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- W116984480 abstract "Abstract The argillic horizon is considered genetically to be an illuvial horizon in which layer-lattice silicate clays have accumulated by illuviation to a significant extent. With micromorphological methods it is possible to demonstrate the process of clay illuviation unequivocally by the presence of argillans, at least in soils of low (to medium) COLE values. Selected Benchmark soils in semiarid parts of South India, developed from saprolitically weathered granitic gneiss have a >20% higher clay content in the B horizon than in the ochric A horizon and a base saturation of >35%, therefore they are classified as (Rhod)Ustalfs. Micromorphological investigations, however, show satisfactory evidence of clay illuviation only in two cases, in the other soils argillans can be seen only in very small amounts; often they are absent. Clay mineralogical investigations indicate that the maximum of clay formation -mainly of kaolinites, illites are less dominant -especially in the Therefore we propose defining Alfisols as soils with significant clay formation expressed by an increase in clay of >10% from the C to the B horizon. According to this definition they can easily be separated from the Inceptisols and even the Brown Forest Soil of higher weathering intensity in the mid-latitudes would fit into this concept of Alfisols. The argillic horizon in its genetic sense should be used on the Great Group level." @default.
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- W116984480 date "1990-01-01" @default.
- W116984480 modified "2023-09-27" @default.
- W116984480 title "Clay Illuviation in Semiarid-Tropical (Sat) Alfisols? A First Approach to a New Concept" @default.
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- W116984480 doi "https://doi.org/10.1016/s0166-2481(08)70328-3" @default.
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