A physical model considered the effect of overland water flow on rainfall-induced shallow landslides

被引：0

作者：

Luo Y. ^{[1
]}

He S.-M. ^{[1
,2
]}

Chen F.-Z. ^{[3
]}

Li X.-P. ^{[1
]}

He J.-C. ^{[4
]}

机构：

[1] Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu

[2] Center for excellence in Tibetan plateau earth sciences, China academy of sciences, Beijing

[3] College of Water Conservancy and civil Engineering, South China Agricultural University, Wushan road, Guangzhou, 510642, Tianhe

[4] Southwest Municipal Engineering Design & Research Institute of China, Chengdu

来源：

Geoenvironmental Disasters | / 2卷 / 1期

基金：

中国国家自然科学基金; 中国科学院西部之光基金;

关键词：

Hillslope hydrology; Overland water flow; Rainfall; Shallow landslide; Slope stability;

D O I：

10.1186/s40677-015-0017-6

中图分类号：

学科分类号：

摘要：

Background: It is well know that many shallow landslides are triggered by rainfalls. In previous studies of shallow landslide models, the effect of overland water flow on slope stability was ignored. Results: In this paper, a physical model considered the effect of overland water flow on rainfall-induced shallow landslides is derived and applied to predict the landslides. The slope stability model is developed by considering the depth of overland water flow in infinite slope stability theory. Hillslope hydrology is modelled by coupling the overland uniform water flow equation with Rosso’s seepage flow equation. And then, the model is used to assess the slope stability in Dujiangyan of China, and the results is compare with Rosso’s model. Conclusions: This model is simple, but has the capability of taking into account the effect of overland water flow in the triggering mechanism of shallow landslide. The results of case study show that the overland water flow can make an obvious effect on shallow landslides, so it is quite important to consider the overland water flow in shallow landslide hazard assessment. © 2015, Luo et al.; licensee Springer.

引用

共 25 条

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