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Baseline-Dependent Responses of Soil Organic Carbon Dynamics to Climate and Land Disturbances
2013
Applied and Environmental Soil Science
Terrestrial carbon (C) sequestration through optimizing land use and management is widely considered a realistic option to mitigate the global greenhouse effect. But how the responses of individual ecosystems to changes in land use and management are related to baseline soil organic C (SOC) levels still needs to be evaluated at various scales. In this study, we modeled SOC dynamics within both natural and managed ecosystems in North Dakota of the United States and found that the average SOC
doi:10.1155/2013/206758
fatcat:iuyb344iojhdbozkvhhlyao63a