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


     


Published online 21 January 2009
Published in Soil Sci Soc Am J 73:138-145 (2009)
DOI: 10.2136/sssaj2007.0384
© 2009 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 White, P. M.
Right arrow Articles by Rice, C. W.
Right arrow Search for Related Content
PubMed
Right arrow Articles by White, P. M.
Right arrow Articles by Rice, C. W.
Agricola
Right arrow Articles by White, P. M.
Right arrow Articles by Rice, C. W.
Related Collections
Right arrow Carbon Sequestration
Right arrow Microbial Processes
Right arrow Tillage

SOIL BIOLOGY & BIOCHEMISTRY

Tillage Effects on Microbial and Carbon Dynamics during Plant Residue Decomposition

Paul M. Whitea,b,* and Charles W. Ricec

a Dep. of Agronomy, Kansas State Univ., Manhattan, KS 66506
b current address: USDA-ARS/SEWRL, 2316 Rainwater Rd., Tifton, GA 31794
c Dep. of Agronomy, Kansas State Univ., 2004A Throckmorton Plant Sciences Center, Manhattan, KS 66506

* Corresponding author (Paul.White{at}ars.usda.gov).

One goal of soil C sequestration is to increase the mass of C stored in agricultural soils. Reducing soil disturbance, e.g., no-till management, facilitates soil fungal growth and results in higher C sequestration rates; however, the specific mechanisms associated with short-term plant residue C and N retention are less clear. We applied 13C- and 15N-enriched grain sorghum [Sorghum bicolor (L.) Moench] residue to no-till (NT) and conventional tillage (CT) soils, and measured the 13C and 15N retention in the soil and in aggregate fractions, along with soil microbial dynamics, during a growing season. The added plant residue mineralized rapidly in both tillage systems, with similar decomposition kinetics, as indicated by 13C data. Mass balance calculations indicated that approximately 70% of the added 13C was mineralized to CO2 by 40 d. Total Gram positive and Gram negative bacteria and fungal phospholipid fatty acids were higher under NT 0 to 5 cm during the most active period of residue mineralization compared with the CT 0- to 5- or 5- to 15-cm depths. No changes were observed in the NT 5- to 15-cm depth. The >1000-µm aggregate size class retained the most 13C, regardless of tillage. The NT >1000-µm aggregates retained more 15N at the end of the experiment than other NT and CT aggregates size classes. Data obtained indicate higher biological activity associated with NT soils than under CT, and increased retention of plant residue C and N in macroaggregates.

Abbreviations: CT, conventional tillage • Gm+, Gram positive • Gm, Gram negative • NT, no-till • PLFA, phospholipid fatty acids • R+, residue added • R–, no residue added • SOC, soil organic carbon • TC, total carbon • TN, total nitrogen • VPDB, Vienna PeeDee Belemnite







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 © 2009 by the Soil Science Society of America.