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采动裂隙网络实时演化及连通性特征
引用本文:高明忠,金文城,郑长江,周宏伟.采动裂隙网络实时演化及连通性特征[J].煤炭学报,2012,37(9):1535-1540.
作者姓名:高明忠  金文城  郑长江  周宏伟
作者单位:1.四川大学 水力学与山区河流开发保护国家重点实验室 水利水电学院,四川 成都 610065;; 2.中国平煤神马集团 能源化工研究院,河南 平顶山 467000
基金项目:国家重点基础研究发展计划(973)资助项目,国家自然科学基金资助项目
摘    要:以平顶山煤业集团八矿己15-14120采煤工作面为试验基地,借助改进后的本质安全型钻孔裂隙窥视仪,实时采集采煤工作面前方煤岩体裂隙网络随工作面推进的演化过程。结合分形几何理论与裂隙岩体连通率投影算法,揭示了采动影响下,工作面前方裂隙网络演化分形特征及连通率变化规律。结果表明:采动对平煤八矿己15-14120采煤工作面上覆岩层裂隙网络沿开采方向的影响范围约为50 m;随着工作面不断接近试验测点,煤岩体采动裂隙网络分形维数总体呈上升趋势,并与矿压分布有较好的对应关系;同时,煤岩体连通率随采煤工作面推进上升趋势明显,可依次分为线性缓慢增长阶段、指数增长阶段及平稳阶段。

关 键 词:裂隙网络  演化特征  连通率  分形维数  现场实验  
收稿时间:2012-06-01

Real-time evolution and connectivity of mined crack network
GAO Ming-zhong,JIN Wen-cheng,ZHENG Chang-jiang,ZHOU Hong-wei.Real-time evolution and connectivity of mined crack network[J].Journal of China Coal Society,2012,37(9):1535-1540.
Authors:GAO Ming-zhong  JIN Wen-cheng  ZHENG Chang-jiang  ZHOU Hong-wei
Affiliation:1.State Key Laboratory of Hydraulics and Mountain River Engineering,College of Hydraulic and Hydropower Engineering,Sichuan University,Chengdu 610065,China;2.Energy & Chemical Industry Research Institute,Shenma Group of Pingdingshan Coal Group,Pingdingshan 467000,China;3.State Key Laboratory of Coal Resources and Safe Mining,China University of Mining and Technology(Beijing),Beijing 100083,China)
Abstract:Based on the field conditions of coal mining face No.15-14120 at No.8 Mine of Pingdingshan Coal Mining Group,the information for real time evolution of coal rock crack network with advancement of working face was collected by using improved intrinsically safe borehole video instrument.Fractal theory and projective arithmetic for the two dimensional connectivity of cracked rock mass were employed to characterize the evolution of crack network and variation of connectivity caused by mining.The results show that the influenced domain of crack network ahead of the working face is 50 m approximately in the condition of coal mining face No.15-14120 at No.8 Mine of Pingdingshan Coal Mining Group,and the calculated fractal dimension of crack network increases as the distance between the monitoring hole and the mining face decreases,which exhibites a good agreement with the variation of pressure at overburden strata.Moreover,the calculated connectivity of mining induced crack network increases obviously with the advancing of mining face and the increasing process can be divided into linear phase,exponential phase and constant phase.
Keywords:crack network  evolution characteristics  connectivity  fractal dimension  in-situ experiment
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