基于层间摩擦滑动的煤柱冲击地压实验研究

    Experimental study on rock burst of coal pillar based on interlayer friction and sliding

    • 摘要: 冲击地压是矿山动力灾害之一,随着煤矿开采深度的增加,导致冲击地压事故频发,造成大量人员和财产损失。为了防治煤矿冲击地压事故的发生,本文基于岩层之间的摩擦滑动过程,开展煤柱冲击地压实验,探究冲击地压发生机理。通过设计弱夹层组合体煤柱模型,利用数字散斑的相关方法对组合煤柱体单轴压缩过程进行观测分析,研究轴向荷载下组合体煤柱变形场演化特征及层间位移演化过程,探索独立煤柱系统的弹性变形能演化规律。研究结果表明:①优先在弱层结构中形成变形局部化带,且变形局部化带以平行于加载方向优先发育并逐渐扩大,直至贯穿整个弱夹层;②煤柱内岩层交界面处发生摩擦滑动,界面处弱夹层出现剪切变形往复循环现象,致使摩擦系数减小,在一定程度上增强冲击地压发生的可能性;③灾变时上层岩块所积累的弹性势能迅速释放并作用于弱夹层,可加速弱夹层的破坏。

       

      Abstract: Rock burst is one of the mine power disasters.With the increase of coal mining depth, rock burst accidents frequently cause a large number of personnel and property losses.In order to effectively prevent coal mine rock burst accidents and explore the mechanism of rock burst, experimental research on coal pillar rock burst is carried out based on the frictional sliding process between rock strata.The coal pillar model of weak interlayer is designed, and the digital speckle correlation method is used to observe the uniaxial compression process of the combined coal pillar.The evolution characteristics of combined coal pillar deformation field, the evolution process of interlayer displacement, and the evolution law of elastic deformation energy of independent coal pillar system under axial load are studied.The results show that the localized zone is formed preferentially in the weak layer structure, and the localized zone develops preferentially parallel to the loading direction and gradually expands throughout the weak intercalation; frictional sliding occurs at the interface of the rock layer in the coal pillar, which causes the shear deformation of the weak interlayer at the interface to reciprocate, reduce the friction coefficient, and increase the impact strength; at the moment of catastrophe, the elastic energy accumulated in the upper rock block is quickly released and acts on the weak interlayer to accelerate the destruction of the weak interlayer.

       

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