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DOI | 10.1306/06071817190 |
A study of hydrogeology and its effect on coalbed methane enrichment in the southern Junggar Basin; China | |
Fu H.; Tang D.; Pan Z.; Yan D.; Yang S.; Zhuang X.; Li G.; Chen X.; Wang G. | |
发表日期 | 2019 |
ISSN | 0149-1423 |
起始页码 | 189 |
结束页码 | 213 |
卷号 | 103期号:1 |
英文摘要 | This paper analyzes regional hydrogeological conditions and divides the study area into three hydrogeological types and seven hydrogeological units, to investigate hydrogeology and its effect on coalbed methane (CBM) enrichment in the southern Junggar Basin, China. From this work, it is found that the groundwater flow paths in the study area are the joint effects of south-to-north and west-to-east flows. This study also shows that microbial gases are widely developed, although the depth limit of microbial gas occurrence is still unclear in the study area. Microbial CO 2 reduction is the leading formation path in the study area, except for the Houxia region, where fermentation is the formation mechanism. The abnormally high CO 2 in stagnant zones (i.e., water flow is slow and stagnant) is mainly associated with methanogenesis, whereas relatively low CO 2 (microbial or thermogenic) is present where water flow is active. The average CBM content within the Xishanyao Formation changes within various hydrogeological units; moreover, the average CBM content within the Badaowan Formation of the same hydrogeological unit (e.g., Fukang) suggests that the hydrogeological and CBM enrichment conditions are different within various structural types. Overall, the hydrogeological conditions exert control on the gas content in the study area; that is, the gas content is high in stagnant zones. Finally, influenced by supplemental microbial gases, changes in the CBMoxidation zone are relatively complex in the study area, the depth of which has no obvious correlation with hydrogeological conditions and changes significantly from west to east. © 2019. The American Association of Petroleum Geologists. |
语种 | 英语 |
scopus关键词 | Carbon dioxide; Coal bed methane; Coal deposits; Firedamp; Groundwater; Groundwater flow; Hydraulics; Hydrogeology; Landforms; Formation mechanism; Formation paths; Gas occurrences; Hydrogeological; Hydrogeological conditions; Methane enrichments; South-to-North; Structural type; Methane; carbon dioxide; coalbed methane; groundwater flow; hydrogeology; oxidation; China; Junggar Basin; Xinjiang Uygur |
来源期刊 | AAPG Bulletin |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/143805 |
作者单位 | Key Laboratory of Tectonics and Petroleum Resources, China University of Geosciences, Ministry of Education, Wuhan, China; Faculty of Earth Resources, China University of Geosciences, Wuhan, China; School of Energy Resources, China University of Geosciences, Beijing, China; Commonwealth Scientific and Industrial Research Organisation Energy Business Unit, Clayton South, VIC, Australia; Coalbed Methane Research and Development Center, Xinjiang Coal Field Geology Bureau, Xinjiang, China; Clean-Seed Energy Limited Liability Company, Urumqi, Xinjiang, China |
推荐引用方式 GB/T 7714 | Fu H.,Tang D.,Pan Z.,et al. A study of hydrogeology and its effect on coalbed methane enrichment in the southern Junggar Basin; China[J],2019,103(1). |
APA | Fu H..,Tang D..,Pan Z..,Yan D..,Yang S..,...&Wang G..(2019).A study of hydrogeology and its effect on coalbed methane enrichment in the southern Junggar Basin; China.AAPG Bulletin,103(1). |
MLA | Fu H.,et al."A study of hydrogeology and its effect on coalbed methane enrichment in the southern Junggar Basin; China".AAPG Bulletin 103.1(2019). |
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