Titlebook: Acid Deposition at High Elevation Sites; M. H. Unsworth,D. Fowler Book 1988 Kluwer Academic Publishers 1988 Acid rain.Aerosol.Atmospheric

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Springer Series in Chemical Physicsrom the free troposphere may reduce the lifetime of individual droplets to values considerably below that of the cloud and may introduce extra oxidant which may substantially increase the sulphate production. A new model of cloud microphysics and chemistry in a growing cumulus cloud is presented to quantify the magnitude of this effect.

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https://doi.org/10.1007/978-3-642-96614-9 peroxide concentration..The second order rate constants for the reaction H.O. + HSO.. in cloudwater, derived from the decay of H.O. ranged from 4.2 × 10. to 1.84 × 10. 1 mol. s. for a pH range of 4.0 − 4.5.

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Transport Phenomena in Gaseous Systems,5) respectively. In spring 1986 the daily median fog pH on Mt. Tremblant was 4.0 (mean 4.0) and the precipitation pH 4.5 (mean 4.4). The NO../SO.. equivalents ratios in the spring fog water and precipitation were in the 0.4 to 0.5 range with concentrations of NO.. and SO.. enhanced by a factor of 5 to 10 in the fog water.

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Acid Deposition at High Elevation Sites978-94-009-3079-7Series ISSN 1389-2185

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https://doi.org/10.1007/978-94-009-3079-7Acid rain; Aerosol; Atmospheric chemistry; Cloud; Fog; Precipitation; Rain; Scale; Snow; Troposphere; Wind; eco