1985
DOI: 10.1038/317027a0
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Chemical mechanisms of acid generation in the troposphere

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Cited by 558 publications
(359 citation statements)
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“…Therefore, H202 (or HOx) production appears to be still active in the autumn. The condition of {H202]<[S02} prior to the occurrence of fog is called Oxidant Limitation, in which a nonlinear relationship exists between the S02 concentration in air and the H2S04 produced in the aqueous phase (Calvert et al, 1985;Kleinman,1986;Meagher et al, 1990). Near the summit of Mt.…”
Section: Hydrogen Peroxidementioning
confidence: 99%
“…Therefore, H202 (or HOx) production appears to be still active in the autumn. The condition of {H202]<[S02} prior to the occurrence of fog is called Oxidant Limitation, in which a nonlinear relationship exists between the S02 concentration in air and the H2S04 produced in the aqueous phase (Calvert et al, 1985;Kleinman,1986;Meagher et al, 1990). Near the summit of Mt.…”
Section: Hydrogen Peroxidementioning
confidence: 99%
“…Ambient particulate sulfate levels, however, are not linearly related to SO 2 emissions, with less than a 1:1 reduction in sulfate concentration per reduction in SO 2 emissions (on a molar basis). 15,16 Also, since SO 2 sources are not uniformly distributed in space and time, nor have they undergone uniform emission reductions, not all areas would be expected to experience a uniform reduction in sulfate-related fine mass.…”
Section: Seasonal Trendsmentioning
confidence: 99%
“…Peroxides in atmospheric aqueous phases are of interest because of their role in dissolved SO 2 oxidation. Hydrogen peroxide is believed to be the dominant oxidant for SO 2 in atmospheric aqueous phases with pH b 5 (Calvert et al, 1985). Although the presence of organic peroxides is often considered, there have been only a few observations of aqueous phase organic peroxide levels in natural waters.…”
Section: Introductionmentioning
confidence: 99%