A Study of the Relationship between Fractal Dimension of Boundary Trace and Stability of the Loess-bedrock Landslide

被引：1
|
作者：
Wu, Bo [1 ]
Zhao, Fa Suo [1 ]
Wu, Shao Yan [1 ]
He, Zi Guang [2 ]
Duan, Zhao [3 ]
机构：
[1] Changan Univ, Sch Geol Engn & Geomat, Xian, Shaanxi, Peoples R China
[2] Huanghuai Univ, Inst Architecture & Engn, Zhumadian, Henan, Peoples R China
[3] Xian Univ Sci & Technol, Xian, Shaanxi, Peoples R China
来源：
2018 INTERNATIONAL CONFERENCE OF GREEN BUILDINGS AND ENVIRONMENTAL MANAGEMENT (GBEM 2018) | 2018年 / 186卷
关键词：
D O I：
10.1088/1755-1315/186/2/012044
中图分类号：
X [环境科学、安全科学];
学科分类号：
08 ; 0830 ;
摘要：
Through the analysis and summary of the characteristics of the boundary trace of the Loess bedrock landslides in the Baota district of Yan' an, it is found that the characteristics are clear and obvious and have some similarity. This paper based on the fractal dimension theory, the fractal dimension of boundary trace of 8 typical loess bedrock landslide in Baota district are calculated by box counting method. A fractal dimension evaluation of landslide steady state model is established by the fractal dimension of the landslide boundary track correlation and stability of landslide. The correctness of the model is Verified through the example. The study shows that the characteristics of the Loess bedrock landslide boundary trajectory can be used to evaluate the stability of the landslides.
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页数：8
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