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- W2046802686 abstract "Continental chemical weathering is discussed with reference to a diagram, in which the ratio (CaO + Na2O + K2O)/(Al2O3+ CaO + Na2O + K2O) is plotted against the ratio (SiO2+ CaO + Na2O + K2O)/(Al2O3+ SiO2+ Na2O + K2O). The former ratio is a measure of the degree of feldspar breakdown, which is accompanied by the formation of secondary minerals (illite, smectite, etc.). The second ratio is a measure of the enrichment during weathering of Al, Si oxide phases such as kaolinite, quartz and gibbsite. The application of the diagram to a series of global examples leads to the statement: 1) Chemical weathering is the principal process by which continental surfaces are modified. 2) The extent of chemical weathering is correlated with the age of continental surfaces. 3) Global agricultural productivity is correlated with geologically recent additions of fresh rock debris by processes of volcanism, glaciation or alluviation." @default.
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- W2046802686 date "1981-09-01" @default.
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- W2046802686 title "QUANTIFICATION OF WEATHERING, SOIL GEOCHEMISTRY AND SOIL FERTILITY" @default.
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- W2046802686 doi "https://doi.org/10.1111/j.1365-2389.1981.tb01721.x" @default.
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