Stability of Unsaturated Soil Slope Considering Stratigraphic Uncertainty

被引:4
作者
Cao, Wei [1 ,2 ]
Wan, Zheng [2 ]
Li, Wenjing [3 ]
机构
[1] Beihang Univ, Sch Transportat Sci & Engn, Beijing 100191, Peoples R China
[2] North China Inst Sci & Technol, Sch Architectural Engn, Langfang 065201, Peoples R China
[3] Yanching Inst Technol, Sch Architecture, Langfang 065201, Peoples R China
基金
中国国家自然科学基金;
关键词
stratigraphic uncertainty; unsaturated soil; slope stability; coupled Markov chain; groundwater table; finite element; RAINFALL-INDUCED LANDSLIDES; SPATIAL VARIABILITY; RELIABILITY EVALUATION; RANDOM-FIELD; HETEROGENEITY; PERMEABILITY; SIMULATION; FAILURE; MODEL;
D O I
10.3390/su151310717
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Stratigraphic uncertainty is widely present in nature, but it has not been well considered in the stability analysis of unsaturated soil slopes in the past. In this study, the stability of the unsaturated soil slope is evaluated based on borehole data considering stratigraphic uncertainty. Firstly, an enhanced coupled Markov chain model is used to simulate stratigraphic uncertainty. Then, a finite element algorithm for automatically calculating the safety factor (FS) and the average groundwater table (AGT) of the unsaturated soil slope is developed. At last, a hypothetical slope located in the stratum from Perth, West Australia is analyzed using the proposed algorithm under different borehole schemes. The results show that with the increase in the borehole number, the statistics of FS and AGT will not monotonically increase or decrease. But the trend is that the mean values of FS and AGT gradually approach and eventually converge to the real values, and the standard deviations of FS and AGT decrease. There is a linear relationship between the standard deviation of FS (or AGT) and the average information entropy. The FS and AGT are negatively correlated considering stratigraphic uncertainty.
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页数:24
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