The Mineralogy, Chemistry, and Physics of Tropical Soils With Variable Charge Clays
The Mineralogy, Chemistry, and Physics of Tropical Soils With Variable Charge Clays
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含可变电荷粘土的热带土壤的矿物学、化学和物理学
DOI：
10.1029/eo064i010p00099-03
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发表时间：
1983
期刊：
影响因子：
--
通讯作者：
D. R. Nielsen
中科院分区：
文献类型：
--
作者：
D. Cassel;D. R. Nielsen
这本书是1974年开始的一项努力的高潮，当时这位资深作者开始为他在北卡罗来纳州立大学休假期间教授的一门热带土壤课程收集信息。这本书付印时，全书引用的文献都是最新的。
土壤系统包含具有恒定或永久表面电荷的矿物和有机材料，例如蒙脱石，或恒定的表面电位，通常被称为可变电荷材料。大多数土壤系统都包含这两种类型。在热带地区，大多数具有永久电荷的矿物都已被严重风化。因此，剩余物质的表面电荷是由势能决定离子的吸附造成的。本书介绍可变电荷矿物和土壤有机质的矿物学、化学和物理学。
This book is the culmination of an effort started in 1974 when the senior author started assembling information for a tropical soils course that he taught while on sabbatical leave at North Carolina State University. The literature cited throughout the book was current when the book went to press.
Soil systems contain mineral and organic materials that have constant or permanent surface charges, such as montmorillonite, or constant surface potentials, usually referred to as variable charge materials. Most soil systems contain some of both kinds. In the tropics, most of the minerals with permanent charge have been severely weathered. Consequently, the surface charge of the remaining material results from adsorption of potential determining ions. This book treats the mineralogy, chemistry, and physics of the variable charge minerals and soil organic matter.