Effect of soil temperature and soil moisture on soil respiration of ungrazed grassland in Loess Plateau,Gansu
Soil respiration (SR) is a major component of greenhouse gas emission and is a crucial pathway of the C cycle.The potential increase of SR caused by global warming may present a positive feedback effect on atmospheric CO2 and climate change (Kirschbaum,1995).However, the factors that control the exchange of CO2 between soil and atmosphere in Loess Plateau, Gansu are not well understood.The results in this paper represent a preliminary exercise in studying SR variations and its correlation with soil temperature ( Ts) and soil moisture (Ms).
soil respiration soil temperature soil moisture grassland Loess Plateau
Li Xudong Guo Ding Li Xiaodong Dong Xiaoyu Fu Hua
Key Laboratory of Grassland Agro-ecosystem,Ministry of Agriculture,College of PastoraLagricultural Science andTechnology,Lanzhou University,Lanzhou 730000,China.
国际会议
呼和浩特
英文
2008-06-29(万方平台首次上网日期,不代表论文的发表时间)