在单轴压缩下岩石中故障加速的两个典型阶段
Lei Cheng1, Shengwang Hao1, Chunsheng Lu2
1School of Civil Engineering and Mechanics, Yanshan University, Qinhuangdao, 066004, China.
Heliyon
|January 25, 2024
概括
预测岩石断裂是通过结合指数函数和功率定律函数来分析应变加速度来改进的. 与传统的法力分析相比,这种新方法为灾难性事件提供了更早的警告.
科学领域:
- 地质技术工程 地质技术工程
- 材料科学 材料科学 材料科学
- 物理 物理学 物理
背景情况:
- 临界功率定律加速是预测故障时间的验证方法.
- 然而,功率定律行为仅在故障附近观察到,限制其应用到整个加速阶段.
研究的目的:
- 为了研究在单轴压缩下岩石断裂期间平均应变的加速度阶段.
- 通过描述整个加速阶段,开发一种更全面的灾难性故障预测方法.
主要方法:
- 在单轴压缩下对岩石样本进行实验分析.
- 使用指数函数和功率定律函数的组合来建模加速阶段.
- 与实验数据对拟议的预测方法的验证.
主要成果:
- 岩石裂变期间平均应变的加速表现出两个不同的阶段.
- 早期加速阶段跟随时间与故障的指数关系.
- 接近灾难性故障的最后加速度阶段符合关键功率定律趋势.
结论:
- 一个结合的指数和功率定律模型准确地描述了岩石崩的整个加速阶段.
- 这种组合模型使得灾难性故障的预测比单独的权力法更早.
- 拟议的方法为岩石爆发和类似事件提供了更可靠的早期预警系统.
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