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 46:280-284 (1982)
© 1982 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 Frankenberger, W. T.
Right arrow Articles by Tabatabai, M. A.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Frankenberger, W. T., Jr.
Right arrow Articles by Tabatabai, M. A.
Agricola
Right arrow Articles by Frankenberger, W. T.
Right arrow Articles by Tabatabai, M. A.

Transformations of Amide Nitrogen in Soils1

W. T. Frankenberger, Jr. and M. A. Tabatabai2

ABSTRACT

Amides added to soils are hydrolyzed to ammonium (NH+4) and their corresponding carboxylic acids. Studies of transformations of amide-N in soils deserve attention because amides have potential as nitrogen (N) fertilizers. In this work, the transformations of amide-N (200 µg/g of soil) were studied in field-moist soils incubated under aerobic conditions at 30°C for 14 days. The recovery of inorganic N (as NH3, NH4+, NO2-, and NO3-) produced from 25 amides or their derivatives was determined and compared with those obtained with (NH4)2SO4 and urea added to five soils. Results showed that with the exception of cyanamide, dicyandiamide, benzenesulfonamide, and sulfanilamide, which resisted decomposition, all other amides were readily hydrolyzed in the five soils used. With most of the amides studied, the inorganic N produced was accumulated as NO3-. The recovery of nitrogen as NO3- from each of five soils treated with urea, acetamide, propionamide, 2-cyanoacetamide, n-butyramide, oxamide, or DL-lactamide was <50% of the N added. The average percentage of NH4+-N recovered from the soils used exceeded 40% of the total inorganic N produced when thioacetamide, fluoroacetamide, and 2-chloroacetamide were added to soils. With one sandy soil, the addition of urea, formamide, N-benzylformamide, and p-nitrobenzamide resulted in accumulation of NO2-, ranging from 5 to 21% of the inorganic N recovered. Appreciable amounts of NH3 were volatilized when formamide, acrylamide, 2-cyanoacetamide, p-nitrobenzamide, and urea were applied to soils, especially from the sandy soil. The average recovery of amide-N as inorganic N from the five soils used ranged from 4% with dicyandiamide to 100% with formamide.


NOTES

1 Journal Paper no. J-10175 of the Iowa Agric. Home Econ. Exp. Stn., Ames. Projects 2,082 and 2,112. Presented before Div. S-3, Soil Science Society of America, Fort Collins, Colo., 8 Aug. 1979.

2 Graduate Research Assistant and Professor of Soil Biochemistry, respectively, Dep. of Agron., Iowa State Univ., Ames, IA 50011. The Senior Author is currently Assistant Professor, Dep. of Soil and Environ. Sciences, Univ. of California, Riverside, CA 92521.

Received for publication February 11, 1981. Accepted for publication November 3, 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 © 1982 by the Soil Science Society of America.