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ABSTRACT
Highly significant linear correlations were found to exist between radiotracer quantities of Rb86 and the K concentrations of the dialyzate phases of clay-water membrane equilibrium systems. The systems extended over a wide range of Ca/K saturation ratios, electrolyte concentrations, and pH values. The linear regression lines for bentonite, illite, kaolinite, and vermiculite systems had similar slopes. The actual amounts of K in the dialyzate phases were about 1.4 times the values indicated by the Rb tracer. Of the four clay minerals only the vermiculite presented problems because of specific fixation of K or Rb. Uptake of K42 by excised barley, corn, and soybean roots from bentonite systems was also significantly correlated with uptake of Rb86. It appeared that Rb86 could be used in tracer quantities to reflect relative changes in the K distribution in these systems.
1 Published with permission of the Director of the Ohio Agr. Exp. Station as Journal Artivle no. 41–64. Presented before Div. II Soil Science Society of America, Denver, Colo., Nov. 20, 1963. A portion of the results were used by the junior author in partial fulfillment of the requirements of the M.S. degree. The Ohio State University, 1964. This study was supported in part by a grant from the National Science Foundation.
2 Assistant Professor and Assistant Instructor, respectively, The Ohio State University and the Ohio Agr. Exp. Sta.
Received for publication November 30, 1964. Accepted for publication April 15, 1965.
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