Chang Zongqiang, Shi Zuomin, Feng Qi, Su Yonghong
Key laboratory of Forest Ecology and Environmnent, State Forestry Administration, Institute of Cold and Arid Regions Environmental and Engineering, Chinese Academy of Sciences, Lanzhou, China.
Ying Yong Sheng Tai Xue Bao. 2005 Sep;16(9):1603-6.
Employing LiCor 6400 gas exchange analyzer and soil respiration chamber attachment (LiCor Inc., Lincoln, NE, USA), this paper continuously measured the soil surface CO2 effluxes on the sloping pasture of Heihe River basin from early April to late October 2003 to investigate the soil CO2 efflux rate and its feedback to the changes of climate and land use. The results showed that from May to October, the diurnal variation of soil respiration was low at night, the lowest at 7:00, 6:30, 5:30, 6:00 and 7:00, raised rapidly at 7:00 - 8:30, and then descended at 16:00 - 18:30. The maximum soil CO2 efflux appeared at 15:00, 14:30, 14:30, 13:30, 14:00 and 15:00. The mean daily soil respiration rate was 0.31 - 6.98 micromol m(-2) s(-1), with the maximum in July and August, the second in May and September, and nearly consistent in April and October. Soil respiration rate had an exponential and power correlation with temperature and soil moisture, respectively.
利用LiCor 6400气体交换分析仪和土壤呼吸室附件(美国内布拉斯加州林肯市LiCor公司),本文于2003年4月初至10月末连续测量了黑河流域坡地牧场土壤表面的CO2通量,以研究土壤CO2排放速率及其对气候和土地利用变化的反馈。结果表明,5月至10月,土壤呼吸的日变化夜间较低,在7:00、6:30、5:30、6:00和7:00时最低;7:00 - 8:30迅速升高,然后在16:00 - 18:30下降。土壤CO2排放最大值出现在15:00、14:30、14:30、13:30、14:00和15:00。土壤呼吸日平均速率为0.31 - 6.98微摩尔·米-2·秒-1,7月和8月最高,5月和9月次之,4月和10月相近。土壤呼吸速率分别与温度和土壤湿度呈指数和幂函数关系。