Details

Autor(en) / Beteiligte

• Dou Zhi, Dou Zhi
• Liu Yimin, Liu Yimin
• Zhang Xueyi, Zhang Xueyi
• Wang Yashan, Wang Yashan
• Chen Zhou, Chen Zhou
• Wang Jinguo, Wang Jinguo
• Zhou Zhifang, Zhou Zhifang
• Xiong, Hao

Titel

Influence of layer transition zone on rainfall-induced instability of multilayered slope

Ist Teil von

• Lithosphere, 2021, Vol.2021 (Special 4)

Ort / Verlag

GeoScienceWorld

Erscheinungsjahr

2021

Link zum Volltext

Quelle

EZB Electronic Journals Library

Beschreibungen/Notizen

• Although numerous studies have been paid much attention to rainfall-induced instability of multilayered slopes, the interface between layers is generally considered to be "zero thickness", and the layer transition zone between layers is neglected. In this study, the influence of the layer transition zone on the rainfall-induced instability of multilayered slope was investigated. A model was developed to simulate the rainfall infiltration process, the distribution of pore water pressure, and the stability of multilayered slope by coupling the unsaturated seepage model and the slope stability analysis method. Based on the analysis of the multilayered slopes with the different thickness ratios of the layer transition zone, a method for determining the critical thickness of the layer transition zone was proposed. The results showed that the layer transition zone had a significant influence on the stability of multilayered slope. It was found that the presence of the layer transition zone in the multilayered slope reduced the hydraulic conductivity of the slope and increased the rate of formation of transient saturated zone, which contributed to excess pore water pressure at the toe of the slope. The analysis of the local factor of safety (LFS) showed that when the thickness ratios of the layer transition zone were between 2.5% and 5%, the corresponding hydraulic conductivity of the slope decreased by 1%-2.5% and the maximum failure area of the slope during the rainfall was 25% of the slope. Our study highlighted the importance of the layer transition zone for the rainfall-induced instability of the multilayered slope.