摘要
1 Introduction With the exploration and development of coalbed methane （CBM）, there has been a growing interest in the coalbed gas desorption behavior and its geological controls. To date, two primary species including the desorption rate and desorption velocity of the coalbed gas have been studied widely （e.g. Pollard and Aydin, 1998; Chen et al., 2008; Liu et al., 2012）.
1 Introduction With the exploration and development of coalbed methane （CBM）, there has been a growing interest in the coalbed gas desorption behavior and its geological controls. To date, two primary species including the desorption rate and desorption velocity of the coalbed gas have been studied widely （e.g. Pollard and Aydin, 1998; Chen et al., 2008; Liu et al., 2012）.
基金
supported by the Natural Science Foundation of Shandong Province(grant no.ZR2014DP007)
