基于 GIS 的皖北朱仙庄煤矿第 10 煤层底板涌水风险评价

Water Supply Pub Date : 2024-04-09 DOI:10.2166/ws.2024.077
Qilin Jiang, Qimeng Liu, Huichan Chai, Xianxiang Hu
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引用次数: 0

摘要

煤层底板石灰岩岩溶涌水问题日益突出,逐渐成为煤矿防治水工作的重点。以朱仙庄煤矿三采区十煤层底板为研究对象,从含水层、隔水层、地质构造等三个方面确定了七项指标作为主要控制因素。采用层次分析法和熵权法确定了主观权重和客观权重,并基于地理信息系统采用脆弱性指数法进行了脆弱性分区评价。根据统计分析计算出的分级阈值,将研究区域划分为五个区。研究表明,太原地层石灰岩岩溶水溃决区自北向东逐渐由安全区向脆弱区过渡。本研究对研究区第十煤层底板太原地层灰岩岩溶涌水具有一定的指导作用。
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GIS-based water inrush risk evaluation of the 10th coal seam floor in Zhuxianzhuang Coal Mine, northern Anhui Province, China
The problem of limestone karst water inrush from coal seam floors is becoming more and more prominent, and gradually becoming the focus of water control work in coal mines. Taking the floor of 10th coal seam in the third mining area of Zhuxianzhuang Coal Mine as the research object, seven indicators were identified as the main controlling factors in three aspects, such as aquifer, water barrier, geological structure. Subjective and objective weights were determined by the analytic hierarchy process and the entropy weighting method, and vulnerability zoning evaluation was carried out based on the geographic information system using the vulnerability index method. The study area was classified into five zones based on the graded thresholds calculated by the statistical analysis. The study shows that the area of Taiyuan Formation limestone karst water outburst gradually transitions from the safe zone to the vulnerable zone from the north to the east. This study has a certain guiding effect on the water inrush of Taiyuan Formation limestone karst from the floor of the 10th coal seam in the study area.
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