SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 32:795-798 (1968)
© 1968 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Dolcater, D. L.
Right arrow Articles by Jackson, M. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Dolcater, D. L.
Right arrow Articles by Jackson, M. L.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Dolcater, D. L.
Right arrow Articles by Jackson, M. L.

Cation Exchange Selectivity of Some Clay-Sized Minerals and Soil Materials1

D. L. Dolcater, E. G. Lotse, J. K. Syers and M. L. Jackson2

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.


NOTES

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.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1968 by the Soil Science Society of America.