Titlebook: Atmospheric Chemistry; Report of the Dahlem E. D. Goldberg Conference proceedings 1982 Springer-Verlag Berlin Heidelberg 1982 atmosphärisch

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Some Influences of the Atmospheric Water Cycle on the Removal of Atmospheric Trace Constituents,Research needed to solve practical precipitation-scavenging problems is outlined. Topics are organized, in the main, into three space scales (local, regional, and global), two time scales (acute and chronic), and separately for particles and gases.

averse

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The Production and Fate of Reduced Volatile Species from Oxic Environments,The oxic part of the biosphere includes the surface, the top soil, and the upper regions of lakes and oceans. It is the site of a surprisingly large proportion of the total biosynthesis of reduced molecular species. The production under oxic conditions of reduced compounds of the principal groups of elements used by the biota is discussed.

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Allgemeiner Teil: Fungi und Fungizideientific revolution of the eighteenth century. Lavoisier, the father of modern chemistry, was well aware of the involvement of atmospheric gases in respiration. Oxygen was the intake gas and carbon dioxide the evolved gas in processes occurring at the surface of the earth. Still, up to the last seve

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https://doi.org/10.1007/978-3-662-11797-2ase neutralizing capacity. For acidic rain observed at most locations, H.SO., HNO., NH., and CaCO. are dominant components. Their local availability or production rates govern net acidity. pH is thus almost entirely determined by these major “strong” components imposed on a CO. background, with some

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anarchist

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https://doi.org/10.1007/978-3-663-04844-2hen their various microfossil and chemical components are analyzed in concert and when stratigraphic sequences are dated by appropriate methods. The peat of raised bogs in some respects is superior as a stratigraphic record of atmospheric composition, for it is not influenced by slope wash from the

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