By P. M. Huang (auth.), B. A. Stewart (eds.)
Advances in Soil technology is a evaluate sequence suitable to all parts of soil technology. those stories, meant essentially for scientists, academics, and scholars of soil technology, additionally supply technical heritage details for plenty of extra staff and teams attracted to our common assets and man's impact on them. this is often the 8th quantity within the sequence with a global record of members from the USA, India, Canada and New Zealand. It comprises 4 overview chapters at the following matters: components affecting aluminum variations in soil; soil productiveness in dryland areas of constructing international locations; alterations in soil constitution below assorted cropping structures; houses and administration of the depleted soils of India. those contributions current precious info on a range of themes and function a superb resource of references.
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Additional info for Advances in Soil Science
1962). Hydroxy-interlayered smectite and vermiculite occur in soils as a product of weathering reactions. These minerals may result from degradation of chlorite or deposition of hydroxy materials in the interlayers of expansible phyllosilicates. 4-nm soil mineral that has properties similar to chlorite at room temperature. O-nm d-spacing when the mineral was heated. M. Huang do not fit the properties of either chlorite or vermiculite and smectite. Geographical distribution of this type of minerals is wide.
0 nm (Figure 16a). 0 nm, respectively. 03 (Figure 16b), which are characterized by the predominance of disordered products with low SiO ziAl z0 3 ratios and pseudoboehmite. 03 shows the presence of a gellike material (Figure 16c). 02 are composed of gellike materials, very distorted imago lite tubes, and hollow spherules (Figure 16e). 0 in the absence of citric acid. 0 nm in the TEM (Figure 17a) and IR spectra of the products (Figure 1Sd) reveal that the noncrystalline aggregates observed in the TEM mainly consist of allophane.
0, citric acid/AI molar ratio of O. 1. 3. Scale bar = 50 nm (Inoue and Huang, 1985; reprinted with permission of Clay Minerals Society). M. ) Figure 18. Relationship between Si0 2 /AI 20 3 molar ratios and organic carbon content of precipitates formed from solutions containing hydroxy Al ions, orthosilicic acid, and humic substances (Inoue and Huang, 1987; reprinted with permission of Clay Minerals Society). 01 /-Lm) products (Inoue and Huang, 1986). Chemical composition, size, number, and nature of the functional groups and concentration of organic ligands have a bearing on the perturbation of the formation of short-range ordered aluminosilicates.
Advances in Soil Science by P. M. Huang (auth.), B. A. Stewart (eds.)