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Drainage feature about coalbed methane wells in different hydrogeological conditions in Fanzhuang area

Drainage feature about coalbed methane wells in different hydrogeological conditions in Fanzhuaug area

作     者:NI Xiao-ming LIN Ran WANG Yan-bin 

作者机构:School of Energy Science and EngineeringHenan Polytechnic UniversityJiaozuo 454000China State Key Laboratory Cultivation Base for Gas Geology and Gas ControlHenan Polytechnic UniversityJiaozuo 454000China College of Geo-science and Surveying EngineeringChina University of Mining&TechnologyBeijing 100083China 

出 版 物:《Journal of Coal Science & Engineering(China)》 (煤炭学报(英文版))

年 卷 期:2012年第18卷第4期

页      面:344-349页

学科分类:081803[工学-地质工程] 0819[工学-矿业工程] 081903[工学-安全技术及工程] 08[工学] 0818[工学-地质资源与地质工程] 

基  金:Supported by the Major Projects of National Science and Technology Project "Development of Coal-bed Gas Dynamic Evaluation Model and Software System" (2011ZX05034-005) the National Natural Science Foundation of China (40902044) 

主  题:coalbed methane hydrogeologicalv condition drainage feature water production Fanzhuang area 

摘      要:It is an important guarantee to enhance the production of coalbed methane (CBM) and reduce the project invest- ment by finding out the drainage feature about CBM wells in different hydrogeological conditions. Based on the CBM explora- tion and development data on the Fanzhuang block in southeast Qinshui Basin and combined with the seepage principle and lithology on the roof and the bottom coalbed, the mathematical model of integrated permeability was established. By perme- ability experiments of the different lithologies on the roof and the floor within the 20 m range combined with the log curves, the integrated permeability of different lithological combinations were obtained. The starting pressure gradient and permeabi- lity of the roof and the floor for different lithologies was tested by "differential pressure-flow method". The relationships be- tween the starting pressure gradient and the integrated permeability were obtained. The critical distance of limestone water penetrating into coal reservoirs was calculated. According to the drainage feature of CBM wells combined with the drainage data of some CBM wells, the results show that, when limestone water can penetrate into coal reservoirs, the daily water production is high and the daily gas production is low although there is no gas at the beginning of the drainage process, the CBM wells stop discharging water within 6 months after the gas began to come out, and the gas production is steadily improved. When limestone water can not penetrate into coal reservoirs, the daily water production is low and the daily gas production is high at the beginning of the drainage process, and it almost stops discharging water after some time when the gas come out, the daily gas production increases, and the cumulative water production is much lower.

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