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Titlebook: Chemistry of the Unpolluted and Polluted Troposphere; Proceedings of the N H. W. Georgii,W. Jaeschke Conference proceedings 1982 D. Reidel

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Henric Bagerius,Christine Ekholstan example a common model on residence time is developed and discussed in its results. The residence time connects the content of a reservoir (size distribution for aerosols) with its source strength or removal rate. This is presented for the aerosol. In addition other physical properties of the tro
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https://doi.org/10.1007/978-3-319-31283-5described. A brief quantitative description of scavenging rate coefficients and washout ratios is given. For dry deposition, the mechanisms are described and the meteorological, surface and constituent properties which affect deposition are identified. A theoretical description of dry deposition of
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Nato Science Series C:http://image.papertrans.cn/c/image/224885.jpg
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Conference proceedings 1982l Protection of the University of Frankfurt, FRG, conducted the NATO Advanced Study Institute because of the rapidly increased interest in the problems of air chemistry and air pollution. This development has contributed in recent years to a significant expansion of knowledge in the field of atmosph
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Synthesis of Pyrrolo[l,2-,]quinoxalines,an made, totaled (40 ± 20) x 1O. g N yr .. Its geographical distribution is also estimated. Existing measurements provide a vertical profile of NO. for continental midlatitudes; it appears to be dominated by anthropogenic sources.
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Sulfur Emissions from Volcanoesy a small fraction of this amount, namely 1.0 x 10. t/a, is emitted during eruptions, while the major part, namely 1.42 x 10. t/a, is contributed by non-eruptive activity. The average global emission of volcanic H.S and SO.2- is found to be around 10. t/a and 10. t/a, respectively. From these estima
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