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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Mingle

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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LINE

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

Merited

companion

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.

Serenity

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.

hazard

充氣女

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).

MOAN

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