Crack propagation laws in sandstone containing elliptical holes under compression-shear loading
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摘要: 为揭示压剪作用下椭圆孔洞砂岩的裂纹扩展规律及其主控因素作用机制,依据室内试验结果,标定砂岩的数值模拟细观力学参数,开展不同孔洞倾角和长短轴比下的压剪数值试验,并对裂纹扩展规律及影响因素作用机制进行分析。研究结果表明:(1)峰值剪切应力、起裂应力及二者差值均随孔洞倾角增大呈先减后增趋势;当孔洞倾角为60°时,三者均达到最小值,试件最易达到破坏状态。(2)平均起裂角随孔洞倾角的增加表现为先增大、后减小、再增大的趋势,并在孔洞倾角为30°,120°时分别取得最大、最小值;起裂角与长短轴比之间未表现出明显相关性。(3)孔洞倾角和长短轴比显著影响裂纹扩展行为,但其作用机制不同。其中,孔洞倾角通过改变应力分布主导裂纹起裂位置和扩展路径,长短轴比通过改变孔洞几何形状影响局部应力状态,进而控制裂纹扩展行为。研究结论可为含孔洞岩体工程稳定性控制与评估提供理论依据。Abstract: To reveal the crack propagation patterns and the underlying mechanisms of controlling factors in sandstone containing elliptical holes under compression-shear loading, mesoscopic mechanical parameters for the sandstone’s numerical model were calibrated based on laboratory test results. Numerical tests under compression-shear loading were conducted for various hole inclination angles and aspect ratios, followed by analysis of crack propagation behavior and the mechanistic effects of influencing factors. The research findings indicate: (1) Peak shear stress, crack initiation stress, and their difference all exhibit a trend of first decreasing and then increasing with increasing pore inclination angle. When the hole inclination angle reaches 60°, all three parameters reach their minimum values, indicating that specimens are most prone to reaching a failure state under this condition. (2) The average crack initiation angle follows a triphasic trend with increasing inclination angle: initial increase, followed by decrease, and final resurgence, reaching maximum (30°) and minimum (120°) values at specific orientations. No significant correlation exists between initiation angles and aspect ratios. (3) While both cavity inclination and aspect ratio significantly govern crack propagation behaviors, their mechanistic controls differ fundamentally. Inclination angle dictates stress redistribution patterns, thereby controlling crack nucleation positions and propagation trajectories. In contrast, aspect ratio modulates localized stress states through geometric confinement effects, ultimately regulating crack evolution dynamics. These findings establish a theoretical foundation for stability assessment and control in cavity-containing rock mass engineering.
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Key words:
- crack propagation /
- sandstone /
- compression-shear loading /
- elliptical holes /
- numerical simulation
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表 1 平行黏结模型宏观参数
Table 1. Macroscopic parameters of parallel bond model
场景 抗压强度/MPa 抗拉强度/MPa 弹性模量/GPa 泊松比 室内试验 71.23 7.08 12.04 0.185 数值模拟 73.24 7.83 11.97 0.185 表 2 平行黏结模型细观参数
Table 2. Mesoscopic parameters of parallel bond model
颗粒参数 取值 黏结参数 取值 颗粒最小半径/mm 0.45 平行黏结弹性模量/GPa 5.5 颗粒最大半径/mm 0.75 平行黏结刚度比 1.6 颗粒密度/(kg∙m−3) 2574 平行黏结法向强度/MPa 15 颗粒摩擦系数 0.5 平行黏结黏聚力/MPa 28 颗粒接触刚度比 1.6 平行黏结内摩擦角/(°) 35 颗粒接触模量/GPa 5.5 平行黏结半径系数 1 表 3 不同倾角α下裂纹扩展模式(k=3)
Table 3. Crack propagation modes under different inclination angles α (k=3)
椭圆孔洞倾角 α=0° α=30° α=60° α=90° α=120° α=150° 





压应力
压应力集中区
拉应力集中区
表 4 不同长短轴比k下裂纹扩展模式(α=30°)
Table 4. Crack propagation mode under different long-short axis ratio k (α=30°)
椭圆孔洞长短轴比 k=1 k=2 k=3 k=4 k=5 k=6 





压应力
压应力集中区
拉应力集中区
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