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 47:448-454 (1983)
© 1983 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 Kim, Y. K.
Right arrow Articles by Hatfield, J. D.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Kim, Y. K.
Right arrow Articles by Hatfield, J. D.
Agricola
Right arrow Articles by Kim, Y. K.
Right arrow Articles by Hatfield, J. D.

Fixation Kinetics in Potassium-Aluminum-Orthophosphate Systems1

Y. K. Kim2, E. L. Gurney3 and J. D. Hatfield3

ABSTRACT

The rate of removal of phosphate and potassium from solution was studied by contacting an aluminum-impregnated, cation exchange resin with solutions of monopotassium phosphate in concentrations of 0.05 to 0.25M and with atomic ratios Al:P from 0.25 to 4.0. The removal of both K and P from solution followed first-order reaction models for all experimental conditions, the K being removed faster than the P. The rate constants for K and P removal increased as the ratio Al:P increased, but were affected to a lesser extent by the initial concentration of KH2PO4. The concentration of Al with time agreed with a consecutive first-order reaction model involving cation exchange and precipitation. The rate constants for each experimental condition were evaluated by nonlinear regression analysis, and the reaction model represents the data well. The precipitate (prepared in 0.25 or 1M KH2PO4 solution) was identified as potassium aluminum taranakite by chemical and x-ray analysis. The phosphate retained in the resin was negligibly small and perhaps was occluded in the beads. Phosphate was removed from solution by the precipitation of taranakite. The taranakite precipitation rate constant, k4, varied directly with the atomic ratio Al:P and inversely with the initial KH2PO4 concentration, Co, by the correlation k4 = 1.09 (Al:P)1.066 (Co)-0.401.


NOTES

1 Contribution from the Division of Chemical Development, National Fertilizer Development Center, Tennessee Valley Authority, Muscle Shoals, AL 35660.

2 Research Chemist.

3 Retired Research Chemists.

Received for publication June 25, 1982. Accepted for publication December 15, 1982.







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 © 1983 by the Soil Science Society of America.