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浅埋煤层采动导水裂隙动态演化规律模拟分析

Simulation analysis on water conducted porosity dynamic evolution law in shallow depth seam after mining operation

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【作者】 范钢伟张东升卢鑫崔廷锋王晓东

【Author】 FAN Gang-wei, ZHANG Dong-sheng, LU Xin, CUI Ting-feng, WANG Xiao-dong(School of Energy and Safety Engineering, China University of Mining and Technology, Xuzhou 221116, China)

【机构】 中国矿业大学能源与安全工程学院中国矿业大学能源与安全工程学院 江苏徐州221116江苏徐州221116

【摘要】 针对单一关键层浅埋煤层,采用实验室物理模拟揭示了采动导水裂隙动态发育规律。模拟结果表明,采动导水裂隙的演化分为发展期、贯通期和压实闭合期3个阶段;导水裂隙的动态发育受基本顶关键层控制;通过分析得出了防止工作面涌水溃沙的基本原理,能解决西部矿区保水防溃采煤的安全问题。

【Abstract】 According to the shallow depth seam as one single key seam, the lab physical simulation showed the dynamic development law of the water conducted pore after the mining activity. The simulation results showed that the evolution of the water conducted pore after the mining activity could be divided into three phases, such as the development phase, connected through phase and compact closed phase. The dynamic development of the water conducted pore was subjected to the control of the key layer in the basic roof. After the analysis, the basic principle of the water inrush and sand inrush prevention and control in coal mining face was obtained, which would solve the mine safety issue of water conservation and water inrush and inrush prevention in the West China.

【基金】 教育部新世纪优秀人才支持计划(NCET-05-0480)
  • 【文献出处】 煤炭科学技术 ,Coal Science and Technology , 编辑部邮箱 ,2008年05期
  • 【分类号】TD82
  • 【被引频次】34
  • 【下载频次】556
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