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Rainfall-induced landslide stability analysis in response to transient pore pressure ―A case study of natural terrain landslide in Hong Kong

机译:瞬态孔隙压力对降雨诱发滑坡稳定性的影响-以香港自然地形滑坡为例

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摘要

Transient pore pressure in response to short intense rainfall process plays an important role in shallow landslide occurrence. Using GIS technology, we carry out the rainfall-induced landslide stability analysis in response to transient pore pressure by means of transient and unsaturated rainfall infiltration modeling. A case study is performed on the shallow landslide stability analysis in Hong Kong. Detailed analysis and discussion reached some useful conclusions on the tempo-spatial behavior and characteristics of slope stability response and pore pressure response to typical rainfall process. Comparison analysis is performed on some important issues including landslide stability response in different types of slopes with different hydraulic properties, antecedent rainfall and landslide stability, and the nature of pore pressure response time. These studies might give us an important insight into landslide tringgering mechanism and the hydrological process in response to rainfall, and provide systematic information and evidences for effective risk assessment and warning system establishment.
机译:响应短时强降雨过程的瞬时孔隙压力在浅层滑坡发生中起重要作用。利用GIS技术,我们通过瞬态和非饱和降雨入渗模型对瞬态孔隙压力进行降雨诱发的滑坡稳定性分析。以香港浅层滑坡稳定性分析为例。对典型降雨过程的边坡稳定响应和孔隙压力响应的时空行为和特征进行了详细的分析和讨论,得出了有益的结论。对一些重要问题进行了比较分析,包括不同类型的具有不同水力特性的边坡的滑坡稳定性响应,前期降雨和滑坡稳定性以及孔隙压力响应时间的性质。这些研究可能使我们对滑坡颤动机理和响应降雨的水文过程有重要的了解,并为有效的风险评估和预警系统的建立提供系统的信息和证据。

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