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Microbial degradation and its influence on components of coalbed gases in Enhong syncline, China

Microbial degradation and its influence on components of coalbed gases in Enhong syncline, China

作     者:Lan Fengjuan Qin Yong Li Ming Tang Yonghong Guo Chen Zhang Fei 

作者机构:School of Resource and Earth Science China University of Mining & Technology Key Laboratory of Coalbed Methane Resources and Reservoiring Process China Ministry of Education Yunnan Bureau of Coal Geological Survey 

出 版 物:《International Journal of Mining Science and Technology》 (矿业科学技术学报(英文版))

年 卷 期:2013年第23卷第2期

页      面:295-301页

核心收录:

学科分类:081901[工学-采矿工程] 0819[工学-矿业工程] 0709[理学-地质学] 0808[工学-电气工程] 08[工学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0807[工学-动力工程及工程热物理] 0815[工学-水利工程] 0813[工学-建筑学] 0814[工学-土木工程] 

基  金:supported by the Key Program of the National Natural Science Foundation of China (No. 40730422) the Key Special Project of the National Science and Technology of China (No.2011ZX05034) the Fundamental Research Funds for the Central Universities of China (No. 2010QNA51) 

主  题:Biologic gases C2+ Microbial degradation Stable isotopes Coalbed gases origin Enhong syncline 

摘      要:Coalbed gases (CBG) in Enhong syncline are characterized by high concentration of C2+ (C2-5 ), with the highest content of ethane over 30%. However, the concentrations of C2+ are not evenly distributed in the syncline. Based on the analysis of δ13C1 , δ13C2 , δ13C3 , δ13CO2 , δDCH4 of CBG and their origin diagrams in the normal and abnormal areas, this research shows that gases in both areas are thermogenic gases and the reason for the uneven distribution of C2+ is that the microbial degradation action on gases is stronger in the normal area than in the abnormal area. The secondary biologic gases in the normal area are mainly characterized by that the carbon isotopes become obviously lighter in methane and become heavier in ethane, whereas the molecular and isotopic compositions of CO2 change little. These features indicate that the secondary biologic gases are mainly generated by the microbial degradation of C2+ , not generated by the reduction of CO2 . The degradation process is selective to make the residual ethane being enriched in 13C and the generated methane rich in 12C.

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