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ABSTRACT
Water-dispersible clay in soils from a number of geographic locations increased in relation to clay measured by a standard procedure as the proportion of sand in the soils increased. Additions of sand to soils containing relatively small amounts of water-dispersible clay relative to "regular" clay markedly increased the yield of water-dispersible clay; medium sand and coarse sand were the most effective. Conversely, the removal of sand from soil containing large amounts of sand reduced the yield of water-dispersible clay. The abrasive action of sand during agitation associated with water dispersion evidently breaks down aggregates containing clay.
1 Contribution from the Soil Survey Lab., SCS, USDA, Lincoln, Nebr.; and the Dep. of Agron., Univ. of Nebraska, Lincoln 68508. Published as paper no. 3282, Journal Series, Nebr. Agr. Exp. Sta. Research reported was conducted under Project no. 12-11.
2 Soil Scientist, SCS, USDA, Colorado Springs, Colo.; Soil Scientist, Soil Survey Lab., SCS, USDA, Lincoln, Nebr.; and Professor of Agron., Univ. of Nebraska, respectively.
Received for publication January 4, 1972. Accepted for publication May 3, 1972.
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