Understanding soil respiration (R-s) response to thinning is an important component of our understanding of belowground carbon (C) dynamics and evaluating effects of forest management on C cycling. Therefore, we partitioned Rs into heterotrophic respiration (R-h) and autotrophic respiration (R-a) using trenched plots in a 20 year-old Pinus tabulaeformis plantation, subjected to varying thinning intensities, in Shanxi Province, China. Soil respiration was measured using an infrared gas exchange analyzer in untrenched and trenched plots. Rates of soil respiration were measured twice a month from May to October in 2011 and 2012, while soil temperature and moisture were obtained using temperature and moisture probes and data loggers. R-s was measured in untrenched plots and R-h in trenched plots. Mean R-s and R-h values were significantly greater in stands subjected to heavy thinning (HT) (R-s = 2.79 mu mol CO2 m(-2) s(-1), R-h = 2.24 mu mol CO2 m(-2) s(-1)) than in the control (CK) (R-s = 2.29 mu mol CO2 m(-2) s(-1), R-h = 1.81 mu mol CO2 m(-2) s(-1)) and low thinned stand (LT) (R-s = 2.48 mu mol CO2 m(-2) s(-1), R-h =1.80 mu mol CO2 m(-2) s(-1)). The mean R-a was greater in the thinned stands (R-a = 0.69, 0.58, 0.55 mu mol CO2 m(-2) s(-1) in LT, moderate thinned stand (MT) and HT) than CK (R-a = 0.48 mu mol CO2 m(-2) s(-1)), possibly the result of increased productivity and root growth in thinned stands. The relative proportion of Rh to Rs averaged 71.6-79.7% over the four thinned stands. Temperature sensitivity (Q(10)) values of R-h ranged from 2.16 to 2.75 in the various thinning intensities, with the highest Q(10) value in the control stand. Temperature sensitivity of R-a was also affected by thinning ranging from 1.34 to 1.84. The model with the best fitted temperature and moisture factors explained 66.7-77.3% of the variation in R-h and 30.2-46.4% in R-a among the four thinned stands during two growing seasons. (C) 2015 Elsevier B.V. All rights reserved.