Abstract
IN the modern study of soils, there is an urgent need for methods of analysis which will express quantitatively the fundamental properties and genetic relationships of the material examined. We are venturing to suggest a provisional method whereby an approximate estimate may be obtained of the extent to which chemical weathering has proceeded in a given soil.
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ROBINSON, G., RICHARDSON, M. Degree of Weathering of Soils. Nature 129, 581–582 (1932). https://doi.org/10.1038/129581b0
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DOI: https://doi.org/10.1038/129581b0
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