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 25:186-189 (1961)
© 1961 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 Schwartzbeck, R. A.
Right arrow Articles by Schmidt, E. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Schwartzbeck, R. A.
Right arrow Articles by Schmidt, E. L.
Agricola
Right arrow Articles by Schwartzbeck, R. A.
Right arrow Articles by Schmidt, E. L.

Gaseous Nitrogen Losses from Nitrogen Fertilized Soils Measured With Infrared and Mass Spectroscopy1

R. A. Schwartzbeck, J. M. MacGregor and E. L. Schmidt2

ABSTRACT

The evolution of nitrogen gases from four soils was studied by total soil nitrogen analysis, the mass spectrometer with N15-labeled nitrogen carriers, and with infrared spectroscopy. The type and amount of nitrogen gas evolved was influenced by a number of factors. Soil type was important in that the Nicollet and Fargo soils resulted in the evolution of more N2 and N2O than did the Fayette and Laredo soils. Soil properties had little effect on the total N2 evolved from NH4NO3, but greater differences occurred from soils treated with HNO3. The type of nitrogen carrier influenced the nature of the gaseous nitrogen released. NH4NO3 treatment favored N2O evolution and HNO3 treatment favored N2. Only small amounts of N2 and N2O were evolved from soils treated with NH4Cl or urea. Nitrogen applied at 1080 pounds per acre always resulted in larger losess of N2O and N2 than that applied at 360 pounds per acre. However, in both the Nicollet and Fargo soils at water saturation, the percentage of applied nitrogen that was lost was about the same at both low and high rates of treatment. Substantial gaseous losses of applied fertilizer occurred mainly when water-saturated conditions prevailed. Small losses did occur from soils at field moisture capacity. N2O evolution was influenced by the ammonium to nitrate ratio of the nitrogen treatment.


NOTES

1 Paper No. 4439 Scientific Journal Series, Minnesota Agr. Exp. Sta., University of Minnesota, St. Paul. Presented before Div. II, Soil Science Society of America, Nov. 17, 1959, at Cincinnati, Ohio.

2 Formerly Research Assistant, Department of Soils, present address Dow Chemical Co., Washington, D. C.; Professor, Department of Soils; Associate Professor, jointly Department of Soils and Department of Bacteriology, respectively.

Received for publication July 22, 1960. Accepted for publication September 30, 1960.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1961 by the Soil Science Society of America.