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ABSTRACT
Suspensions of bentonite clay saturated with varying Ca and K or Rb ratios and containing several concentrations of CaCl2 or KCl were membrane equilibrated with equal volumes of water. Activities and concentrations of Ca and K or Rb, and Cl ions in both suspension and dialyzate phases were determined with electrode and radioactive tracer techniques. The "suspension effect" (greater activity of cations and lesser activity of anions in the suspension than in the dialyzate phase) increased with increased K saturation (decreased Ca saturation) and with decreased electrolyte concentrations. Permanent charge cation exchange sites appeared to contribute most to the suspension effect, while the pH-dependent charges favored hydrolysis of the metallic cations and thus tended to mask the suspension effect.
A given concentration of electrolyte was many times more effective in causing changes in cation retention by the clay phase when the clay was predominantly saturated with Ca rather than with Rb. Higher retention of cations at high Rb saturations generally paralleled the electrode-measured activities and excised root uptake (corn and soybeans) of cations. Addition of 0.2 S of CaCl2 decreased the differences in cationic activities between phases and generally eliminated significant differences in uptake between phases.
1 Published with the permission of the Director of the Ohio Agr. Res. & Devel. Center as Journal Article no. 91-66. Presented in part before Div. S-2, Soil Science Society of America, Denver, Colo. Nov. 20, 1963, and Columbus, O. Nov. 4, 1965. Portions of the results appear in M.S. Theses presented by the two senior authors to the Graduate School, Ohio State University 1964 and 1965. This study was supported in part by a grant from the National Science Foundation.
2 Former Research Assistants, Professor, and Associate Professor, The Ohio State University and the Ohio Agr. Res. & Devel. Center.
Received for publication November 28, 1967. Accepted for publication March 5, 1968.
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