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李治豪, 陈世江, 杜广盛, 高臻炜, 谷运峰, 刘守彬. 不同围压和水压加载下煤岩渗流规律研究[J]. 煤炭科学技术, 2020, 48(12).
引用本文: 李治豪, 陈世江, 杜广盛, 高臻炜, 谷运峰, 刘守彬. 不同围压和水压加载下煤岩渗流规律研究[J]. 煤炭科学技术, 2020, 48(12).
LI Zhihao CHEN Shijiang DU Guangsheng GAO Zhenwei GU Yunfeng LIU Shoubin, . Research on coal and rock seepage laws under different confining pressures and hydraulic pressures[J]. COAL SCIENCE AND TECHNOLOGY, 2020, 48(12).
Citation: LI Zhihao CHEN Shijiang DU Guangsheng GAO Zhenwei GU Yunfeng LIU Shoubin, . Research on coal and rock seepage laws under different confining pressures and hydraulic pressures[J]. COAL SCIENCE AND TECHNOLOGY, 2020, 48(12).

不同围压和水压加载下煤岩渗流规律研究

Research on coal and rock seepage laws under different confining pressures and hydraulic pressures

  • 摘要: 随着煤炭资源逐步进入深部开采,煤岩的赋存条件异常复杂,严重影响其渗流特性。基于此,研究煤岩在复杂地质条件作用下其渗流特性的变化规律,采用岩石渗透分析仪和核磁共振煤岩孔隙分析系统,进行煤岩试件在不同水压和围压下的加载试验,得到了不同载荷下的渗流量。以此为基础,分别分析计算了渗透率、渗透系数与围压的关系,进而分析了渗流场和应力场的耦合作用。研究结果表明:煤岩受载渗流过程分为3个阶段:非线性阶段、近线性阶段和线性阶段;围压是煤岩渗流主要影响因素,且低围压和高围压下煤岩渗流速度变化规律不同;此次煤岩渗流试验,围压小于4 MPa时,渗流变化量呈指数增长;围压大于4 MPa时渗流变化量呈线性增长;煤岩孔隙变形分3个阶段:孔隙受压急剧变形阶段、孔隙受压缓慢变形阶段和孔隙受压压密阶段。研究结果可为煤层涌水量估算提供参考。

     

    Abstract: As coal resources gradually enter deep mining,the occurrence conditions of coal and rock are extremely complicated,which seriously affects the seepage characteristics. Based on this study,the seepage characteristics of coal and rock under complex geological conditions,the loading tests of coal specimens were perform ed under different hydraulic pressure and confining pressure using rock permeability analyzer and nuclear magnetic resonance. The seepage flow under different loads was calculated. Based on this,the relationship between permeability,permeability coefficient and confining pressure was analyzed and calculated,and then the coupling effect of seepage field and stress field was analyzed. The results show that: The process of coal seepage under load is divided into three stages: nonlinear stage,nearly linear stage and linear stage. Confining pressure is one of the major influencing factors of coal seepage, and the law of seepage velocity of coal is different under low Co nfining pressure and high confining pressure. In this coal seepage test,when the confining pressure is less than 4 MPa,the seepage change increases linearly and when the seepage change is greater than 4 MPa,it is linear. The pore deformation of coal can be divided into three stages ,and they are rapid pore deformation under pressur e,slow pore deformation under pressure and pore compaction. The research results can provide references for coal seam water inflow estimation.

     

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