Fig. 2: Different responses of the temperature sensitivity (Q10) of SOC- and SIC-derived CO2 emissions to aridity changes. | Nature Communications

Fig. 2: Different responses of the temperature sensitivity (Q10) of SOC- and SIC-derived CO2 emissions to aridity changes.

From: Drought may exacerbate dryland soil inorganic carbon loss under warming climate conditions

Fig. 2

Relationships of the Q10 of SOC- and SIC-derived CO2 emissions with aridity in the topsoil (0–10 cm, a) and subsoil (35–50 cm, b). Linear regression was used, and the dashed lines surrounding the regression lines correspond to the 95% confidence interval of the correlation. Q10 was estimated under field moisture conditions.

Back to article page