Atmospheric hydrogen peroxide: Does it share a role with ozone in degrading air quality?

Numerous investigations regarding atmospheric H{sub 2}O{sub 2} have been conducted during the 1980s; nevertheless, the distribution pattern of H{sub 2}O{sub 2} and its formation, decomposition, and deposition processes still are not clearly understood. In this article, the authors summarize previous...

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Bibliographic Details
Published inEnvironmental science & technology Vol. 24; no. 10; pp. 1452 - 1462
Main Authors Sakugawa, H. (University of California, Los Angeles, CA), Kaplan, I.R, Tsai, W, Cohen, Y
Format Journal Article
LanguageEnglish
Published Washington, DC American Chemical Society 01.10.1990
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Summary:Numerous investigations regarding atmospheric H{sub 2}O{sub 2} have been conducted during the 1980s; nevertheless, the distribution pattern of H{sub 2}O{sub 2} and its formation, decomposition, and deposition processes still are not clearly understood. In this article, the authors summarize previous investigators' findings concerning the levels of H{sub 2}O{sub 2} in the gas and aqueous phases at various locations in the world. They also review and evaluate previous studies on factors affecting the formation of gaseous H{sub 2}O{sub 2}. Additionally, they review studies on the decomposition and deposition of atmospheric H{sub 2}O{sub 2}, including its gas-phase and aqueous-phase reactions, to evaluate the role of H{sub 2}O{sub 2} as an oxidizer of sulfur dioxide (SO{sub 2}) in the atmosphere. Finally, they suggest that although H{sub 2}O{sub 2} may be the dominant oxidant of atmospheric SO{sub 2} to sulfate, the limited amount of field data currently available on the temporal and geographic concentration and distribution of H{sub 2}O{sub 2} hinders the identification of major factors affecting the formation of atmospheric H{sub 2}O{sub 2}.
Bibliography:T01
9102627
ISSN:0013-936X
1520-5851
DOI:10.1021/es00080a002