Characteristics of CO2 release from forest soil in the mountains near Beijing

CO2 release from forest soil is a key driver of carbon cycling between the soil and atmosphere ecosystem. The rate of CO2 released from soil was measured in three forest stands (in the mountainous region near Beijing, China) by the alkaline absorption method from 2004 to 2006. The rate of CO2 released did not differ among the three stands. The CO2 release rate ranged from -aEuro parts per thousand 341 to 1,193 mg m (-aEuro parts per thousand 2) h (-aEuro parts per thousand 1), and the mean value over all three forests and sampling times was 286 mg m (-aEuro parts per thousand 2) h (-aEuro parts per thousand 1). CO2 release was positively correlated with soil water content and the soil temperature. Diurnally, CO2 release was higher in the day than at night. Seasonally, CO2 release was highest in early autumn and lowest in winter; in winter, negative values of CO2 release suggested that CO2 was absorbed by soil.