Clay migration in upland soils of Malaysia
Clay movement was studied in a large number of well‐drained soils from Peninsular Malaysia, with a kaolinite mineralogy and an udic or perudic moisture regime. Dispersion in subsoils was found to be related to the net charge on the clay, while in topsoils it was virtually independent of charge or we...
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| Format: | Article |
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British Society of Soil Science
1984
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| Online Access: | http://psasir.upm.edu.my/id/eprint/118792/ |