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- W2062012010 abstract "Using the acid-resistant residue of soil fine earth as internal standard, the redistribution and losses of SiO2, Al2O3, MgO, K2O, Na2O, and TiO2 were determined for an upland developmental sequence of five profiles on Silurian scree. The mobilization of Al, Fe, and Mg was related to chlorite breakdown. Of these constituents Fe began to be released at an early stage of weathering whereas A1 release lagged behind Fe and Mg; although substantial amounts of Fe and A1 were mobilized in highly weathered horizons. Subsequently, whereas mobilized Fe was almost completely redeposited in illuvial horizons, little of the mobilized A1 was retained by the soils. Amounts of Fe and A1 extracted by 0.1M potassium pyrophosphate were compared with redistribution computed using the internal standard. The concentrations in drainage water of soil constituents mobilized during pedogenesis were estimated and compared with measured concentrations in stream water draining the catchment." @default.
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- W2062012010 date "1975-09-01" @default.
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- W2062012010 title "QUANTITATIVE PEDOLOGICAL STUDIES ON SOILS DERIVED FROM SILURIAN MUDSTONES" @default.
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- W2062012010 doi "https://doi.org/10.1111/j.1365-2389.1975.tb01957.x" @default.
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