采动应力路径下裂隙砂岩细观力学特性和能量演化特征

    Meso-mechanical properties and energy evolution characteristics of fractured sandstone under mining stress path

    • 摘要: 为了探究裂隙岩体在采动应力路径下的变形破坏特征和能量演化的差异,利用PFC数值模拟对不同裂隙长度和角度的砂岩试样进行了三轴加卸载试验;通过试样的破坏模式来分析试样破坏的原因,通过能量释放系数k来表征储能和耗散之间的转化关系。结果表明:随着裂隙长度的增加,砂岩的峰值强度、弹性模量降低;随着裂隙角度的增加,砂岩的峰值强度、弹性模量先减小后增大;试样破坏产生共面剪切裂纹、抗剪切裂纹、拉伸裂纹、远场拉伸裂纹4种裂纹,剪切裂纹从预制裂隙尖端向端部扩展是试样破坏的主要原因,剪切裂纹与裂隙长度呈现共面−非共面−共面的演化趋势,而与裂隙角度呈现共面−非共面的演化趋势;预制裂隙对周围位移场的影响随裂隙长度的增大而增大,随裂隙角度的增加呈现先增后减的变化;能量释放系数k呈现下降−上升−下降−平稳下降的变化趋势,岩石的破坏强度可通过基于能量演化的峰值应力处的能量系数kc进行评价。

       

      Abstract: In order to explore the differences in deformation failure characteristics and energy evolution of fractured rock masses under the mining stress path, triaxial loading and unloading tests were conducted on sandstone samples with different fracture lengths and angles using PFC numerical simulation. The causes of sample failure are analyzed through the failure modes of the samples, and the transformation relationship between energy storage and dissipation is characterized by the energy release coefficient k. The results show that: with the increase of fracture length, the peak strength and elastic modulus of sandstone decrease, while with the increase of fracture angle, the peak strength and elastic modulus of sandstone first decrease and then increase; four types of cracks, namely coplanar shear cracks, anti-shear cracks, tensile cracks and far-field tensile cracks, are produced during specimen failure, and the main cause of specimen failure is the expansion of shear cracks from the tip to the end of the prefabricated cracks; the shear cracks show an evolution trend of coplanar-non-coplanar-coplanar with the fracture length, while the shear cracks show an evolution trend of coplanar-non-coplanar with the fracture angle; the influence of prefabricated fractures on the surrounding displacement field increases with the increase of fracture length and shows a change of first increasing and then decreasing with the increase of fracture angle; the energy release coefficient k shows a changing trend of decreasing-increasing-decreasing-steady decreasing, and the failure strength of the rock can be evaluated by the energy coefficient kc at the peak stress based on energy evolution.

       

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