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 43:95-100 (1979)
© 1979 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 Westerman, R. L.
Right arrow Articles by Tucker, T. C.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Westerman, R. L.
Right arrow Articles by Tucker, T. C.
Agricola
Right arrow Articles by Westerman, R. L.
Right arrow Articles by Tucker, T. C.

In Situ Transformations of Nitrogen-15 Labeled Materials in Sonoran Desert Soils1

R. L. Westerman and T. C. Tucker2

ABSTRACT

Influences of ammonium, nitrate, organic N sources and organic C amendments on microbial respiration, N transformations and gaseous losses were measured under natural environmental conditions in two field experiments. Microbial respiration was increased by addition of wheat straw and barley grain. Addition of N as (15NH4)2SO4 and K15NO3 alone did not increase CO2 evolution significantly.

Significant immobilization of added inorganic-15N occurred with few exceptions in all treatments except nitrate alone. Organic-15N in soils amended with wheat straw increased with increasing N rates with both inorganic N sources. Inorganic-15N was practically void in both soils at the end of 12 months. Mineralization of 15N-labeled barley grain occurred but at a very low rate and no significant accumulations of inorganic-15N were observed.

Gaseous losses of N at the end of 12 months varied from 73 to 94% of the inorganic-N added alone, with the greatest loss occurring from K15NO3. The incorporation of wheat straw stimulated immobilization of added N and reduced gaseous losses to 30 to 86% of the total N applied and the smallest loss occurred with (15NH4)2SO4. The average loss of mineralized organic-15N derived from barley grain for the two soils was 19% of the total N added. Most of the gaseous losses occurred within the first 3 months, the period of the measurable rainfall.

Analyses of subdivided soil sections (0–5 and 5–10 cm) showed that 95 to 100% of 15N remaining in the soil was in the upper 5-cm layer indicating that leaching was not appreciable in any treatment.


NOTES

1 Contribution from Department of Soils, Water and Engineering, Arizona Agr. Exp. Sta., Tucson 85721. Published with approval of the Director as journal article No. 2702. This work was supported in part by a grant from US IBP Desert Bionie Program of the National Science Foundation.

2 Associate Professor and Professor, Department of Soils, Water and Engineering, the Univ. of Arizona, respectively. Address of senior author is now Dept. of Agron., Oklahoma State Univ., Stillwater, Oklahoma 74074.

Received for publication December 9, 1977. Accepted for publication August 24, 1978.







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 © 1979 by the Soil Science Society of America.