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Title: Chemical conversions in clouds

Conference ·
OSTI ID:5257497

Clouds constitute an extreme atmospheric aerosol in terms of particle size and condensed-phase mass. The large amount of liquid water in clouds as well as the high state of dispersion make clouds a potentially important medium for atmospheric reactions, depending upon thermochemical driving force and chemical kinetics of particular reactions. This paper presents the formalism for evaluating the rates of in-cloud reactions making use of laboratory-determined physical-chemical properties and assumed or measured reagent concentrations and other situational variables. Accurate description of these rates is sensitive to the mass-accommodation coefficient ..cap alpha.. (fraction of gas kinetic collisions at the air-water interface effective in transfering gaseous species to cloud droplets) if ..cap alpha..< 0.01. Little information pertinent to ..cap alpha.. is available for relevant solute gases. Attention is directed to reaction of SO/sub 2/ and NO/sub 2/ to form sulfuric and nitric acids, respectively, and to reactions involving oxidants (O/sub 3/, H/sub 2/O/sub 2/) and free radicals (HO, HO/sub 2/). Important in-cloud reactions identified include aqueous-phase oxidation of SO/sub 2/ by H/sub 2/O/sub 2/ and O/sub 3/ and gas-phase oxidation of NO/sub 2/ by O/sub 3/ followed by uptake of N/sub 2/O/sub 5/ or NO/sub 3/ by cloudwater. 141 refs., 8 figs., 5 tabs.

Research Organization:
Brookhaven National Lab., Upton, NY (USA)
DOE Contract Number:
AC02-76CH00016
OSTI ID:
5257497
Report Number(s):
BNL-36923; CONF-8505106-1; ON: DE86000033
Resource Relation:
Conference: 2. US-Dutch international symposium on aerosols, Williamsburg, VA, USA, 19 May 1985
Country of Publication:
United States
Language:
English