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斜坡的稳定性考虑到多裂在降雨条件下透
Jianqing Jia1, Chengxin Mao2, Victor O Tenorio3
1School of Traffic and Transportation, Lanzhou Jiaotong University, Lanzhou, 730070, China. 19427431@qq.com.
Scientific reports
|May 22, 2024
概括
裂通过加速雨水透,显著影响斜坡的稳定性. 考虑到多裂的透会增加孔隙水压,并影响随时间推移的斜坡位移和稳定性.
科学领域:
- 地质技术工程 地质技术工程
- 水文地质学 水文地质学
- 环境科学 环境科学
背景情况:
- 土壤斜坡上的裂作为雨水透的首选途径.
- 这种透显著改变了斜坡的透场和整体稳定性.
- 了解这些影响对于评估和减轻山体滑坡风险至关重要.
研究的目的:
- 为了研究多裂纹透对斜坡稳定的影响.
- 在降雨条件下,分析裂纹斜坡内透,位移和应力演变的过程.
- 用现场监测数据验证流体结构合模型.
主要方法:
- 相当的透系数方法,使裂土壤均化.
- 开发一个和-不和漏流体结构合模型.
- 对降雨透和地下水位边界条件的分析.
主要成果:
- 多裂的透加快了孔水压,使得土壤表层中的水含量增加.
- 在裂透区内观察到较高的孔水速度.
- 多裂浸的影响随着深度增加和接近地下水位而减少.
- 来自该模型的斜率位移预测与现场观测很好地对齐.
- 降雨持续时间的增加逐渐降低了坡度稳定系数.
结论:
- 多裂的透是影响斜坡水文和稳定的关键因素.
- 已建立的流体结构合模型准确地模拟了降雨下的斜坡行为.
- 雨水透随着时间的推移显著降低了斜坡的稳定性,需要仔细监测和管理.
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