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形态演变表明压力干扰在平行骨折中的转化
Qianlong Zhou1, Xiaodong Hu2, Shaobo Han3
1College of Artificial Intelligence, China University of Petroleum, Beijing, Beijing, 102249, Beijing, China.
Scientific reports
|January 8, 2026
概括
这项研究揭示了应力干扰如何影响地质材料中的断裂传播. 一个新的实验量化了这种相互作用,显示了一个过渡区,并定义了一个应力干扰因子 (β),以更好地评估工程稳定性.
科学领域:
- 地质物理学 地质物理学
- 地质工程是地质工程.
- 材料科学 是一种材料科学.
背景情况:
- 断裂传播在自然层和地质工程中至关重要.
- 以前的研究集中在单一骨折上,忽视了压力干扰效应.
- 了解应力干扰是工程稳定性和设计的关键.
研究的目的:
- 调查骨折形态与应力干扰之间的动态相关性.
- 量化应力干扰对断裂传播的影响.
- 开发一种应力干扰的分析模型.
主要方法:
- 创新的镜面对称双重断裂实验.
- 光衰减技术用于量化形态演变.
- 在骨折停滞事件期间进行能量平衡分析.
主要成果:
- 根据应力干扰水平确定了不同的传播区域.
- 当断裂半径接近断裂间距时观察到区域过渡.
- 定义并建模了与实验数据一致的应力干扰因子 (β).
- 发现能量分区 (储存与消散) 与断裂半径不同,影响停滞.
结论:
- 压力干扰显著影响骨折形态和传播动态.
- 为应力干扰因子 (β) 开发的分析模型提供了定量见解.
- 了解停滞期间的能量动态对于预测地质工程中的断裂行为至关重要.
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