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ABSTRACT
Ion-exchange chromatography was employed to study the effects of electrolyte imbibition by soils on their cation-exchange behavior. This was accomplished by study of the shape of effluent breakthrough curves from columns of Ca-saturated soils to which either Al+3 or K+ solutions were added. B-horizon samples of Cecil, Lloyd and Davidson, and the Ap horizon of a Yolo soil were employed in the study.
Comparison of experimental effluent curves with those predicted by the modified Walter equation showed a large discrepancy when anion interaction with soils was encountered. Anion distribution coefficients (Kd's) varied in the order Cl- = NO3- < SO4-2 < H2PO4- on a Ca-Lloyd soil. Only H2PO4- had a Kd above zero on the Yolo soil. Column "symmetry values" for Ca+2
K+ exchange were reduced as electrolyte imbibition by soils increased. Practical implications of these results are discussed.
1 A contribution from the Agronomy Department, Virginia Polytechnic Institute, Blacksburg. Presented before Div. II, Soil Science Society of America at Cincinnati, Ohio. Nov. 18, 1959.
2 Assistant Professor of Agronomy.
Received for publication January 8, 1960. Accepted for publication February 24, 1960.
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