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 45:478-482 (1981)
© 1981 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Keren, R.
Right arrow Articles by Gast, R. G.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Keren, R.
Right arrow Articles by Gast, R. G.
Agricola
Right arrow Articles by Keren, R.
Right arrow Articles by Gast, R. G.

Effects of Wetting and Drying, and of Exchangeable Cations, on Boron Adsorption and Release by Montmorillonite1

R. Keren and R. G. Gast2

ABSTRACT

The effect of drying and rewetting sequences on boron adsorption and desorption by Na- and Ca-montmorillonite suspensions was determined with (i) nondried suspensions, (ii) suspensions dried prior to boron addition, and (iii) suspensions dried once or twice after boron adsorption. Boron adsorption in the nondried suspensions was completely reversible for both the Na- and Ca-systems. There was little effect of exchangeable cation species (Na+ vs. Ca2+) on boron adsorption in the pH values of 7.0 and 7.2. There was a significant exchangeable cation effect, however, at higher pH's, with the Ca-system adsorbing the greatest amount of boron. Boron adsorption on clays dried prior to boron addition was essentially the same for the nondried systems, indicating that the drying and rewetting sequence does not have any effect on the adsorption sites of the clay. The amount of boron adsorbed increased with drying and wetting after boron addition for both the Na- and Ca-systems, with the greatest increase occurring after the first drying-wetting cycle for both systems. Drying and rewetting of the clay suspensions after boron addition not only increased the amount of boron adsorbed, but significantly reduced the reversibility of the adsorption process as well. The relative amount of reversibility of adsorbed boron is a complex function of the drying and rewetting cycles, pH, and type of exchangeable cations.


NOTES

1 Contribution from the Institute of Soils and Water, Agricultural Research Organization. The Volcani Center, Bet Dagan, Israel. No. 230-E, 1980 series. This research was supported by a grant from the United States-Israel Binational Science Foundation (BSF), Jerusalem, Israel.

2 Soil Scientist, Institute of Soils and Water, ARO, The Volcani Center, Bet Dagan, Israel; and Professor and Head, Department of Agronomy, Univ. of Nebraska, Lincoln, respectively.

Received for publication October 7, 1980. Accepted for publication January 12, 1981.




This article has been cited by other articles:


Home page
Vadose Zone JHome page
P. J. Vaughan, P. J. Vaughan, and D. L. Suarez
Constant Capacitance Model Computation of Boron Speciation for Varying Soil Water Content
Vadose Zone J., May 1, 2003; 2(2): 253 - 258.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
A. Deyhle, A. J. Kopf, and G. Aloisi
Boron and boron isotopes as tracers for diagenetic reactions and depth of mobilization, using muds and authigenic carbonates from eastern Mediterranean mud volcanoes
Geological Society, London, Special Publications, January 1, 2003; 216(1): 491 - 503.
[Abstract] [PDF]




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 © 1981 by the Soil Science Society of America.