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ABSTRACT
Selectivity coefficients for Pb2+, Cd2+, and Ca2+ exchange adsorption with montmorillonite, illite, and kaolinite clays were determined over a wide range of clay surface concentration and found constant. The average selectivity coefficients describing the ion distributions for montmorillonite, illite, and kaolinite, respectively, were 0.60, 0.44, 0.34 for Pb-Ca exchange, 1.04, 1.01, 0.89 for Cd-Ca exchange and 0.58, 0.56, 0.31 for Pb-Cd exchange. Whereas Cd2+ may compete more or less on an even basis with Ca2+ for clay adsorption sites, the adsorption of Pb2+ would be favored by a factor of 2 or 3 over Ca2+.
Key Words: cation adsorption heavy metals cation exchange
1 Supported in part with funds from the Illinois Agr. Exp. Sta. and NSF RANN Grant GI-31605.
2 Research Associate and Professor, Dep. of Agronomy, University of Illinois, Urbana 61801. Present address, Dow Coming, Midland, Mich.; Associate Dean and Director, Idaho Agr. Exp. Sta., Univ. of Idaho, Moscow, 83843, respectively.
Received for publication July 13, 1973.
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