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Titlebook: Stable Isotope Geochemistry; Jochen Hoefs Textbook 20096th edition Springer-Verlag Berlin Heidelberg 2009 Fractionation.Isotope properties

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书目名称Stable Isotope Geochemistry
编辑Jochen Hoefs
视频videohttp://file.papertrans.cn/876/875454/875454.mp4
概述Includes supplementary material:
图书封面Titlebook: Stable Isotope Geochemistry;  Jochen Hoefs Textbook 20096th edition Springer-Verlag Berlin Heidelberg 2009 Fractionation.Isotope properties
描述.Stable Isotope Geochemistry is an introduction to the use of stable isotopes in the geosciences. It is subdivided into three parts: theoretical and experimental principles; fractionation processes of light and heavy elements; the natural variations of geologically important reservoirs. Since the application of stable isotopes to earth sciences has grown in the last few years, a new edition appears necessary. Recent progress in analysing the rare isotopes of certain elements for instance allow the distinction between mass-dependent and mass-independent fractionations. Special emphasis has been given to the growing field of "heavy" elements. Many new references have been added, which will enable quick access to recent literature. For students and scientists alike the book will be a primary source of information with regard to how and where stable isotopes can be used to solve geological problems..
出版日期Textbook 20096th edition
关键词Fractionation; Isotope properties; Mechanisms; Natural variations; Stable isotopes; geochemistry; geoscien
版次6
doihttps://doi.org/10.1007/978-3-540-70708-0
isbn_softcover978-3-642-08960-2
isbn_ebook978-3-540-70708-0
copyrightSpringer-Verlag Berlin Heidelberg 2009
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ing their uptake, effects on plant functioning and detoxification mechanisms. The particular significance of glutathione S-transferases in bio-indication and bio-monitoring, and in the detoxification of volatile organic air pollutants and herbicides is evaluated, and their potential significance in
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Variations of Stable Isotope Ratios in Nature, system. A major difference between extraterrestrial and terrestrial materials is the existence of primordial isotopic heterogeneities in the early solar system. These heterogeneities are not observed on the Earth or on the Moon, because they have become obliterated during high-temperature processes
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ck access to recent literature. For students and scientists alike the book will be a primary source of information with regard to how and where stable isotopes can be used to solve geological problems..978-3-642-08960-2978-3-540-70708-0
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