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 45:782-786 (1981)
© 1981 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 Power, J. F.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Power, J. F.
Agricola
Right arrow Articles by Power, J. F.

Long-Term Recovery of Fertilizer Nitrogen Applied to a Native Mixed Prairie1

J. F. Power2

ABSTRACT

Previous research on perennial grassland soils has generally shown that a large part of any fertilizer nitrogen (N) added is immobilized in grass roots or in soil organic matter. Few studies have measured the amount of such immobilized N that eventually becomes mobilized and taken up by plant growth in subsequent years. In this experiment, up to 540-kg fertilizer N/ha was applied to native mixed prairie in North Dakota during a 1- to 6-year period, and residual effects of these treatments on grass production were followed until no further plant growth response was measured. When a total of 270- or 540-kg N/ha had been applied, plant growth responses were measured for up to 9 years after fertilization ceased. As fertilizer N rate decreased, length of residual effects likewise decreased. Part of the residual response may have resulted from increased density of cool-season grasses where higher N rates were applied. Growth responses after fertilization ceased were often greater when fertilizers were applied over a 6-year period, rather than applying an equal quantity of fertilizer N all in 1 year. For the 540-kg N/ha treatment, as much as 12% of the fertilizer N applied was recovered in top growth after fertilization ceased. Assuming that all increased inorganic N in the soil resulting from fertilization was used by plants during the residual period, and that the remaining fertilizer N taken up by top growth after fertilization ceased came from mobilization of fertilizer N present in grass roots in 1968, then an estimate can be made of availability of fertilizer N in roots. Maximum value for such an estimate was 44-kg N/ha, leaving 60- to 160-kg fertilizer N/ha permanently immobilized as this root material decomposed. Thus, when 270- or 540-kg fertilizer N/ha was applied, typically about 30% was permanently immobilized by absorption into root material during the period of fertilization, 35% was removed in top growth, and 35% was either immobilized permanently in soil organic matter or lost by gaseous means.


NOTES

1 Contribution from Agric. Res., Science and Ed. Admin., USDA.

2 Research Leader, USDA-SEA-AR, Lincoln, Nebr., formerly located at Mandan, N. Dak.

Received for publication December 3, 1980. Accepted for publication March 16, 1981.







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 © 1981 by the Soil Science Society of America.