Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States); US Dept. of Agriculture (USDA), Davis, CA (United States). California Climate Hub
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Aims: Land use change from native grasslands to arable lands globally impacts soil ecosystem functions, including the storage of soil organic carbon (SOC). Understanding the factors affecting SOC changes in topsoil and subsoil due to land use is crucial for effective mitigation strategies. We determined SOC storage and persistence as affected by land use change from native prairies to arable lands. Methods: Here we examined SOC stocks, soil δ13C and Δ14C signatures, microbial communities (bacteria and fungi), and soil mineral characteristics under native prairies and long-term arable lands (i.e., > 40 years) down to 3 m in the U.S. Midwest. Results: Native prairie soils had higher SOC stocks in the A horizon and 0–50 cm depth increment than arable soils. For both land use types, the δ13C and Δ14C values significantly decreased with depth, with the latter pointing towards highly stabilized SOC, especially in the B- and C-horizons. Analysis of the microbial communities indicated that the diversity of bacteria and fungi decreased with increasing soil depth. The content of oxalate soluble Al appeared to be the single most important predictor of SOC across horizons and land use types. Conclusion: Our data suggest that most SOC gains and losses and transformation and translocation processes seem to be restricted to the uppermost 50 cm. Increasing SOC retention in the A and B horizons within the 0–50 cm depth would enhance organic material serving as substrate and nutrients for microbes and plants (A horizon) and facilitate long-term SOC storage in the subsoil (B horizon).
Anuo, Christopher O., et al. "Storage and persistence of organic carbon in the upper three meters of soil under arable and native prairie land use." Plant and Soil, vol. 509, no. 1-2, Jul. 2024. https://doi.org/10.1007/s11104-024-06850-0
Anuo, Christopher O., Li, Lidong, Moreland, Kimber C., McFarlane, Karis J., Malakar, Arindam, Cooper, Jennifer A., Maharjan, Bijesh, & Kaiser, Michael (2024). Storage and persistence of organic carbon in the upper three meters of soil under arable and native prairie land use. Plant and Soil, 509(1-2). https://doi.org/10.1007/s11104-024-06850-0
Anuo, Christopher O., Li, Lidong, Moreland, Kimber C., et al., "Storage and persistence of organic carbon in the upper three meters of soil under arable and native prairie land use," Plant and Soil 509, no. 1-2 (2024), https://doi.org/10.1007/s11104-024-06850-0
@article{osti_2438170,
author = {Anuo, Christopher O. and Li, Lidong and Moreland, Kimber C. and McFarlane, Karis J. and Malakar, Arindam and Cooper, Jennifer A. and Maharjan, Bijesh and Kaiser, Michael},
title = {Storage and persistence of organic carbon in the upper three meters of soil under arable and native prairie land use},
annote = {Aims: Land use change from native grasslands to arable lands globally impacts soil ecosystem functions, including the storage of soil organic carbon (SOC). Understanding the factors affecting SOC changes in topsoil and subsoil due to land use is crucial for effective mitigation strategies. We determined SOC storage and persistence as affected by land use change from native prairies to arable lands. Methods: Here we examined SOC stocks, soil δ13C and Δ14C signatures, microbial communities (bacteria and fungi), and soil mineral characteristics under native prairies and long-term arable lands (i.e., > 40 years) down to 3 m in the U.S. Midwest. Results: Native prairie soils had higher SOC stocks in the A horizon and 0–50 cm depth increment than arable soils. For both land use types, the δ13C and Δ14C values significantly decreased with depth, with the latter pointing towards highly stabilized SOC, especially in the B- and C-horizons. Analysis of the microbial communities indicated that the diversity of bacteria and fungi decreased with increasing soil depth. The content of oxalate soluble Al appeared to be the single most important predictor of SOC across horizons and land use types. Conclusion: Our data suggest that most SOC gains and losses and transformation and translocation processes seem to be restricted to the uppermost 50 cm. Increasing SOC retention in the A and B horizons within the 0–50 cm depth would enhance organic material serving as substrate and nutrients for microbes and plants (A horizon) and facilitate long-term SOC storage in the subsoil (B horizon).},
doi = {10.1007/s11104-024-06850-0},
url = {https://www.osti.gov/biblio/2438170},
journal = {Plant and Soil},
issn = {ISSN 0032-079X},
number = {1-2},
volume = {509},
place = {United States},
publisher = {Springer Nature},
year = {2024},
month = {07}}
McFarlane, Karis; Finstad, Kari; Van Straaten, Oliver
Environmental System Science Data Infrastructure for a Virtual Ecosystem; Tropical Forest Response to a Drier Future: Turnover Times of Soil Organic Matter, Roots, Respired CO2, and CH4 Across Moisture Gradients in Time and Spacehttps://doi.org/10.15485/2283436