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 34:118-121 (1970)
© 1970 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 Brown, P. L.
Right arrow Articles by Dickey, D. D.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Brown, P. L.
Right arrow Articles by Dickey, D. D.
Agricola
Right arrow Articles by Brown, P. L.
Right arrow Articles by Dickey, D. D.

Losses of Wheat Straw Residue Under Simulated Field Conditions1

Paul L. Brown and David D. Dickey2

ABSTRACT

Wheat (Triticum aestivum L.) straw residues contained in fiberglass screen envelopes were exposed to field conditions at Bozeman and Huntley, Mont. Samples from above-soil, on-soil, and buried exposures were taken periodically during an 18-month period to measure weight losses and changes in N and P contents of the residues. Decomposition was more rapid at Huntley than at Bozeman, probably because air temperatures averaged 2.3C warmer at Huntley. Percentage losses were inversely related to residue amounts. After 18 months, on-soil residue losses averaged 31% at Bozeman and 40% at Huntley. The 50% decomposition stage for buried straw occurred in 3 months at Huntley and 6 months at Bozeman, and after 18 months, losses of buried straw averaged 93% at Bozeman and 98% at Huntley. Compared to the original straw, both N and P percentages increased as much as sixfold in the buried samples during decomposition. For buried straw, maximum percent N was 1.18 at Bozeman and 1.46 at Huntley. Similar values for maximum percent P were 0.132 at Bozeman and 0.147 at Huntley.

For buried straw, N and P immobilization was maximum after 3 months at both locations. At that time, N contents at the two locations exceeded original content by an average of 1.6, 2.9, 2.8, 2.9, and 5.3 kg/ha for straw rates of 1,121, 2,242, 3,363, 4,484, and 6,732 kg/ha. P contents exceeded original content by an average of 0.3, 0.5, 0.7, 1.0, and 1.7 kg/ha for the same straw rates.


NOTES

1 Contribution from the Soil and Water Conservation Research Division, ARS, USDA, in cooperation with the Montana Agr. Exp. Sta., Montana Agr. Exp. Sta. J. Series no. 952.

2 Research Soil Scientist and Agricultural Research Technician, USDA, Bozeman, Mont.

Received for publication April 24, 1969. Accepted for publication August 27, 1969.




This article has been cited by other articles:


Home page
Soil Sci.Home page
J.L. Steiner, H.H. Schomberg, P.W. Unger, and J. Cresap
Crop Residue Decomposition in No-Tillage Small-Grain Fields
Soil Sci. Soc. Am. J., November 1, 1999; 63(6): 1817 - 1824.
[Abstract] [Full Text] [PDF]




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 © 1970 by the Soil Science Society of America.