Abstract
Although most of chemical processes constituting an atmospheric chemistry system consist of gas phase reactions, there are some phenomena in which multiphase processes play an important role. In the stratosphere, chemical reactions on polar stratospheric clouds (PSC) are the most prominent example, and are of essential importance in the formation of the “ozone hole”. In the troposphere, historically multiphase reactions in clouds and fog have long been investigated being related to acid rain. Surface reactions on sea salt in the marine boundary layer have been studied related to tropospheric halogen chemistry. The heterogeneous reactions of HO2 radicals and nitrogeneous compounds on aerosols have been studied related to tropospheric ozone chemistry. In such processes uptake of atmospheric molecules on the solid and liquid surface, heterogeneous reactions on the surface, bulk reactions in aqueous phase, etc. are important. In this chapter, uptake coefficients of atmospheric species on water droplet, sea salt and alkali halides, soil dust and mineral particle, and soot as important surfaces for tropospheric heterogeneous processes, and reactive uptake on PSC, liquid phase chemistry of oxides of sulfur are described.
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Akimoto, H. (2016). Heterogeneous Reactions in the Atmosphere and Uptake Coefficients. In: Atmospheric Reaction Chemistry. Springer Atmospheric Sciences. Springer, Tokyo. https://doi.org/10.1007/978-4-431-55870-5_6
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