王云飞, 王立平, 焦华喆, 赵洪波. 不同围压下砂岩的变形力学特性与损伤机制[J]. 煤田地质与勘探, 2015, 43(4): 63-68. DOI: 10.3969/j.issn.1001-1986.2015.04.014
引用本文: 王云飞, 王立平, 焦华喆, 赵洪波. 不同围压下砂岩的变形力学特性与损伤机制[J]. 煤田地质与勘探, 2015, 43(4): 63-68. DOI: 10.3969/j.issn.1001-1986.2015.04.014
WANG Yunfei, WANG Liping, JIAO Huazhe, ZHAO Hongbo. Mechanical charactristics of deformation and damage mechanism of sandstone under different confining pressure[J]. COAL GEOLOGY & EXPLORATION, 2015, 43(4): 63-68. DOI: 10.3969/j.issn.1001-1986.2015.04.014
Citation: WANG Yunfei, WANG Liping, JIAO Huazhe, ZHAO Hongbo. Mechanical charactristics of deformation and damage mechanism of sandstone under different confining pressure[J]. COAL GEOLOGY & EXPLORATION, 2015, 43(4): 63-68. DOI: 10.3969/j.issn.1001-1986.2015.04.014

不同围压下砂岩的变形力学特性与损伤机制

Mechanical charactristics of deformation and damage mechanism of sandstone under different confining pressure

  • 摘要: 开展不同围压下砂岩的强度、变形和损伤演化研究,对岩体工程的结构设计和稳定性评价具有重要意义。对赵固一矿二1煤层顶板砂岩进行试验获得其力学参数,并采用颗粒流程序获得砂岩细观力学参数,结合编制的fish语言程序进行试验,研究砂岩在不同围压的强度、变形和损伤演化机制,得到如下结论:随着围压增加砂岩的屈服段变长,围压小于40 MPa时峰值强度随围压变化敏感,大于40 MPa时敏感性降低,随着围压增加砂岩由脆性破坏逐步转变为延性破坏;砂岩的扩容经历线性体缩、线性扩容和非线性扩容3个阶段,围压增大线性扩容阶段缩短而非线性扩容阶段增加,扩容指数和扩容起始点轴向应变与围压存在指数变化规律;砂岩的损伤破坏经历损伤弥散分布、聚集成核、形成局部裂隙和主控破裂面形成4个阶段,低围压下砂岩沿单一主控破裂面发生压剪破坏,高围压下主控破裂面呈X型交叉破坏岩体,为X型共轭斜面剪切破坏形式。

     

    Abstract: The sandstone of the roof of coal seam 21 in Zhaogu mine was tested under uniaxial compression to obtain its mechanical parameters. The meso-mechanical parameters were got by Particle Flow Code(PFC), in combination with fish program, the test was conducted to study sandstone strength, deformation characteristics and damage mechanism under different confining pressures. It is concluded that the sandstone yield stage increases with the increase of confining pressure, the variation of peak strength with confining pressure is more sensitive under 40 MPa confining pressure, the sensitivity is reduced when confining pressure is greater than 40 MPa. As the confining pressure increases, sandstone failure mode gradually changes from brittle model into ductile failure; sandstone volumetric strain experiences three stages:linear compression, linear expansion and nonlinear expansion. The linear expansion stage shortens and the nonlinear expansion stage lengthens with confining pressure. There is a exponential variation among dilatation index, the axial strain of initial point and confining pressure. Sandstone damage evolution in failure process is divided into four stages:dispersion distribution, damage gathered in some zone, formation of local fractures and formation of rupture surface. Sandstone is destroyed in compression and shear mode along the single rupture surface under lower confining pressure, and destroyed in X shearing failure mode under higher confining pressure.

     

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