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

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Die elektroerosive Bearbeitung,f some stratified water bodies. Organic matter is here decomposed mainly by microorganisms which release metabolic products containing carbon, nitrogen, and sulfur. Among the gaseous products considered here are CH., NH., N.O, NO, H.S, (CH.) SH, (CH.).S, CS., OCS, and H.. As most of these trace gase
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https://doi.org/10.1007/978-3-322-90446-1act selectively with certain neutral trace gases, and thus in situ ion composition measurements can be used as a powerful tool for trace gas detection. This analytical application of atmospheric ions has attracted great interest and already provided a wealth of new information on trace gases and aer
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https://doi.org/10.1007/978-3-322-90446-1l troposphere are reviewed briefly. Many important gas phase reactions are common to both the troposphere and the stratosphere. However, because of the substantially different chemical compositions and physical conditions between the two spheres, there exist numerous gas phase oxidation processes wh
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https://doi.org/10.1007/978-3-322-90446-1 OH concentrations in the absence of radical scavenging by aerosol particles in the atmosphere. The other solution provides excellent descriptions of the observed CFCl., CF.Cl. distributions, good approximations of the ozone observations, and a very good agreement with the global observations of CH.
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https://doi.org/10.1007/978-3-322-83339-6n scale, gases such as oxygen are vital to sustaining animal respiration, whilst at the other end, trace species such as nitrogen oxides control fundamental geochemical phenomena such as the earth’s ozone shield and the level of hydroxyl radicals present in the troposphere. The most numerous trace g
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https://doi.org/10.1007/978-3-642-68638-2atmosphärische Chemie; chemistry; air pollution and air quality
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