Results 201 to 210 of about 129,587 (250)
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Soils: genesis and geomorphology
Choice Reviews Online, 2006Randall J. Schaetzl and Sharon Anderson. New York: Cambridge University Press, 2005. xiii and 817 pp., maps, diagrams, photos, refs, glossary, and index. $85.00 cloth (ISBN 0-521-81201-1).
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Soil genesis, soil classification and soil survey
Geoderma, 1970Abstract Mutual relationships exist between soil genesis, soil classification and soil survey. The first two subjects are dealt with separately. Some of the general lines in soil genetic investigation are traced. Next trends in soil classification are dealt with.
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Feedback processes in soil genesis
Geoderma, 1978Abstract Feedback can be defined as the returning of a part of the effects of a given process to its beginning or to a preceding stage so as to reinforce or modify that process. Feedback processes are self-accelerating because of continuous reinforcement of the causes starting them. Up to a certain moment, reinforcement is proportional to the effects
J. Torrent, W.D. Nettleton
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Mica Genesis in Hawaiian Soils
Soil Science Society of America Journal, 1968Abstract A soil mica having a formula Na 0.11 NH4 0.06 K 1–24 (Al, Si) (Al, Fe, Mg) O 20 (OH) 4 has been identified
T. C. Juang, G. Uehara
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Peat soils: Genesis and classification
Eurasian Soil Science, 2006This paper considers three topical problems—the definition of peat soils as natural-historical formations and the estimation of their profile thickness, the analysis of the genesis of organic soils, and the principles of the classification of peat soils.
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Surface-water gley soils in Bangladesh: Genesis
Geoderma, 1977Abstract Extensive areas of periodically wet, acid soils in Bangladesh have a seasonally fluctuating pH of the surface horizon and evidence for net clay loss. Morphological, chemical, mineralogical and other data mainly on a typical profile of these surface-water gley soils indicate a clay loss of some 1.5 kg/dm' ; alteration of smectite to a soil ...
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Soil landscape systems: A model of soil Genesis
Geoderma, 1975Abstract The paper describes a model of the soil system. There are two different, partly complementary means of building such a model. One approach is to construct, using empirical physical science methods, an isomorphic model, in which each and every component (variable) of the system is an element in the model. The other approach is to build, using
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