SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 30 September 2008
Published in Soil Sci Soc Am J 72:1570-1579 (2008)
DOI: 10.2136/sssaj2007.0118
© 2008 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
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 Burger, M.
Right arrow Articles by Venterea, R. T.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Burger, M.
Right arrow Articles by Venterea, R. T.
Agricola
Right arrow Articles by Burger, M.
Right arrow Articles by Venterea, R. T.
Related Collections
Right arrow Nitrogen
Right arrow Microbial Processes
Right arrow Nutrient Management

SOIL BIOLOGY & BIOCHEMISTRY

Nitrogen Immobilization and Mineralization Kinetics of Cattle, Hog, and Turkey Manure Applied to Soil

Martin Burgera,b,* and Rodney T. Ventereaa

a USDA-ARS, Soil and Water Management, St. Paul, MN 55108
b Currently at: Dep. of Land, Air and Water Resources, Univ. of California, One Shields Ave., Davis, CA, 95616-8780

* Corresponding author (mburger{at}ucdavis.edu).

Nitrogen mineralization and immobilization following manure application are critical processes influencing plant N supply and offsite N losses. We conducted laboratory experiments to examine the influence of these two processes in addition to N oxide gas production on N availability for 180 d following manure addition. A Tara loam (fine-silty, mixed, superactive, frigid Aquic Hapludoll) and a Webster clay loam (fine-loamy, mixed, superactive, mesic Typic Endoaquoll) amended with liquid dairy (Bos taurus) manure (LD) were incubated at 25 and 10°C, while Tara soil amended with solid dairy manure (SD) and turkey (Meleagris gallopavo) manure (T), and Webster soil amended with liquid hog (Sus scrofa) manure (H), were incubated at 25°C. Maximum net N immobilization was 14 and 40% of the initial NH4+ concentration in H and LD, respectively, and persisted for 35 to 180 d. In LD-, H-, and T-amended soils, net manure N mineralization was not apparent, and there was good agreement between initial NH4+ content and available inorganic N from the manure. These data suggest that, for these manure types, estimates of first-season available N would be improved by measuring manure NH4+. In contrast, in soil amended with SD, which had the lowest initial NH4+ content, 22% of organic N was mineralized. Gaseous N losses were <1% of the added N in all treatments. The previously developed model NCSOIL was used to predict plant N availability and NO3 leaching potential with various manure incorporation dates. Under climate conditions typical of the Upper Midwest, no clear advantage of late fall compared with spring incorporation of manure with regard to N availability could be shown, but NO3 leaching potential seemed high with early fall incorporation.

Abbreviations: H, liquid hog manure • LD, liquid dairy manure • MBC, microbial biomass carbon • MBN, microbial biomass nitrogen • SD, solid dairy manure • T, turkey manure







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 © 2008 by the Soil Science Society of America.