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 18:259-264 (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 Ensminger, L. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Ensminger, L. E.
Agricola
Right arrow Articles by Ensminger, L. E.

Some Factors Affecting the Adsorption of Sulfate by Alabama Soils1

L. E. Ensminger2

ABSTRACT

The sulfate content of a number of Alabama Soils was determined by extracting with various solutions. The sulfate extracted was measured turbidimetrically. Some factors affecting the adsorption of sulfate by soils were studied.

About the same amount of sulfate was extracted by neutral sodium acetate solution, sodium acetate buffered at pH 4.8, KH2PO4 solution containing 100 ppm. phosphorus, and KH2PO4 solution containing 500 ppm. phosphorus. However, 0.1 N HCl solution extracted little or no sulfate. The samples contained only small quantities of water-soluble sulfate except where sulfate had been recently applied.

The results show that sulfate is retained to a certain extent by most soils. The subsurface layers usually contain more sulfate and are capable of adsorbing more sulfate than the surface layers. The surface layers of most of the light textured soils did not contain sulfate or show a capacity to adsorb sulfate from solution.

The capacity of soils to adsorb sulfate is affected by certain soil treatments. Increasing amounts of superphosphate applied to a Cecil sandy clay loam resulted in decreasing amounts of soluble sulfate. The data show that superphosphate decreased the capacity of this soil to adsorb sulfate from a CaSO4 solution. Liming also resulted in a decrease in the retention of sulfate.

The sulfate adsorption capacity of a number of materials was determined in an attempt to show what fractions of soils may be responsible for the retention of sulfate. The data show that dehydrated Al2O3 adsorbed much more sulfate than any of the other materials. The iron minerals adsorbed rather small amounts of the sulfate while the Davidson colloid, kaolinite, and bauxite were intermediate.


NOTES

1 Contribution from the Department of Agronomy and Soils, Agr. Exp. Sta. of the Alabama Polytechnic Institute, Auburn, Ala. Published with the approval of the Director. The work was supported in part by funds made available on a contractual basis by the Soils and Fertilizer Branch, Agricultural Relations Division, Tennessee Valley Authority. Presented before Div. II. Soil Science Society of America, Dallas, Tex., Nov. 18, 1953.

2 Soil Chemist.

Received for publication December 27, 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.