Titlebook: Environmental Geochemistry; A Holistic Approach John A. C. Fortescue Book 1980 Springer-Verlag New York Inc. 1980 Geochemie.Umwelt.biospher

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Hans-Ernst Schwiete,Bikash Dasgupta major and lasting contribution to the then infant science of geochemistry was made by the American geochemist F. W. Clarke (1847–1934) who collected, classified, and synthesized this information in his classic book ., originally published in 1908. So well did he complete his task that the book went

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,Problemstellung und Versuchsdurchführung,roach to the study of environmental geochemistry has two component parts: one, which is common to all studies of the geochemistry of the environment, is called its philosophical base; the other, which deals with the concepts and principles of the subject, is called its discipline. This chapter outli

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https://doi.org/10.1007/978-3-662-42312-7uring the past twenty years the study of the geochemistry of the environment has become of major concern to the scientific community as a whole. For example, the chapter entitled “Objectives and History of Geochemistry” in the introductory text by Wedepohl (1971) includes no reference to environment

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https://doi.org/10.1007/978-3-662-29581-6ntil now the tendency, outside Russia, has been to stress the study of absolute mobility of elements in landscapes. But in Russia, ever since the pioneer studies of Polynov (1937), both kinds of mobility have been considered by landscape geochemists. Consequently, as the study of environmental geoch

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Einleitung und Problemstellung, to the study of the circulation of elements in landscapes. More recently Kozlovskiy (1972) provided a series of conceptual models and principles, from the viewpoint of theoretical landscape geochemistry, that together summarize neatly the principal flow patterns of elements in landscapes. His paper

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https://doi.org/10.1007/978-3-662-24847-8 plant cover types or in response to some environmental factor; in soil science the concept is often used in relation to relief or natural drainage. Two kinds of gradient are commonly distinguished: (1) continuous gradients within which the rate of change is gradual and relatively uniform; and (2) d

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