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• W2895172385 abstract "Soils contain globally significant stocks of C, but the mechanisms regulating the preservation and stability of soil C stocks are not well defined. The role of climate has long been implicated as a major driver of soil C stock variation, with rising temperatures associated with higher decomposition rates and therefore smaller C stocks. The role of minerals in directly regulating the size and stability of C stocks has only recently become a focus of interest as researchers seek out new mechanistic explanations for the observed variance in the distribution of C across soils. The complex interactions among climatic and soil mineral variables and how these mechanistic relationships will change under different climate change scenarios are currently unknown. Although soil organic C is the focus of most soil C cycle research, soils also contain substantial inorganic C stocks. Climate and soil mineral assemblage influence the cycling of both these C reservoirs. Although the processes and mechanisms governing the cycling of these two pools are very different, both represent globally important C reservoirs with unique capacities to influence atmospheric CO2 concentrations and, by extension, feedbacks to global climate." @default.
• W2895172385 created "2018-10-12" @default.
• W2895172385 creator A5007560067 @default.
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• W2895172385 date "2018-01-01" @default.
• W2895172385 modified "2023-09-27" @default.
• W2895172385 title "Role of Mineralogy and Climate in the Soil Carbon Cycle" @default.
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• W2895172385 doi "https://doi.org/10.1016/b978-0-444-63865-6.00004-1" @default.
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