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ABSTRACT
Cation exchange selectivity (CES) values for montmorillonite, vermiculite, biotite, muscovite, and micaceous vermiculitic clays from Triangle and Harpster soils were determined by equilibration of each exchanger with a mixed, equinormal solution containing two competing cations. The cation affinity of Na-saturated materials increased in the order K < Mg < Ca < Sr < Ba for montmorillonite and the soil clays, Mg < K < Ca < Sr < Ba for biotite, Mg < Ca < Sr < K < Ba for muscovite, and K < Ba < Sr < Ca < Mg for vermiculite. Sodium-saturated micaceous vermiculite gave a K/Ca CES value of 0.2, whereas K-saturated, dried vermiculite gave a K/Ca CES value of 0.4, indicating that the large number of interlayer wedge sites produced by the structural collapse in K-saturated and dried vermiculite increased the selectivity for K ions. Potassium-saturated and dried muscovite having a CEC equal to the similarly treated vermiculite gave a K/Ca CES value of 4.0 compared to 0.4 for the vermiculite, suggesting that layer charge density has a large influence upon K selectivity. The higher CES values for muscovite relative to those for biotite are explained by the smaller ditrigonal holes and the oblique orientation of hydroxyl groups in the muscovite structure.
1 Contribution from the Department of Soil Science, University of Wisonsin, through an International Consortium for Interinstitutional Cooperation in the Advancement of Learning (ICICAL). Supported in part by the Division of Biology and Medicine, Environmental Sciences Branch, US Atomic Energy Commission Contract AT(11-1)-1515-Jackson (paper COO-1515-15). Presented before Div. S-2, Soil Science Society of America, Nov. 6, 1967, at Washington, D.C.
2 Research Assistant; Associate Professor, Department of Plant and Soil Sciences, University of Maine, Orono (formerly Project Associate); Project Associate; and Professor.
Received for publication March 28, 1968. Accepted for publication June 27, 1968.
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