摘要
The released soil CO2-C flux of four different land covers was studied in Guizhou karst region by static close chamber coupled with GC technique. The results showed that: 1) the released CO2-C flux of the four different land covers are significantly different, in a sequence of forest > secondary forest > burned field > maize field. The seasonal variation was obvious in all fields, with the highest average flux in summer and the lowest in winter; 2) the litter remarkably influenced the soil CO2-C flux in forest. The contribution of litter to forest total soil CO2-C emission was about 17%. Based on ground temperature, the calculated Q10 was 1.92 in the forest with litter and 2.10 in that without; and 3) excepted burned field and secondary forest, there was a remarkable positive correlation between soil CO2-C flux and temperature in different soil layers. By contrast, no obvious correlation between soil CO2-C flux and humidity (WFPS) was observed.