龙凤煤矿9号煤层隐伏断层瓦斯响应与渗透率演化识别方法研究

    Study on identification method of gas response and permeability evolution of hidden faults in No.9 coal seam of Longfeng Coal Mine

    • 摘要: 煤矿开采过程中瓦斯事故频发,其中构造区是瓦斯事故的高风险区域,因此精准预测隐伏构造是有效防治煤矿瓦斯突出的关键。为实现对隐伏构造的有效识别,以金沙县林东龙凤煤矿9号煤层为例,综合运用现场监测与实验室试验进行研究。系统收集了120905运输巷、120910回风巷等典型工作面在通过隐伏构造前后的瓦斯体积分数与涌出量动态数据。采集距已知断层不同距离(20、50、100 m)的煤样,利用TAW−2000型岩石三轴试验机,开展不同围压(1~2 MPa)、不同气体压力(1~2 MPa)及不同加载速率(40~80 N/s)条件下的力学−渗流耦合试验,定量分析煤样的强度、变形及渗透率演化特征。结果表明:煤体距断层越近,其结构越破碎,强度越低,渗透率越高,距断层20 m处煤体渗透率约为100 m处的2倍;在所有应力路径下,煤体渗透率均呈现先减小后急剧增大的演化趋势,且距断层20 m处煤样的初始、最小及破坏渗透率平均值为100 m处煤样的2倍,证明近断层煤体具备更强的瓦斯运移能力。现场监测发现,当瓦斯体积分数或涌出量显著异常时,常指示前方存在未揭露构造。基于此,构建了“瓦斯异常响应−渗透性演化识别”综合识别方法,并在掘进工作面成功应用,提升了构造预测精度与瓦斯灾害防控能力。

       

      Abstract: Gas accidents occur frequently in the process of coal mining, and the structural area is a high-risk area of gas accidents. Therefore, accurate prediction of hidden structures is the key to effective prevention and control of coal mine gas outburst. In order to realize the effective identification of concealed structures, this study takes the No.9 coal seam of Longfeng Coal Mine in Lindong, Jinsha County as an example, and comprehensively uses field monitoring and laboratory experiments to study. The system collects the dynamic data of gas volume fraction and emission before and after passing through concealed structures in typical working faces such as 120905 transport roadway and 120910 air roadway. Coal samples with different distances (20 m, 50 m, 100 m) from known faults were collected. The mechanical-seepage coupling tests under different confining pressures (1-2 MPa), different gas pressures (1-2 MPa) and different loading rates (40-80 N / s) were carried out by using TAW-2000 rock triaxial testing machine. The strength, deformation and permeability evolution characteristics of coal samples were quantitatively analyzed. The results show that the closer the coal body is to the fault, the more broken the structure is, the lower the strength is, and the higher the permeability is. The permeability of the coal body at 20 m from the fault is about twice that at 100 m. Under all stress paths, the permeability of coal body shows an evolution trend of decreasing first and then increasing sharply, and the initial, minimum and failure permeability of coal samples at 20 m from the fault is 2 times that of coal samples at 100 m, which proves that the near-fault coal body has stronger gas migration ability. On-site monitoring found that when the gas volume fraction or emission is significantly abnormal, it is often indicated that there is an undisclosed structure in front of it. Based on this, a comprehensive identification method of “gas abnormal response-permeability evolution identification” was constructed and successfully applied in the heading face, which improved the accuracy of structural prediction and the ability of gas disaster prevention and control.

       

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