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- W2000402901 abstract "Abstract The micropedological approach to the study of soils has made considerable progress recently. It provides a basis for investigation of the processes of soil formation (10, 12, 1, 3, 4, 2). From micromorphological studies KUBIENA (11) came to the conclusion that soil formation probably started with the formation of a “braunlehm” (brownloam) fabric. Depending on climatic differences, characteristic changes might take place in the braunlehm fabric, which led to the development of different kind of soils. According to this hypothesis tropical soils should also be considered as transformation products of the braunlehm. Crystallization of iron oxide as goethite and haematite microcrystals in the braunlehm fabric would lead to “rotlehm” , redloam) or non-lateritic red earth formation, whereas formation of coarse crystal aggregates of goethite and haematite was considered characteristic of laterization processes." @default.
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- W2000402901 date "1967-03-01" @default.
- W2000402901 modified "2023-09-26" @default.
- W2000402901 title "On the taxonomic value of soil fabric formation in red tropical soils" @default.
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- W2000402901 doi "https://doi.org/10.1080/00380768.1967.10431974" @default.
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