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 27:200-204 (1963)
© 1963 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 Walsh, L. M.
Right arrow Articles by Murdock, J. T.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Walsh, L. M.
Right arrow Articles by Murdock, J. T.
Agricola
Right arrow Articles by Walsh, L. M.
Right arrow Articles by Murdock, J. T.

Recovery of Fixed Ammonium by Corn in Greenhouse Studies1

L. M. Walsh and J. T. Murdock2

ABSTRACT

The availability of native fixed NH4 and applied NH4 fixed in the Ap and B1 horizons of a Dodge silt loam was investigated. In addition, the effect of freezing on the fixation of applied NH4 was studied. By applying K and N to either the same or separate layers of soil in green-house pots it was also possible to evaluate the effect of K on the release of fixed NH4. When NH4 and K were applied in the same layer of soil, the Ap and Bl horizons fixed 5 and 15% of the added NH4, respectively. An additional 5% of the added NH4 was fixed in each horizon when the soil was frozen after applying NH4. However, when NH4 and K were applied to separate layers of soil, negligible amounts of NH4 were fixed. Highly significant correlations between exchangeable K in the moist soil after cropping and the amount of applied NH4 fixed as measured by differential N uptake showed that the level of exchangeable K in the soil controlled the release of fixed NH4 to the crop. Correlations between two methods of measuring fixation of applied NH4, namely, differential N uptake and analysis of the soil after cropping, were highly significant.

These studies also indicated that about 15% (0.12 me. per 100 g.) of the native fixed NH4 in the Bl horizon was released when the level of exchangeable K in the soil was very low. However, very little native fixed NH4 was released from the Ap horizon, presumably because sufficient K remained in the soil of this horizon to block release of fixed NH4. These studies indicate that even under the most advantageous conditions very little of the native fixed NH4 is available to crops.


NOTES

1 Contribution from the Soils Department, University of Wisconsin, Madison. Published with the permission of the Director of the Wisconsin Agr. Exp. Sta. Presented before Div. IV, Soil Science Society of America, Nov. 16, 1959, at Cincinnati, Ohio.

2 Assistant Professor and Associate Professor, respectively, Soils Department, University of Wisconsin.

Received for publication May 7, 1962. Accepted for publication July 3, 1962.







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 © 1963 by the Soil Science Society of America.