Moreover, Fmax/DOC of each component at sites A2 to A3 showed a decreasing trend, and the endogenous component (C3) decreased by 52% at A3 compared to that at A2, while DOC content increased.
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Soil Organic Carbon Distribution and Its Response to Soil Erosion Based on EEM-PARAFAC and Stable Carbon Isotope, a Field Study in the Rocky Desertification Control of South China Karst.
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