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 48:671-676 (1984)
© 1984 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 Korentajer, L.
Right arrow Articles by Hellums, D. T.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Korentajer, L.
Right arrow Articles by Hellums, D. T.
Agricola
Right arrow Articles by Korentajer, L.
Right arrow Articles by Hellums, D. T.

Leaching Losses and Plant Recovery from Various Sulfur Fertilizers1

Leonid Korentajer, Bernard H. Byrnes and Deborah T. Hellums2

ABSTRACT

Two greenhouse experiments were conducted with soils fertilized with various S fertilizers. The soils were subjected to percolation during early growth of a corn (Zea mays, L. var. Funks G5757) crop to determine the effects of leaching rate, sulfur rate, and S source on SO2-4 leaching losses and plant growth. In the first experiment, the effects of percolation rate (0–6.1 mm d–1) and rate of gypsum application (0–40 µg S g–1) on SO2-4 leaching losses and S recovery by two successive crops were studied. Increasing the percolation rate greatly increased SO2-4 leaching losses and decreased the apparent fertilizer recovery by the first crop. Apparent S recovery was also greatly reduced with increasing amounts of applied gypsum. In the second experiment, S leaching losses from gypsum and anhydrite of various particle sizes and from powdered elemental S were evaluated at one percolation rate (3.9 mm d–1). The rate of SO2-4 leaching loss from powdered gypsum and anhydrite gradually decreased with time, indicating a decrease in the dissolution rate of the source as the amount of solid phase material decreased. Increasing the particle size of the materials decreased the leaching losses but had no effect on apparent S recovery by the plants. At a given particle size other than powdered materials, there were no differences in leaching losses between gypsum and anhydrite. The amount of powdered gypsum leached, however, was three times greater than the amount of powdered anhydrite leached. Leaching losses from powdered elemental S were similar to the losses from the larger-sized particles of gypsum and anhydrite. Moderate to high percolation rates led to SO2-4 losses and decreased fertilizer efficiency. Increasing the size of gypsum particles and the use of anhydrite are promising methods of reducing such losses.


NOTES

1 Contribution from the Agro-Economic Div., International Fertilizer Development Center (IFDC), P.O. Box 2040, Muscle Shoals, AL 35660, U.S.A.

2 Former Soil Microbiologist (present address: Soils and Irrigation Inst., 600 Belvedere St., Private Bag X79, Pretoria 0001, South Affica), Research Associate, and Research Assistant, respectively.

Received for publication June 27, 1983. Accepted for publication October 11, 1983.







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 © 1984 by the Soil Science Society of America.