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Oxidation of Atmospheric SO2 by Products of the Ozone–Olefin Reaction

Abstract

OZONE is the most abundant oxidant in the troposphere and is generated in the stratosphere by the reaction of oxygen atoms, formed by photolysis, with molecular oxygen. Some is then transferred to the troposphere and 0–0.05 p.p.m. of ozone is found in unpolluted air at ground level1. Ozone can also be formed directly in tropospheric polluted air by the photolysis of NO2 in the presence of hydrocarbons; concentrations in excess of 0.15 p.p.m. are regularly recorded in Los Angeles2 and other cities of the United States. Significant increases in equivalent ozone concentrations over background levels have been recorded in Holland3—up to 0.10 p.p.m. in conditions suitable for the build up of photochemical oxidants. The ambient sulphur dioxide level was found to vary inversely with equivalent ozone level.

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COX, R., PENKETT, S. Oxidation of Atmospheric SO2 by Products of the Ozone–Olefin Reaction. Nature 230, 321–322 (1971). https://doi.org/10.1038/230321a0

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