中文摘要：

Long-term continuous cropping of soybean(Glycine max), spring wheat(Triticum aesativum) and maize(Zea mays) is widely practiced by local farmers in northeast China. A field experiment(started in 1991) was used to investigate the differences in soil carbon dioxide(CO 2) emissions under continuous cropping of the three major crops and to evaluate the relationships between CO 2 fluxes and soil temperature and moisture for Mollisols in northeast China. Soil CO 2 emissions were measured using a closed-chamber method during the growing season in 2011. No remarkable differences in soil organic carbon were found among the cropping systems(P>0.05). However, significant differences in CO 2 emissions from soils were observed among the three cropping systems(P<0.05). Over the course of the entire growing season, cumulative soil CO 2 emissions under different cropping systems were in the following order: continuous maize((829±10) g CO 2 m-2)>continuous wheat((629±22) g CO 2 m-2)>continuous soybean((474±30) g CO 2 m-2). Soil temperature explained 42-65% of the seasonal variations in soil CO 2 flux, with a Q 10 between 1.63 and 2.31; water-filled pore space explained 25-47% of the seasonal variations in soil CO 2 flux. A multiple regression model including both soil temperature(T, °C) and water-filled pore space(W, %), log(f)=a+bT log(W), was established, accounting for 51-66% of the seasonal variations in soil CO 2 flux. The results suggest that soil CO 2 emissions and their Q 10 values under a continuous cropping system largely depend on crop types in Mollisols of Northeast China.

英文摘要：

Long-term continuous cropping of soybean （Glycine max）, spring wheat （Triticum aesativum） and maize （Zea mays） is widely practiced by local farmers in northeast China. A field experiment （started in 1991） was used to investigate the differences in soil carbon dioxide （CO2） emissions under continuous cropping of the three major crops and to evaluate the relationships between CO2 fluxes and soil temperature and moisture for Mollisols in northeast China. Soil CO2 emissions were measured using a closed-chamber method during the growing season in 2011. No remarkable differences in soil organic carbon were found among the cropping systems （P〉0.05）. However, significant differences in CO2 emissions from soils were observed among the three cropping systems （P〈0.05）. Over the course of the entire growing season, cumulative soil CO2 emissions under different cropping systems were in the following order： continuous maize （（829±10） g CO2 m2）〉continuous wheat （（629±22） g CO2 m^2）〉continuous soybean （（474±30） g CO2 m-2）. Soil temperature explained 42-65% of the seasonal variations in soil CO2 flux, with a Q10 between 1.63 and 2.31; water-filled pore space explained 25-47% of the seasonal variations in soil CO2 flux. A multiple regression model including both soil temperature （T, ~C） and water-filled pore space （W, %）, log（]）=a＋bT log（W）, was established, accounting for 51-66% of the seasonal variations in soil CO2 flux. The results suggest that soil CO2 emissions and their Q10 values under a continuous cropping system largely depend on crop types in Mollisols of Northeast China.