在热水力机械合下,深层岩石的动态损伤特征和能量消耗的多尺度研究
Qi Ping1,2, Bobo Zhang3,4
1School of Civil Engineering and Architecture, Anhui University of Science and Technology, Huainan, 232001, Anhui, China.
Scientific reports
|January 26, 2026
概括
由于热水力机械 (THM) 合和采矿,深地工程面临岩石爆裂风险. 这项研究揭示了THM因素如何影响岩石破裂模式,并介绍了一种经过验证的微裂纹传播模型.
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
- 多物理工程 多物理工程
背景情况:
- 深地工程挖掘容易受到岩石爆破灾害的影响.
- 热水机械 (THM) 合和采矿干扰显著增加了这些风险.
研究的目的:
- 研究THM合在动态负载下对岩石破裂机制的影响.
- 为了描述经过高应变率压缩的岩石中的微观结构和孔隙变化.
- 开发和验证微裂传播的机械模型.
主要方法:
- 使用THM开发的多物理合装置和分裂的霍普金森压力杆进行高应变率压缩实验.
- 使用扫描电子显微镜 (SEM) 和核磁共振 (NMR) 来分析骨折和孔隙结构.
- 构建并验证了滑动微裂传播的机械模型.
主要成果:
- 动态应力-应变曲线显示了一个"塑料平台区域"的非线性行为.
- 通过高斯函数,与水压相关的能量消耗系数.
- 故障模式从压缩剪切演变为断裂故障,随着温度和水压的增加;动态损坏值在0.35-0.36.0之间.
- 显微镜分析表明,从粒际骨折转变为粒际骨折.
- 核磁共振显示,孔隙结构完整性增强,水压升高时孔隙性降低.
结论:
- THM合显著改变岩石断裂模式和微观结构特征.
- 开发的机械模型准确地预测了THM和冲击负载下的微裂纹启动.
- 这些发现为减轻深层土壤工程中的岩石爆破风险提供了关键的见解.
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