刚性与柔性边界下红层岩石的侧限压缩力学特性

    MECHANICAL PROPERTIES OF RED-BED ROCK WITH RIGID AND FLEXIBLE BOUNDARY UNDER LATERAL CONFINING COMPRESSION

    • 摘要: 红层岩体是我国西南地区广泛分布的一类岩体。红层岩体中的滑坡、崩塌等地质灾害十分普遍,掌握红层岩石的力学行为对防止红层滑坡具有重要的意义。基于室内试验与数值模型相结合的方法,以马家沟滑坡红层岩石为研究对象,利用岩样的室内三轴压缩应力-应变曲线校准数值岩样的模型参数。采用颗粒流程序模拟岩样的侧限压缩试验,分析了刚性和柔性边界条件下岩样的应力-应变曲线、泊松比、破坏模式和微观颗粒接触力的差异。结果表明,刚性边界条件对岩样侧向约束较强,岩样弹模、峰值强度随着围压升高增长较柔性边界快。在同围压下,柔性边界条件峰前试样的泊松比变化不大,而刚性边界条件下的试样泊松比在峰前有增大趋势,峰值点处刚性边界条件下的泊松比显著大于柔性边界条件下的岩样。刚性边界条件下的岩样破坏形态常见轴向劈裂、斜对角剪切破坏特征,以张拉和剪切破坏为主。而柔性边界条件下的试样破坏主要表现为试样端部的剪切破坏,破坏试样可观察到明显的侧向鼓胀变形。围压较小时,同应变水平下的柔性边界试样破坏时内部颗粒间的平均剪切应力和平均拉伸应力比刚性边界稍大。围压增加后,柔性边界平均剪切应力和平均拉伸应力显著超过刚性边界,当围压进一步增大时,两种边界条件下的平均剪切应力和平均拉伸应力相近。

       

      Abstract: The red-bed rock mass, prevalent in Southwestern China, often leads to geological hazards like landslides. Understanding its mechanical behavior is crucial for prevention. Through a combination of indoor tests and numerical modeling, the red-bed rocks from the Majiagou landslide area have been extensively studied. Specifically, indoor triaxial compression tests have been conducted to obtain the stress-strain curves of the rock samples. Additionally, numerical rock samples, generated using particle flow code (PFC),have undergone calibration according to experimental results. Based on numerical simulations of lateral confined compression tests, differences in stress-strain curves, poisson's ratios, failure modes, and microscopic particle contact forces of the rock samples have been analyzed under both rigid and flexible boundary conditions. The results indicate that the rigid boundaries strongly constrain rock samples, causing elastic modulus and peak strength to rise rapidly with increased confining pressure. At the same pressure, the Poisson's ratio remains stable for flexible boundary samples pre-peak, but tends to increase for rigid boundary samples. The Poisson's ratio at peak is notably higher under rigid conditions. Rigid boundary samples often fail by axial splitting or diagonal shear, with tension and shear damage prevailing. Flexible boundary samples mainly fail by shear damage, showing lateral dilatation. At lower confining pressures, flexible boundary samples show marginally higher shear and tensile stresses. These stresses significantly surpass those of rigid boundary samples as confining pressure rises, but converge at higher pressures.

       

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