首页 | 本学科首页   官方微博 | 高级检索  
     


Geochemical and stable carbon isotopic composition of coal-related gases from the SW Upper Silesian Coal Basin,Czech Republic
Affiliation:1. School of Energy Resource, China University of Geosciences Beijing, 100083, China;2. Coal Reservoir Laboratory of National Engineering Research Center of CBM Development & Utilization, China University of Geosciences Beijing, China;3. Beijing Key Laboratory of Unconventional Natural Gas Geological Evaluation and Development Engineering, China;4. Unconventional Research Institute, Research Institute of Petroleum Exploration and Development, China
Abstract:Gas associated with Carboniferous coal seams and younger Miocene sediments in the SW Upper Silesian Basin in Czech Republic shows wide compositional variation. Coal-related gas extracted from cross-measure degassing boreholes, as well as gas released during canister desorption of coal samples from three different mines was analyzed to evaluate the genetic origin and the influence of sorption/desorption processes on the gas composition. Analyses comprised the compositional and stable carbon and isotope composition of coal-related gases. The isotopic composition of gas from cross-measure boreholes indicates thermogenic origin in the southern part of the basin and microbial CO2 reduction and mixed type origin in the northern part. Gas from canister desorption shows similar origins, but larger compositional and isotopic variation. No consistent isotopic fractionation due to desorption could be observed. Differences in geochemical composition of thermogenic gases could indicate a contribution of gas migrated from deeper formations below the Carpathian overthrust.
Keywords:
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号