首页|期刊导航|矿业科学学报|煤矿地下水库下压煤层开采中层间岩体裂隙网络的拓扑演化分析

煤矿地下水库下压煤层开采中层间岩体裂隙网络的拓扑演化分析OA

Underground reservoirs-belowed coal mining-induced topological evolution of fracture networks in rock interlayer

中文摘要英文摘要

在地下水库下压煤层开采过程中,层间岩体受到开采扰动影响发生变形破坏,其裂隙的扩展贯通威胁到地下水库的安全.文中以神华大柳塔煤矿大柳塔井 2-2 与 5-2 煤层工作面为原型,开展物理相似模拟试验,分析下压煤层开采过程中层间岩体的应力与裂隙演化规律.通过将裂隙划分为迹线和段线,分析开采过程中裂隙拓扑几何特征的演化过程.基于裂隙平均连接数绘制裂隙三相图定量评价裂隙连通性.结果表明,随着下压煤层开采工作面的推进,层间岩体经历非线性增压、突降卸压和应力波动 3 个阶段,层间岩体裂隙在产生后持续张开,达到最大值后转而趋于闭合.随着开采推进,迹线、段线及节点数均呈增大趋势,其中最长迹线通常是水平离层裂隙.在裂隙演化过程中,裂隙网络主要以连通簇的形式向外蔓延,且其空间分布具有延续性.研究成果可为煤矿地下水库下压煤层开采的安全距离计算,以及层间岩体安全性评价提供依据与参考.

During the mining of lower coal seams beneath underground reservoirs,the interlayer rock mass undergoes deformation and failure due to mining-induced disturbances.Crack propagation and in-terconnection pose significant threat to reservoir safety.Taking the working faces of 2-2 and 5-2 coal seams in Shenhua Daliuta Mine as prototypes,this study conducted physical similarity simulation exper-iments to analyze stress and crack evolution patterns in interlayer rock masses during lower seam extrac-tion.We classified fractures into trace lines and segment lines to investigate the evolution of their topol-ogical and geometric characteristics.A three-phase diagram of fractures was established based on aver-age connection numbers to quantitatively evaluate connectivity.Results indicate that as mining ad-vanced,the interlayer rock mass experienced a nonlinear increase in pressure,followed by sudden pressure relief and stress fluctuations.Cracks continued to expand until reaching a maximum aperture before closing.The number of nodes in trace lines and segment lines increased with mining advance-ment,with the longest trace line typically being a horizontal bedding separation fracture.During evolu-tion,fracture networks predominantly propagated as connected clusters while maintaining spatial conti-nuity.This study provides a method for calculating the safety distance of coal seam mining beneath un-derground reservoirs and evaluating the safety of interlayer rock masses in coal mines.

程建超;欧阳迪;侯孟冬;王琪;王路军;刘殷彤;刘升贵;杨晓峰;薛东杰

北京低碳清洁能源研究院煤炭开采水资源保护与利用全国重点实验室,北京 102211||中国矿业大学(北京)力学与土木工程学院,北京 100083||中国矿业大学(北京)隧道工程灾变防控与智能建养全国重点实验室,北京 100083中国矿业大学(北京)力学与土木工程学院,北京 100083中国矿业大学(北京)力学与土木工程学院,北京 100083中国矿业大学(北京)力学与土木工程学院,北京 100083北京低碳清洁能源研究院煤炭开采水资源保护与利用全国重点实验室,北京 102211中国矿业大学(北京)力学与土木工程学院,北京 100083中国矿业大学(北京)力学与土木工程学院,北京 100083北京理工大学宇航学院,北京 100081北京低碳清洁能源研究院煤炭开采水资源保护与利用全国重点实验室,北京 102211||中国矿业大学(北京)力学与土木工程学院,北京 100083||中国矿业大学(北京)隧道工程灾变防控与智能建养全国重点实验室,北京 100083

矿业与冶金

地下水库层间岩体相似模拟裂隙演化拓扑演化

underground reservoirsinterlayer rocksimilar simulationcrack evolutiontopological evolution

《矿业科学学报》 2026 (1)

241-252,12

煤炭开采水资源保护与利用国家重点实验室开放基金(GJNY-20-113-04)地球深部探测与矿产资源勘探国家重大科技专项(2024ZD1003902)国家自然科学联合基金(U21B2072)隧道工程灾变防控与智能建养全国重点实验室开放基金重点课题(XD2025007)

10.19606/j.cnki.jmst.2025063

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