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Title: Laboratory studies of free radical reactions in cloudwater

Conference ·
OSTI ID:7148125

Reactions in cloudwater can be important pathways for chemical transformation of atmospheric trace gases because of high solubility of reagent gases, rapid aqueous-phase kinetics, and large thermodynamic driving force. A key cloudwater reaction is oxidized of dissolved SO{sub 2} and H{sub 2}O{sub 2}. It is thus important to understand processes controlling H{sub 2}O{sub 2} formation in the atmosphere by gas- and aqueous-phase reactions of HO{sub 2} free radicals. A concern with models of free radical chemistry in cloudwater is that of the applicability of present chemical kinetic schemes to such complex milieus. This concern arises because, at the low free-radical concentrations expected for cloudwater, reactions of radicals with trace impurities are favored over radical-radical reactions, which dominate at high radical concentrations commonly employed in laboratory investigations. We report initial results of a study in which the rate of change in H{sub 2}O{sub 2} concentration is monitored in synthetic and authentic cloudwater in which HO{sub 2} radicals are produced by {sup 60}Co{gamma} radiolysis at rates comparable to those expected upon transfer of HO{sub 2} from interstitial cloud air to cloudwater. These results indicate that micromolar concentrations of Fe(III) decrease H{sub 2}O{sub 2} yields and can even lead to H{sub 2}O{sub 2} loss rather than formation. Implications on cloud chemistry will be discussed. 14 refs., 2 figs.

Research Organization:
Brookhaven National Lab., Upton, NY (USA)
Sponsoring Organization:
DOE/ER; National Science Foundation (NSF)
DOE Contract Number:
AC02-76CH00016
OSTI ID:
7148125
Report Number(s):
BNL-43551; CONF-900402-2; ON: DE90003961; CNN: ATM-8808480
Resource Relation:
Conference: 199. national meeting of the American Chemical Society, Boston, MA (USA), 22-27 Apr 1990
Country of Publication:
United States
Language:
English