关于不同入水条件的山体滑坡水的故障过程和特征的实验调查
Zhaozhao Liu1, Qun Chen2, Chen Wang1
1State Key Laboratory of Hydraulics and Mountain River Engineering, College of Water Resource and Hydropower, Sichuan University, Chengdu, 610065, Sichuan, China.
Scientific reports
|March 4, 2025
概括
滑坡水侵蚀模式,由流入驱动,显著影响失败. 漏和覆盖侵蚀的结合更具破坏性,对评估和救援工作构成风险.
科学领域:
- 地质技术工程 地质技术工程
- 天然危害 天然危害
- 环境科学 环境科学
背景情况:
- 滑坡水是不稳定的自然形成.
- 上游的流入条件决定了山体滑坡大的故障模式.
- 了解侵蚀模式对于风险评估至关重要.
研究的目的:
- 为了研究不同侵蚀模式下的山体滑坡大故障过程.
- 分析合漏和覆盖侵蚀的影响.
- 为了比较各种输入条件导致的故障特征.
主要方法:
- 进行了物理模型测试,以模拟山体滑坡水侵蚀.
- 控制水位以达到明显的侵蚀模式.
- 监测了故障过程,包括管道,扫和漏洞演变.
主要成果:
- 结合侵蚀涉及管道,斜坡侵蚀,定居点,破裂演变和冲洗.
- 漏时间的增加加剧了斜坡和内部侵蚀.
- 合侵蚀导致水残留体积减少,下游积增加,沉积物运输时间更长.
结论:
- 漏侵蚀改变了内部压力,导致土壤变形,影响了土壤的失败.
- 合侵蚀比快速覆盖或漏引发的故障更有害.
- 调查结果强调了合侵蚀对风险管理构成的风险增加.
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