Titlebook: Interactions at the Soil Colloid; Soil Solution Interf G. H. Bolt,M. F. Boodt,E. B. A. Strooper Book 1991 Springer Science+Business Media D

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The Electrified Interface of the Soil Solid Phaseolid surface with a discussion of the effects of possible lateral heterogeneities of such surfaces. In soil there are several reasons for the presence of such heterogeneities. These include the diversity of the materials of the soil solid phase, the presence of different faces on the crystalline con

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Surface Complexation at (Hydr)Oxide Surfacess with hydrogen- and hydroxide ions, with metal ions (Lewis to the (hydr)oxide-water interface. It leads to an accumulation of matter at the interface without the development of a three dimensional molecular structure (Sposito, 1986). This step is usually considered to be fast and reversible. It is

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Adsorption of Heavy Metals by Clay-Aluminum Hydroxide Complexesllinity from the ‘model (hydr)oxides’ used frequently in laboratory studies. They may occur as discrete particles, having hardly any contact with the clay surface, and as coatings on, or as interlayers between clay mineral surfaces. Jenne (1968) suggested that the reactivity of hydroxide coatings wo

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Micronutrient Adsorption by Soils and Soil Colloids that are considered essential for the growth and reproduction of plants and/or animals. Over the past decade, a great deal of attention has been directed towards problems of soil pollution involving the accumulation in soils of excess levels both of some of the essential micronutrients and some of

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Interactions between Small Organic Chemicals and Soil Colloidal Constituentsds, insects, and plant diseases, and for regulating plant growth. These may be applied directly to the soil as sprays, or incorporated in the soil as solids or vapors, or they may enter the soil as canopy drip from spray applications to crops. In the ideal system the soil applied chemical would be h

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Interactions between Organic Macromolecules and Soil Inorganic Colloids and Soilsen returned to the soil since agriculture began in order to improve soil ‘tilth’ and to aid crop growth. To be effective, these amendments require transformations by soil organisms, and products formed or transformed during microbial metabolism are well positioned to interact with the soil inorganic

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Complexation of Metal Ions by Humic Substances: Fundamental Considerationsnd toxicity of these ions. For those and other reasons, humic substances have been investigated by soil scientists for many years (Stevenson, 1982; Saar and Weber, 1982; Sposito, 1986; Weber, 1988). In more recent years, as the importance of humic substances to processes in other environments was re