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综放采动应力路径下单裂隙砂岩力学特性试验研究

Experimental study on mechanical properties of sandstone with single fracture under fully-mechanized top-coal caving mining stress path

  • 摘要: 综放开采会形成有别于常规三轴压缩的应力路径,为研究综放采动状态下顶板岩体的力学特性,针对特定长度和角度的单裂隙砂岩,进行恒定卸围压同时变速率加轴压的加卸载三轴试验,以模拟综放开采过程中的应力路径,分析单裂隙砂岩的破坏形式,并用超声波实时测试,探究超声波特性和应力应变的关系以及裂纹演化规律。试验结果表明:①常规三轴应力路径下,不同长度单裂隙砂岩试件的破坏形式基本为拉-剪复合型破坏,不同角度单裂隙砂岩试件破坏形式包含纯剪切破坏、拉伸破坏、拉-剪复合破坏和X型共轭剪切破坏。加卸载三轴应力路径下,随着裂隙长度增加,破坏形式表现为拉-剪复合型破坏—“X”型非共面剪切破坏—“X”型共面剪切破坏,拉伸裂纹会被次生共面裂纹所替代;裂隙角度是裂隙起裂的诱因,不同角度裂隙砂岩试件破坏形式包含拉-剪复合型破坏、单剪切破坏、“X”型非共面剪切破坏;②P波波速能有效反映试件应力水平和细观结构。相较于常规三轴应力路径下整体上P波速度随轴向应变的增大先增大后减少,在加卸载三轴应力路径下,整体上P波速度随轴向应变的增大而增大,但增速随着应力水平的增加而减小;在试件达到屈服点时,试件密度达到最大值,表现为P波波速达到最大值;在试件达到峰值强度附近时,试件内部裂纹交叉和相互联合的现象加剧,表现为P波波速出现明显波动;裂隙长度增大,波速稳定段逐渐减小,裂隙角度增大,波速稳定段先增大后减小;③根据波速反映的裂纹宽度变化,常规三轴应力路径下裂纹演化阶段可分为裂纹压密阶段、裂纹发展阶段、裂纹稳定阶段和破坏后失稳阶段4个阶段,加卸载三轴应力路径下则分为裂纹压密阶段、裂纹稳定阶段和裂纹扩展阶段3个阶段,裂纹稳定阶段随裂隙长度增加整体上呈现减小趋势,裂隙角度对裂纹稳定阶段基本没有影响。

     

    Abstract: In the process offully-mechanized top-coal caving, the stress path is different from the conventional triaxial compression. In order to study the mechanical properties of roof rock mass under fully-mechanized top-coal caving mining compared with conventional triaxial compression, for single fissure sandstone with specific length and angle, carry out the loading and unloading triaxial tests of constant unloading confining pressure and variable rate loading axial pressure to simulate the stress path in fully-mechanized top-coal caving mining process, analyze the failure form of single fissure sandstone, study the relationship between ultrasonic characteristics and stress-strain and the law of crack evolution by real-time ultrasonic testing. The results show that:①Under the conventional triaxial stress path, the failure mode of single fissure sandstone specimen with different lengths is basically tensile shear composite failure, and the failure mode of single fissure sandstone specimen with different angles includes pure shear failure, tensile failure, tensile shear composite failure and X-type conjugate shear failure. Under the loading and unloading triaxial stress path, with the increase of crack length, the failure mode is tension shear composite failure -“X” non-coplanar shear failure -“X” coplanar shear failure, and the tensile crack will be replaced by secondary coplanar crack; the fracture angle is the inducement of crack initiation, the failure modes of sandstone specimen with different angles include tensile shear composite failure, single shear failure and X-type non-coplanar shear failure. ②P wave velocity can effectively reflect the stress level and microstructure of the specimen. Compared with the results that the overall P-wave velocity first increases and then decreases with the increase of axial strain under the conventional triaxial stress path, under the loading and unloading triaxial stress path, the overall P-wave velocity increases with the increase of axial strain, while the growth rate slows down with the increase of stress level; when the specimen reaches the yield point, the specimen density reaches the maximum and the P-wave velocity reaches the maximum; when the specimen reaches the peak strength, the phenomenon of internal crack crossing and mutual combination intensifies, the P wave velocity fluctuates obviously; with the increase of fissure length, the P wave velocity stable section decreases gradually, with the increase of the fissure angle, the P wave velocity stable section increases first and then decreases. ③According to the change of crack width reflected by P wave velocity, the crack evolution stage under conventional triaxial stress path can be divided into four stages:crack compaction stage, crack development stage, crack stability stage and post failure instability stage. While under loading and unloading triaxial stress path, it can be divided into three stages:crack compaction stage, crack stability stage and crack propagation stage. The crack stability stage decreases with the increase of fissure length, and the fissure angle has almost no effect on the crack stability stage.

     

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