Modeling biogeochemistry in agricultural soils
Abstract
An existing model of C and N dynamics in soils was supplemented with a plant growth submodel and cropping practice routines (fertilization, irrigation, tillage, crop rotation, and manure amendments) to study the biogeochemistry of soil carbon in arable lands. The new model was validated against field results for short-term (1-9 years) decomposition experiments, the seasonal pattern of soil CO{sub 2} respiration, and long-term (100 years) soil carbon storage dynamics. A series of sensitivity runs investigated the impact of varying agricultural practices on soil organic carbon (SOC) sequestration. The tests were simulated for corn (maize) plots over a range of soil and climate conditions typical of the United States. The largest carbon sequestration occurred with manure additions; the results were very sensitive to soil texture (more clay led to greater sequestration). Increased N fertilization generally enhanced carbon sequestration, but the results were sensitive to soil texture, initial soil carbon content, and annual precipitation. Reduced tillage also generally (but not always) increased SOC content, through the results were very sensitive to soil texture, initial SOC content, and annual precipitation. A series of long-term simulations investigated the SOC equilibrium for various agricultural practices, soil and climate conditions, and crop rotations. Equilibrium SOC contentmore »
- Authors:
-
- Univ. of New Hampshire, Durham, NH (United States)
- Publication Date:
- OSTI Identifier:
- 96048
- Resource Type:
- Journal Article
- Journal Name:
- Global Biogeochemical Cycles
- Additional Journal Information:
- Journal Volume: 8; Journal Issue: 3; Other Information: PBD: Sep 1994
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; BIOGEOCHEMISTRY; MATHEMATICAL MODELS; MAIZE; PLANT GROWTH; SOILS; CARBON DIOXIDE FIXATION; CROPS; ATMOSPHERIC PRECIPITATIONS
Citation Formats
Li, C, Frolking, S, and Harriss, R. Modeling biogeochemistry in agricultural soils. United States: N. p., 1994.
Web. doi:10.1029/94GB00767.
Li, C, Frolking, S, & Harriss, R. Modeling biogeochemistry in agricultural soils. United States. https://doi.org/10.1029/94GB00767
Li, C, Frolking, S, and Harriss, R. 1994.
"Modeling biogeochemistry in agricultural soils". United States. https://doi.org/10.1029/94GB00767.
@article{osti_96048,
title = {Modeling biogeochemistry in agricultural soils},
author = {Li, C and Frolking, S and Harriss, R},
abstractNote = {An existing model of C and N dynamics in soils was supplemented with a plant growth submodel and cropping practice routines (fertilization, irrigation, tillage, crop rotation, and manure amendments) to study the biogeochemistry of soil carbon in arable lands. The new model was validated against field results for short-term (1-9 years) decomposition experiments, the seasonal pattern of soil CO{sub 2} respiration, and long-term (100 years) soil carbon storage dynamics. A series of sensitivity runs investigated the impact of varying agricultural practices on soil organic carbon (SOC) sequestration. The tests were simulated for corn (maize) plots over a range of soil and climate conditions typical of the United States. The largest carbon sequestration occurred with manure additions; the results were very sensitive to soil texture (more clay led to greater sequestration). Increased N fertilization generally enhanced carbon sequestration, but the results were sensitive to soil texture, initial soil carbon content, and annual precipitation. Reduced tillage also generally (but not always) increased SOC content, through the results were very sensitive to soil texture, initial SOC content, and annual precipitation. A series of long-term simulations investigated the SOC equilibrium for various agricultural practices, soil and climate conditions, and crop rotations. Equilibrium SOC content increased with decreasing temperatures, increasing clay content, enhanced N fertilization, manure amendments, and crops with higher residue yield. Time to equilibrium appears to be one hundred to several hundred years. In all cases, equilibration time was longer for increasing SOC content than for decreasing SOC content. Efforts to enhance carbon sequestration in agricultural soils would do well to focus on those specific areas and agricultural practices with the greatest potential for increasing soil carbon content. 64 refs., 13 figs., 5 tabs.},
doi = {10.1029/94GB00767},
url = {https://www.osti.gov/biblio/96048},
journal = {Global Biogeochemical Cycles},
number = 3,
volume = 8,
place = {United States},
year = {Thu Sep 01 00:00:00 EDT 1994},
month = {Thu Sep 01 00:00:00 EDT 1994}
}