (2.5 ± 0.2) × 10-13 molecule-1 cm3 s-1 at 298 K. On the basis of the Arrhenius plot in the region of 273−312 K, the reaction has a negative activation energy (Ea = −18.5 ± 3.8 kJ mol-1). The atmospheric implications of these findings are discussed. In light of these new data, DMS oxidation by IO can compete with oxidation by the hydroxyl radical in the marine boundary layer. Quoted uncertainties are one standard deviation from regression analysis.

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