Abstract: The amount of moisture in a soil and its orientation to individual soil particles may be influenced by small additions of organic cationic compounds. Clay particles adsorb these cations, and because of their hydrophobic nature a waterproofing effect occurs. Thermodynamic considerations are presented to explain the strength retention of treated soils.
Clays and Clay Minerals; 1960 v. 9; no. 1; p. 585-591; DOI: 10.1346/CCMN.1960.0090143
© 1960, The Clay Minerals Society
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