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法向扰动下裂隙砂岩的剪切力学性质与细观演化特征

Shear mechanical properties and microscopic evolution characteristics of fractured sandstone under normal disturbance

  • 摘要: 为探究裂隙岩体在扰动作用下的剪切力学行为和细观演化特征, 开展了恒定作用下裂隙砂岩的直剪试验, 采用PFC2D建立了不同裂隙角度离散元模型, 分析了法向恒定和扰动作用下试样的剪切强度和破坏特征; 基于剪切过程中细观演化规律, 揭示了扰动作用下裂隙砂岩的裂纹扩展规律和能量耗散机理。研究结果表明: ①预制裂隙使岩石剪切强度显著降低, 两种加载模式下不同裂隙角度的剪切强度降幅分别为9.79%~20.28%和11.12%~16.78%; 随着裂隙角度增加, 应力–应变曲线斜率降低, 剪切强度和峰值位移呈现出先增大后减小的趋势, 具有明显的角度效应, 剪切强度与裂隙角度成三次函数关系; 法向扰动削弱了角度效应的影响, 使岩石抵抗剪切变形的能力减弱, 破坏提前。②在剪切过程中, 岩石内部力链呈现出与荷载方向一致的演化趋势, 微裂纹主要从试样两端和预制裂隙两端萌生和发育; 微裂纹倾角主要分布在20°~80°, 破坏后剪切裂纹占比为78%~81%, 扰动作用使该过程中产生的各类裂纹增多, 起裂位移减小, 剪切裂纹占比增大。③AE振铃计数的发展可分为平静期、缓增期、爆发期和稳定期, 扰动作用下“平静期”较短, 且在“缓增期”呈现出阶梯性增长趋势。④扰动作用下的剪切试验, 试样失效点的总能量较低; 直至试样破坏, 大部分输入能都以弹性应变能的形式储存在试样中, 且在扰动作用下的弹性能显著低于恒定作用下的, 降幅达到9.87%~13.94%; 扰动使试样储能能力降低, 耗散能增加, 更容易产生裂纹从而破坏。

     

    Abstract: To study the shear mechanical behavior and micro-evolution characteristics of fractured rock masses under normal disturbance, direct shear tests of fractured sandstone under constant normal stress were carried out, and using PFC2D, discrete element model considering different fracture angles was established to study the shear strength and failure characteristics of the specimen under constant normal stress and normal disturbance. Based on the microscopic evolution laws during the shearing process, the crack propagation pattern and energy dissipation mechanism of fractured sandstone under normal disturbance are analyzed. The results indicate that prefabricated cracks significantly reduce the shear strength of rocks by 9.79%-20.28% and 11.12%-16.78% for different crack angles under two loading modes. As the crack angle increases, the slope of the stress-strain curve decreases, and shear strength and peak strain exhibit a first increase and then decrease trend, showing a clear angle effect. Shear strength and crack angle have a cubic function relationship. Normal disturbance weakens the influence of angular effects, and accordingly the ability of the rock to resist shear deformation is weakened and damage is advanced. During the shearing process, the internal force chain of the rock exhibits an evolving trend consistent with the direction of the load, and microcracks mainly arise and develop from both ends of the specimen and the ends of the prefabricated cracks. Microcracks are mainly distributed at angles between 20° and 80°, with shear cracks accounting for 78% to 81% after failure. The disturbance causes an increase in the number of different types of cracks, the initiation displacement decreases and the proportion of shear cracks increases. The development of acoustic emission ringing count can be divided into four stages: calm, slow increase, outbreak and stable periods. Under the disturbance, the “calm period” is shorter, and a stepwise increasing trend appearred during the “slow increase period”. The total energy at the failure point of the specimen is lower in the shear test under normal perturbation. Most of the input energy is stored in the sample in the form of elastic strain energy until the sample is destroyed, and the elastic energy under the normal disturbance is significantly lower than constant normal stress effect, with a reduction of 9.87% to 13.94%. The disturbance reduces the energy storage capacity of the sample, increases dissipation energy, facilitating crack formation and ultimate failure.

     

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