Extended Data Fig. 7: The effects of soil moisture on the relationships between temperature and various SOC cycling metrics.
From: Temperature effect on erosion-induced disturbances to soil organic carbon cycling
a, The relationship between soil moisture and the coefficient denoting the sensitivity of lateral SOC fluxes caused by erosion to the variation of mean annual temperature. Details of the regression between lateral SOC fluxes by erosion and temperature under various soil moisture conditions are displayed in Supplementary Fig. 3. b, The relationship between soil moisture and the coefficient denoting the sensitivity of SOC decomposition rates to the variation of mean annual temperature. Details of the regression between SOC decomposition rates and temperature under various soil moisture conditions are displayed in Supplementary Fig. 4. c, The relationship between soil moisture and the coefficient denoting the sensitivity of the C sink strength per unit lateral SOC flux to the variation of mean annual temperature. Details of the regression between the C sink strength per unit lateral SOC flux and temperature under various soil moisture conditions are displayed in Supplementary Fig. 5. d, The relationship between soil moisture and the coefficient denoting the sensitivity of the C sink strength per unit cropland area to the variation of mean annual temperature. Details of the regression between the C sink strength per unit cropland area and temperature under various soil moisture conditions are displayed in Supplementary Fig. 6.
