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Low-intensity radiolysis study of free-radical reactions in cloudwater: H sub 2 O sub 2 production and destruction. [Gamma radiation]

Journal Article · · Environmental Science and Technology; (United States)
DOI:https://doi.org/10.1021/es00016a027· OSTI ID:5156344
;  [1]
  1. Brookhaven National Lab., Upton, NY (United States)
Reactions in cloudwater can be important pathways for chemical transformation of atmospheric trace gases. One such reaction is the oxidation of dissolved sulfur dioxide by hydrogen peroxide. H{sub 2}O{sub 2} is formed by the disproportionation of hydroperoxyl and superoxide radicals, O{sub 2}({minus}I). The authors report measurements of the rate of H{sub 2}O{sub 2} production from O{sub 2}({minus}I) radicals generated by low-intensity cobalt-60 radiolysis of synthetic cloudwater solutions and actual precipitation samples. The authors results, employing O{sub 2}({minus}I) production rates comparable to those expected upon transfer of HO{sub 2} from interstitial cloud air to cloudwater, confirm model predictions that H{sub 2}O{sub 2} production if frequently the major fate of O{sub 2}({minus}I) radicals. However, there is evidence of significant reaction between S(IV) and O{sub 2}({minus}I), with a rate coefficient of (3 {plus minus} 2) {times} 10{sup 4} at pH 4.96. In addition, the presence of 1 {mu}M dissolved iron decreases the H{sub 2}O{sub 2} yield, principally because of destruction of H{sub 2}O{sub 2} by Fe(II).
DOE Contract Number:
AC02-76CH00016
OSTI ID:
5156344
Journal Information:
Environmental Science and Technology; (United States), Journal Name: Environmental Science and Technology; (United States) Vol. 25:4; ISSN ESTHA; ISSN 0013-936X
Country of Publication:
United States
Language:
English

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