煤炭工程 ›› 2025, Vol. 57 ›› Issue (8): 161-170.doi: 10. 11799/ ce202508022

• 研究探讨 • 上一篇    下一篇

沁水盆地东北部煤层气地质特征及有利区划分

傅永帅,杨丽兵   

  1. 黑龙江科技大学 矿业工程学院,黑龙江 哈尔滨 150022

  • 收稿日期:2025-02-17 修回日期:2025-06-25 出版日期:2025-08-11 发布日期:2025-09-11
  • 通讯作者: 傅永帅 E-mail:18834388157@163.com

Geological characteristics and favorable area division of coalbed methane in northeast Qinshui Basin

  • Received:2025-02-17 Revised:2025-06-25 Online:2025-08-11 Published:2025-09-11

摘要:

为了助力沁水盆地东北部煤层气高效勘探开发,收集了区域内31个矿井的煤储层厚度与埋深,通过等温吸附试验、压力恢复曲线法、计算推导和孔渗特征实验手段,测定了矿井煤样的兰氏压力、储层压力、含气量、渗透性、含气饱和度、临界解吸压力及孔隙率等参数,结合构造、水文地质背景系统地分析了研究区煤层气地质特征,并从煤层气富集因素的角度出发,建立多层次煤层气开发选区评价指标体系,进行了二级指标敏感性分析,且在研究区太原组15号煤层开展应用,划分了煤层气开发有利区块。结果表明:该区域15号煤层变质条件较高,顶底板以灰岩、砂质泥岩与泥岩为主,煤层厚度在4.30~8.25m之间, 平均埋深389m,属于中~浅埋深,储层压力较小,平均0.67MPa,含气量在2.61~19.50m3/t之间,平均含气量9.37m3/t,吸附能力强,兰氏压力平均36.65m3/t,渗透性与孔隙率较差,平均渗透性0.029mD,平均孔隙率5%;煤层气富集主要受煤层埋深控制,相较浅部,深部煤储层煤层厚度,孔隙率变化不大,而兰氏压力高,渗透率低,储层压力、含气性大,更有利于煤层气储存;将研究区煤层气开发潜力划分为5类,其中和顺、寿阳与阳泉区域是研究区勘探开发优势区块;兰氏压力、渗透率、含气饱和度与临界解吸压力等参数较低,是未来煤层气开发的主要不利因素。

关键词:

沁水盆地 , 煤层气 , 模糊综合评价 , 煤储层特征 , 潜力评价

Abstract:

In order to improve the degree of CBM exploration and development in the northeast of Qinshui Basin, the coal reservoir thickness and buried depth of 31 mines in the region were collected, and the a and b values, reservoir pressure, gas content, permeability, gas saturation, critical desorption pressure and porosity of coal samples were measured by isothermal adsorption test, pressure recovery curve method, calculation deduction and porosity test. Based on the structural and hydrogeological background, this paper systematically analyzes the CBM geological characteristics and the law of accumulation and accumulation in the study area, and establishes a multi-level CBM development selection evaluation index system from the perspective of CBM enrichment factors, and carries out application in the No.15 coal seam of Taiyuan Formation in the study area, and divides the favorable CBM development blocks. The results show that: No. 15 coal seam in this area has higher metamorphic conditions, with sandy mudstone and mudstone as the main surface and roof. The thickness of coal seam is between 4.30 and 8.25 m, and the average burial depth is 389 m, which belongs to medium-shallow burial depth. The average gas content is 9.37 m3/t, the adsorption capacity is strong, the average Langley pressure is 36.65 m3/t, the average permeability and porosity are poor, the average permeability is 0.029 mD, the average porosity is 5%; Coal seam gas enrichment is mainly controlled by the depth of coal seam. Compared with shallow coal seam, the thickness and porosity of deep coal reservoir have little change, and the coal reservoir pressure, gas content and Langley pressure are higher, so they have better coal seam gas storage capacity. The CBM development potential in the study area is divided into 4 categories, among which the deep buried coal seams in Pingxi and Yangquan areas are the dominant exploration and development blocks. Low Langley pressure, permeability, gas saturation and critical desorption pressure are the main disadvantages of future CBM development. The research has a certain guiding significance to the exploration and development practice of coalbed methane in the northeast of Qinshui Basin.

中图分类号: