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Temperature sensitivity of soil organic carbon (SOC) mineralization (i.e.,\udQ10) determines how strong the feedback from global warming may be on\udthe atmospheric CO2 concentration; thus, understanding the factors\udinfluencing the interannual variation in Q10 is important for\udaccurately estimating local soil carbon cycle. In situ SOC mineralization rate was\udmeasured using an automated CO2 flux system (Li-8100) in long-term\udbare fallow soil in the Loess Plateau (35°12' N,\ud107°40' E) in Changwu, Shaanxi, China from 2008 to 2013.\udThe results showed that the annual cumulative SOC mineralization ranged from\ud226 to 298 g C m−2 yr−1, with a mean of 253 g C m−2 yr−1\udand a coefficient of variation (CV) of 13%, annual Q10 ranged from 1.48 to 1.94, with a mean\udof 1.70 and a CV of 10%, and annual soil moisture content ranged from\ud38.6 to 50.7% soil water-filled pore space (WFPS), with a mean of\ud43.8% WFPS and a CV of 11%, which were mainly affected by the\udfrequency and distribution of precipitation. Annual Q10 showed\uda quadratic correlation with annual mean soil moisture content. In\udconclusion, understanding of the relationships between interannual variation\udin Q10, soil moisture, and precipitation are important to accurately\udestimate the local carbon cycle, especially under the changing climate

Soil moisture influence on the interannual variation in temperature sensitivity of soil organic carbon mineralization in the Loess Plateau