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循环荷载作用下红砂岩能量演化特征研究

Energy evolution characteristics of red sandstone under cyclic load

  • 摘要: 岩石是一种非均质、各向异性的天然介质,由随机分布的晶粒和裂隙构成。结合红砂岩单轴循环加卸载试验,重新划分了加卸载过程中的应变能密度的组成,包括塑性应变能密度和弹性应变能密度,后者为裂隙应变能密度与基质应变能密度之和,旨在进一步探索红砂岩在循环荷载作用下的能量演化特征。研究结果表明:①随着应力水平的升高,各应变能均呈指数式增长,弹性应变能占主导,为60%~80%,其中基质应变能基本不低于70%,塑性阶段,二者增速降低;②将整个加卸载过程分为3个应力水平阶段:低于20%应力水平、20%~70%应力水平和大于70%应力水平,与岩石单轴载荷作用下的压密阶段、弹性阶段和塑性阶段具有一致性;③弹性能量指数整体呈先升后降趋势,在65%~75%应力水平时出现最大值,该应力状态下岩石启动岩爆的可能性增加,回弹变形指数整体呈降低—波动—升高—降低的趋势,反映岩石内部基质与裂隙在载荷作用下的变形特征。研究结果可为分析工程岩体稳定性及冲击危险性提供参考。

     

    Abstract: Rock is a heterogeneous and anisotropic natural medium composed of randomly distributed grains and fractures. Combined with the uniaxial cyclic loading and unloading test of red sandstone,the composition of strain energy density during loading and unloading is redefined,including plastic strain energy density and elastic strain energy density. And the latter is the sum of fracture strain energy density and base-material strain energy density. The aim is to further explore the energy evolution characteristics of red sandstone under cyclic load. Studies indicate that: ① With the increase of stress level,the strain energy increases exponentially. And the elastic strain energy dominates,60%-80%,where in the base-material strain energy is not less than 70%. In the plastic stage,their growth rates decrease;② The whole loading and unloading process is divided into three stress level stages:lower than 20% stress level,20%-70% stress level and more than 70% stress level,which is consistent with the rock compaction stage,elastic stage and plastic stage;③ The elastic energy index increases first and then decreases,and the maximum stress level is about 65%-75%. Under this stress state,the possibility of rockburst initiation is increased. And the rebound deformation index generally shows the trend of decreasing,fluctuating,rising and decreasing,reflecting the deformation characteristics of rock internal base material and fracture. The research results can be used as the theoretical basis for analyzing the stability and rockburst risk of engineering rock mass.

     

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