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Background  Soil respiration ( R   S  ) plays an important role in the concentration of atmospheric CO 2  and thus in global climate patterns. Due to the feedback between  R   S   and climate, it is important to investigate  R   S   responses to climate warming.    Methods  A soil warming experiment was conducted to explore  R   S   responses and temperature sensitivity ( Q  10 ) to climate warming in subtropical forests in Southwestern China, and infrared radiators were used to simulate climate warming.    Results  Warming treatment increased the soil temperature and  R   S   value by 1.4 °C and 7.3%, respectively, and decreased the soil water level by 4.2% (%/%). Both one- and two-factor regressions showed that warming increased the  Q  10  values by 89.1% and 67.4%, respectively. The effects of water on  Q  10 show a parabolic relationship to the soil water sensitivity coefficient. Both  R   S   and  Q  10  show no acclimation to climate warming, suggesting that global warming will accelerate soil carbon release.

Soil warming increases soil temperature sensitivity in subtropical Forests of SW China