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Titlebook: Geochemistry of Organic Matter in the Ocean; Evgenii A. Romankevich Book 1984 Springer-Verlag Berlin Heidelberg 1984 Matter.Ocean.chemistr

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书目名称Geochemistry of Organic Matter in the Ocean
编辑Evgenii A. Romankevich
视频video
图书封面Titlebook: Geochemistry of Organic Matter in the Ocean;  Evgenii A. Romankevich Book 1984 Springer-Verlag Berlin Heidelberg 1984 Matter.Ocean.chemistr
描述My work Geochemistry oj organic matter in the ocean first appeared in Russian in 1978. Since then much progress has been made in the exploration of various forms of organic matter in the ocean: dissolved, colloidal, organic matter sus­ pended in particles and that contained in bottom sediments and in interstitial waters. The appropriate evidence is found in hundreds of articles and several re­ view works, such as Andersen (1977), Biogeochimie de [a matiere organique a [‘interjace eau-sedimentmarine (1980), Duursma and Dawson (1981). A great amount of new information has been obtained in the Soviet Union‘s scientific institutions on the composition and distribution in natural waters and bottom sediments of organic matter and its separate components playing a crucial role in the formation of the chemical and biological structure of the ocean and its productivity, in the biogeochemistry of the elements and geochemistry of organic matter in the Earth‘s sedimentary cover. The areas of exploration have expanded over the past four-and-a-half years to embrace many new, little-known regions, including the Arctic seas. In contrast to the three preceeding decades, the research has been focuse
出版日期Book 1984
关键词Matter; Ocean; chemistry; geochemistry; marine
版次1
doihttps://doi.org/10.1007/978-3-642-49964-7
isbn_softcover978-3-642-49966-1
isbn_ebook978-3-642-49964-7
copyrightSpringer-Verlag Berlin Heidelberg 1984
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978-3-642-49966-1Springer-Verlag Berlin Heidelberg 1984
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International Human Resource Management,tate in the ocean waters, and in the sediments. Inorganic and organic forms of these elements are the most essential biogenic constituents of ocean waters, and being functionally involved in the processes of living organisms, are subjected to a rapid turnover.
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Nitrogen and Phosphorus in the Process of Sedimentogenesis,tate in the ocean waters, and in the sediments. Inorganic and organic forms of these elements are the most essential biogenic constituents of ocean waters, and being functionally involved in the processes of living organisms, are subjected to a rapid turnover.
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Carbon of Dissolved Organic Matter in the Ocean,ve analysis, OM is classified at present in the majority of works only as dissolved and particulate (suspended). Definition of the term “dissolved organic matter” (DOM) means distinguishing between these two arbitrarily identified forms of organic compounds in natural waters. No uniform opinion prev
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Carbon of Particulate Organic Matter,in the filters with 0.45 – 1 µm pore size or in separators. Large OM particles in natural waters are present in an extremely scattered state and are usually not to be found in filtration particulate suspensates. Their quantity in the ocean, compared to the bulk of OM is insignificant, but they play
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