|
|
||||||||
a Great Plains Systems Res. Unit, USDA-ARS, P.O. Box E, Fort Collins, CO 80522
b Dep. of Soil and Crop Science, Colorado State Univ., Fort Collins, CO 80523
* Corresponding author (Lucretia.Sherrod{at}colostate.edu)
Previous studies of no-till management in the Great Plains have shown that increased cropping intensity increased soil organic carbon (SOC). The objectives of this study were to (i) determine which soil C pools (active, slow, and passive) were impacted by cropping intensity after 12 yr of no-till across potential evapotranspiration (PET) and slope position gradients; (ii) relate C pool sizes to the levels found in total SOC; and (iii) determine C pool sizes relative to C levels found in a grass treatment (G). Cropping systems were wheat (Triticum aestivum)-fallow (WF), wheat-corn (Zea mays L.)-fallow (WCF), wheat-corn-millet (Panicum miliaceum)-fallow (WCMF), and continuous cropping (CC) at three PET sites in Colorado. Active C (Soil microbial biomass C [SMBC]); and slow pool C (particulate organic matter C; POM-C) increased as cropping intensity increased, dependent on PET. Passive C (mineral associated organic C [MAOC]) was strongly influenced by a site-by-slope position interaction but not by cropping system. Toeslope soils had 35% higher POM-C compared with summits and sideslopes. All C pools were strongly correlated with total SOC, with the variability decreasing as C pool turnover time increased. Carbon pool sizes in cropping systems relative to levels found in G were independently influenced by cropping system. The highest were found in the CC system, which had 91, 78, and 90% of the amounts of C found in the perennial G system in the active, slow, and passive C pools, respectively.
Abbreviations: CC, continuous cropping CMIN, carbon mineralized CRP, Conservation Reserve Program G, grass LSD, least significant difference MAOC, mineral-associated organic carbon MAT, mean annual temperature OPE, open pan evaporation PET, potential evapotranspiration POM-C, particulate organic matter carbon SMBC, soil microbial biomass C SOC, soil organic carbon SOM, soil organic matter WCF, wheatcornfallow WCMF, wheatcornmilletfallow WF, wheatfallow
This article has been cited by other articles:
![]() |
H. Minoshima, L. E. Jackson, T. R. Cavagnaro, and H. Ferris Short-Term Fates of Carbon-13-Depleted Cowpea Shoots in No-Till and Standard Tillage Soils Soil Sci. Soc. Am. J., October 29, 2007; 71(6): 1859 - 1866. [Abstract] [Full Text] [PDF] |
||||
![]() |
H. Minoshima, L.E. Jackson, T.R. Cavagnaro, S. Sanchez-Moreno, H. Ferris, S.R. Temple, S. Goyal, and J.P. Mitchell Soil Food Webs and Carbon Dynamics in Response to Conservation Tillage in California Soil Sci. Soc. Am. J., May 16, 2007; 71(3): 952 - 963. [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 | |||