关于破裂砂岩对中间主应力加上毛孔压力的反应的实验研究
Qinming Liang1,2, Gun Huang1,2, Jie Zheng3
1State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400044, China.
ACS omega
|May 20, 2024
概括
介质主应力 (σ2) 影响破裂岩石裂变和水扩散. 较高的σ2最初会加强岩石,然后削弱它,增加地下工程中的水冲入风险.
科学领域:
- 地质技术工程 地质技术工程
- 岩石机械学 岩石机械学
- 水文地质学 水文地质学
背景情况:
- 在复杂的压力和孔隙压力条件下,地下破裂岩石质量容易发生故障.
- 这些故障对地下工程项目的人员和运营安全构成重大风险.
研究的目的:
- 为了研究中间主应力 (σ2) 在破裂岩石破裂期间对机械行为和体积变化 (ΔV) 的影响.
- 了解压力条件与破碎岩石质量中的水扩散特征之间的关系.
主要方法:
- 在破裂的砂岩样本上进行了真正的三轴强度实验.
- 在整个实验中保持稳定的孔隙压力.
- 测量了裂纹启动应力 (σci),裂纹损伤应力 (σcd),峰值应力 (σ1,峰值) 和体积变化 (ΔV) 在不同的σ2.2.下.
主要成果:
- 岩石强度 (σci, σcd, σ1,峰值) 最初增加,然后随着 σ2.2 的上升而下降.
- 体积变化 (ΔV) 呈现了反向趋势,首先下降,然后随着σ2的增加而增加.
- 观察到岩石强度和在升高 σ2.2 的情况下的 ΔV 之间的反向关系.
结论:
- 中间主应力显著影响破裂岩石中的故障机制和水扩散.
- 升高的σ2可以降低岩石强度,可能增加ΔV和水冲入灾害的风险.
- 这些发现为提高岩石质量的稳定性和减轻地下工程中的水冲入提供了理论基础.
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