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


     


Published online 25 January 2008
Published in Soil Sci Soc Am J 72:370-378 (2008)
DOI: 10.2136/sssaj2007.0126
© 2008 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
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
Google Scholar
Right arrow Articles by Haile-Mariam, S.
Right arrow Articles by Paul, E. A.
PubMed
Right arrow Articles by Haile-Mariam, S.
Right arrow Articles by Paul, E. A.
Agricola
Right arrow Articles by Haile-Mariam, S.
Right arrow Articles by Paul, E. A.
Related Collections
Right arrow Tillage
Right arrow Soil Organic Matter

SOIL BIOLOGY & BIOCHEMISTRY

Fractionation and Long-Term Laboratory Incubation to Measure Soil Organic Matter Dynamics

S. Haile-Mariama, H. P. Collinsb,*, S. Wrightc and E. A. Pauld

a Washington State Univ., Irrigated Agricultural Research and Extension Center, 24106 N. Bunn Rd., Prosser, WA 99350
b USDA-ARS, Vegetable and Forage Research Unit, 24106 North Bunn Rd., Prosser, WA 99350
c USDA-ARS, 10300 Baltimore Ave., Bldg. 001, Room 140, BARC-West, Beltsville, MD 20705
d Colorado State Univ., Natural Resource Ecology Lab., Fort Collins, CO

* Corresponding author (hal.collins{at}ars.usda.gov).

Soil organic matter (SOM) in agricultural soils comprises a significant part of the global terrestrial C pool. It has often been characterized by utilizing a combination of chemical dispersion of the soil followed by physical separation. We fractionated soil samples under continuous corn (Zea mays L.) rotations at four long-term sites in the Corn Belt to determine the concentration of C and N associated with soil fractions (light fraction [LF], particulate organic matter [POM], silt size, clay size, and Bradford reactive soil protein [BRSP]) and to identify the change in C concentration and {delta}13C signal of each fraction using laboratory incubations. Light fractions comprised 3 to 5% of the soil organic carbon (SOC), with no significant difference between conventional tillage (CT) and no-till (NT) treatments. The POM fraction accounted for 5 to 11% of the SOC in the soils with >30% clay and 17 to 23% for the soils with <20% clay. The clay-size fraction contained the highest proportion of SOC. Measurement of 13C during long-term incubation showed that the average mean residence time (MRT) of corn-derived C in the LF was 3.5 yr, whereas the POM fractions ranged from 6 to 12 yr. The 13C changes during incubation show that both fractions consist of a mixture of active and resistant materials, with movement between fractions. The BRSP has long MRTs except in the NT Hoytville soil. Measurement of the dyna mics of these fractions provides a basis for C models to test the impacts of land use and management on C sequestration.

Abbreviations: BRSP, Bradford reactive soil protein • CT, conventional tillage • KBS, Kellogg Biological Station • LF, light fraction • MRT, mean residence time • NT, no-till • OM, organic matter • POM, particulate organic matter • SOC, soil organic carbon • SOM, soil organic matter







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 © 2008 by the Soil Science Society of America.