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Titlebook: Origin and Mineralogy of Clays; Clays and the Enviro Bruce Velde Book 1995 Springer-Verlag Berlin Heidelberg 1995 Clays.Erden.Erosion.Sedim

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发表于 2025-3-21 19:25:02 | 显示全部楼层 |阅读模式
书目名称Origin and Mineralogy of Clays
副标题Clays and the Enviro
编辑Bruce Velde
视频video
图书封面Titlebook: Origin and Mineralogy of Clays; Clays and the Enviro Bruce Velde Book 1995 Springer-Verlag Berlin Heidelberg 1995 Clays.Erden.Erosion.Sedim
描述.Origin and Mineralogy of Clays., the first of two volumes, lays the groundwork for a thorough study of clays in the environment. The second volume will deal with environmental interaction. Going from soils to sediments to diagenesis and hydrothermal alteration, the book covers the whole spectrum of clays. The chapters on surface environments are of great relevance in regard to environmental problems in soils, rivers and lake-ocean situations, showing the greatest interaction between living species and the chemicals in their habitat. The book is of interest to scientists and students working on environmental issues.
出版日期Book 1995
关键词Clays; Erden; Erosion; Sediment; Sedimentation; Ton; Umwelt; diagenesis; environment; mineralogy; soil
版次1
doihttps://doi.org/10.1007/978-3-662-12648-6
isbn_softcover978-3-642-08195-8
isbn_ebook978-3-662-12648-6
copyrightSpringer-Verlag Berlin Heidelberg 1995
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发表于 2025-3-21 23:04:11 | 显示全部楼层
Erosion, Sedimentation and Sedimentary Origin of Clays,ut a third of the Earth’s surface (Fig. 4.1). Similarly, although proportionally much smaller in area, continental aquatic environments are often dominated by fine-grained sediments, and these environments include many of the rivers, lakes, deltas and estuaries used extensively by man.
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ations, showing the greatest interaction between living species and the chemicals in their habitat. The book is of interest to scientists and students working on environmental issues.978-3-642-08195-8978-3-662-12648-6
发表于 2025-3-22 11:24:50 | 显示全部楼层
发表于 2025-3-22 14:49:55 | 显示全部楼层
Origin of Clays by Rock Weathering and Soil Formation,a homogeneous process. As a consequence, it is possible to model chemical transfers and clay-mineral stability fields using calculation codes. On the other extreme, the intimate dissolution-recrystallization mechanisms at the fluid-mineral interface scale are studied on isolated pure crystals in order to simplify the chemical system.
发表于 2025-3-22 20:12:52 | 显示全部楼层
Compaction and Diagenesis,ow ones, and in fact the Earth is hotter inside than at its skin (i.e. the solid gas interface known as the Earth’s surface). So as sediments get buried in basins, or on the edges in continents, they get hotter.
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Formation of Clay Minerals in Hydrothermal Environments,eralogical changes which occur on the scale of a rock or rock mass are considered to have been dealt with in the preceding chapter. The exact process of change via local, vein-influenced exchange processes is ignored for simplicity (see Chap. 6).
发表于 2025-3-23 06:42:09 | 显示全部楼层
volume will deal with environmental interaction. Going from soils to sediments to diagenesis and hydrothermal alteration, the book covers the whole spectrum of clays. The chapters on surface environments are of great relevance in regard to environmental problems in soils, rivers and lake-ocean situ
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