在基岩断层移位的影响下对土壤斜坡进行物理模型试验
Yijie Song1,2,3, Jianyi Zhang1,2,3, Jianke Ma1,2,3
1School of Geological Engineering, Institute of Disaster Prevention, Langfang 065201, China.
PloS one
|September 5, 2025
概括
造成山坡不稳定,肩部破裂是最大的威胁. 滑坡的产生包括三个阶段:孕期,发育期和破裂引起的失败期.
科学领域:
- 地质工程
- 地震学
- 地质学
背景情况:
- 基岩断层的移位对邻近岩石和土壤斜坡的稳定性产生了重大影响.
- 了解地震滑坡动态对于斜坡研究的理论进步至关重要.
研究的目的:
- 通过岩石底部断层失调引起的滑坡起源机制和动态特征进行调查.
- 模拟土壤斜坡的地震断层出现并分析故障模式.
主要方法:
- 试验模拟土壤斜坡的地震断层出现.
- 分析两个故障模式:斜肩和脚的破裂.
- 将山体滑坡发生分为三个不同的阶段.
主要成果:
- 斜坡肩部的破裂对土壤斜坡的稳定性构成了比脚破裂更大的威胁.
- 确定了山体滑坡发生的三个阶段:妊娠,发育和破裂诱导的失败.
- 建立了基岩断层移位和表面断裂区域之间的相关性.
结论:
- 这些发现有助于我们更好地了解地震断层失位条件下的坡度稳定性.
- 提供了靠近断层区域的斜坡保护和管理策略的见解.
- 模型测试和现场数据证实了断层移位与山体滑坡位置之间的联系.
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