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Experimental test method for subcritical propagation rate of rock fractures based on triaxial stress—strain curve

机译:基于三轴应力 - 应变曲线的岩骨折亚临界传播速率的实验试验方法

摘要

The invention discloses an experimental test method for subcritical propagation rate of rock fractures based on triaxial stress-strain curve, including: Step 1: preparing test sample core for experiment; Step 2: putting core into triaxial rock mechanics test system, applying constant radial confining pressure to core, and applying axial stress in the axial direction until the core is macroscopically damaged; recording experimental parameters of axial stress, strain and corresponding loading time of the core; Step 3: drawing stress-strain curve of the test core according to detection data points of axial stress and axial strain; Step 4: in the stress-strain curve of the test core, starting time and ending time of the subcritical propagation stage of fractures inside the core correspond to the initiation stress σci and damage stress σcd, respectively, and calculating subcritical propagation rate of the subcritical fracture propagation stage of the test core.
机译:本发明公开了一种基于三轴应力 - 应变曲线的岩骨折亚临界传播速率的实验试验方法,包括:步骤1:制备试验试验样品核心;步骤2:将核心放入三轴岩石力学测试系统,将恒定的径向限制压力施加到芯,并在轴向上施加轴向应力,直到芯宏观损坏;记录轴向应力,应变和芯的相应加载时间的实验参数;步骤3:根据轴向应力和轴向应变的检测数据点,拉伸测试核的应力 - 应变曲线;步骤4:在测试核心的应力 - 应变曲线中,核心内部骨折的亚临界传播阶段的开始时间和结束时间对应于起始应力σci和损伤应力σcd,并计算亚临界的子临界传播速率测试核心的断裂传播阶段。

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