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Titlebook: Heterogeneous Processes of Geochemical Migration; V. S. Golubev,A. A. Garibyants Book 1971 Consultants Bureau, New York 1971 biology.chemi

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發(fā)表于 2025-3-21 19:36:49 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Heterogeneous Processes of Geochemical Migration
編輯V. S. Golubev,A. A. Garibyants
視頻videohttp://file.papertrans.cn/427/426009/426009.mp4
圖書(shū)封面Titlebook: Heterogeneous Processes of Geochemical Migration;  V. S. Golubev,A. A. Garibyants Book 1971 Consultants Bureau, New York 1971 biology.chemi
描述The problem of the geochemical migration of elements has received wide attention in the works of V. I. Vernadskii and A. E. Fersman [1, 2J. Vernadskii considered geochemistry to be the science of the history of chemical elements on the earth, their distribution and move- ments in space and time, and their genetic relations [IJ. Geochemical migration was defined by Fersman as "the movement of chemical elements in the earth‘s crust leading to their dissemination or concentration. " The views of Vernadskii and Fersman on the migration of elements have received added support and development in connection with successes in physics, chemistry, biology, and other sciences. According to Fersman, the earth is looked upon as a cosmic body, characterized by common origin and Similarity of composition with the sun, the planets, meteorites, and other bodies of the solar system. The scale and trend of geochemical migration of elements in the earth are determined by the initial state of terrestrial matter, its thermal history, and the scale of time. The rules of elemental migration are determined by internal and exterual fac- tors. Fersman distinguishes five groups of internal factors, i. e.
出版日期Book 1971
關(guān)鍵詞biology; chemistry; development; distribution; geochemistry; history; migration; solar system
版次1
doihttps://doi.org/10.1007/978-1-4684-1587-2
isbn_softcover978-1-4684-1589-6
isbn_ebook978-1-4684-1587-2
copyrightConsultants Bureau, New York 1971
The information of publication is updating

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Diffusion in Rocks,ogeneous processes of geochemical migration. In the following chapters we shall examine the effect of diffusion on the range of geochemical migration (Chaps. 2, 6, and 7) and on the rate of interaction between the dissolved substance and the rock (Chaps. 4 and 5).
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The Kinetics of Adsorption, Ion Exchange, and Chemical Reactions of Solutions and Gases with Rocks,action processes (adsorption, ion exchange, and chemical reactions) of the substances with rocks under certain initial and boundary conditions. Consequently, the interaction rate of solutions and gases with the rocks determines the laws of geochemical migration (Chaps. 6 and 7). This makes it import
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e, un choque de culturas milenarias, de una parte la aborigen y de otra la cristiana que venía de Europa. Tal choque fue, al mismo tiempo, una fusión de culturas, la una dentro de la otra conforme a un proceso que ha durado más de cuatrocientos a?os.
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V. S. Golubev,A. A. Garibyants major cause of mortality in Great Britain. What are described as socially induced disorders are taking their place. The increase in lung cancer, much of it almost certainly due to cigarette smoking is an example, but accidents, drug addiction and suicide are also taking an increasing toll, especial
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V. S. Golubev,A. A. GaribyantsNational Cancer Institute for 1973–76 [1], the incidence of Cancer in the United States has increased by 1.3% annually since the previous survey for 1969–71. Among the major sites of cancer the incidence of Cancer of the breast, colon, rectum, uterine corpus and lung increased while the incidence of
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