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 18:143-147 (1954)
© 1954 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 McLean, E. O.
Right arrow Articles by Baker, F. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by McLean, E. O.
Right arrow Articles by Baker, F. E.
Agricola
Right arrow Articles by McLean, E. O.
Right arrow Articles by Baker, F. E.

Cationic Activities as Indexes for Characterizing Five Arkansas Soils Occurring in the Southern Region1

E. O. McLean and F. E. Baker2

ABSTRACT

Five soils and 3 extracted colloidal materials were characterized by means of the clay membrane electrode technique for measuring ionic interactions. The study dealt with Lakeland loamy fine sand, Ruston sandy loam, Crowley silt loam, Houston clay, Sharkey clay soils and the <.2 µ clay, the <25 µ clay, and the crude humic acid fractions extracted from the Sharkey clay soil.

The characteristic curves resulting from the plotting of the fractions of K active at various K-Ca saturations of the soils and extracted materials were prepared. Comparison of these curves with those of the individual clay minerals made possible the characterization of the soils and the extracts with respect to which clay minerals appeared to predominate in them.

The results indicate that kaolinite clay dominates the regulation of cationic interactions in the Lakeland, Ruston,a nd Crowley soils. Beidellite appears to predominate in the Houston and Sharkey soils. Montmorillonite seems to play the major role in the < 25 µ clay from the Sharkey, but the beidellite evidently masks the effect of the montmorillonite in the < .2 µ clay and in the whole soil. The crude humic acid from the Sharkey gave no evidence of any appreciable effect upon the cationic interactions of the whole soil.


NOTES

1 Research paper No. 1104 Journal Series, University of Arkansas, Fayetteville, Ark. Published with the permission of the Director of the Ark. Agr. Exp. Sta. Presented before Division II, Soil Science Society of America, Dallas, Tex., Nov. 18, 1953. A major part of this work was submitted by the junior author in a thesis for a partial fulfillment of the requirements for the M.S. Degree in the Graduate School, University of Arkansas. This investigation was largely supported by the Mathieson Chemical Co., Inc., and this support is gratefully acknowledged.

2 Associate Professor and former Graduate Assistant, respectively.

Received for publication November 28, 1953.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1954 by the Soil Science Society of America.