SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 42:77-80 (1978)
© 1978 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 Kissel, D. E.
Right arrow Articles by Smith, S. J.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Kissel, D. E.
Right arrow Articles by Smith, S. J.
Agricola
Right arrow Articles by Kissel, D. E.
Right arrow Articles by Smith, S. J.

Fate of Fertilizer Nitrate Applied to Coastal Bermudagrass on a Swelling Clay Soil1

D. E. Kissel and S. J. Smith2

ABSTRACT

The purpose of this study was to determine why N fertilizer recovery by Coastal bermudagrass (Cynodon dactylon L.) is lower on swelling clay soils than on coarse-textured soils. The disposition of N fertilizer applied to Coastal bermudagrass in the field over two growing seasons was determined by applying 560 kg N/ha as Ca(NO3)2 tagged with 7.599 atom % 15N to a field microplot during 1974 and measuring various components of the N balance. Plant uptake of residual N was measured during 1975.

Forty-nine percent of the applied N was recovered in harvested forage in 1974. About 40% of the applied N remained in the soil as residual N at the end of 1974. About 10% of the N was unaccounted for, indicating that denitrification losses were no more than 10% of the applied N. Most of the residual N at the end of the first growing season was immobilized N or was present in the root system of the grass. Immobilization is, therefore, a major factor causing low recovery of applied N by Coastal bermudagrass on swelling clay soils. Moreover, since only 17% of the residual N was recovered in forage during 1975 (7% of the N applied in 1974), most of the immobilized N was not available the following year.


NOTES

1 Contribution from Texas Agric. Exp. Stn., Texas A&M Univ., College Stn., Texas, in cooperation with the USDA-ARS, Durant, Okla.

2 Associate Professor, Texas Agric. Exp. Stn., Blackland Res. Center, Temple, TX 76501; and Soil Scientist, USDA Water Quality Management Lab., Durant, OK 74701, respectively.

Received for publication July 18, 1977. Accepted for publication September 7, 1977.




This article has been cited by other articles:


Home page
Soil Sci.Home page
M. A. Williams, C. W. Rice, and C. E. Owensby
Nitrogen Competition in a Tallgrass Prairie Ecosystem Exposed to Elevated Carbon Dioxide
Soil Sci. Soc. Am. J., March 1, 2001; 65(2): 340 - 346.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
D. L. Jones and D. Shannon
Mineralization of Amino Acids Applied to Soils: Impact of Soil Sieving, Storage, and Inorganic Nitrogen Additions
Soil Sci. Soc. Am. J., September 1, 1999; 63(5): 1199 - 1206.
[Abstract] [Full Text]




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 © 1978 by the Soil Science Society of America.