Landslide Formation Mechanism and its Control Measures in Dabaolang

Abstract:

Through analyzing Dabaoliang geological characteristics, this paper discussed the factors of the mechanism of landslide in Dabaoliang area and simulated its evolutionary process. The paper could get some conclusions, and the factors of landslide are as follow: the stability of the slope which mainly composed by clastic rock not only depended on the performance of the mudstone layer but also the skid resistance of the sliding surface and the shape of slope. Under the influence of regional structure, the joint fissures which developed along the boundary of the landslide will connect the crack and benefit the permeation of the surface water. The heavy rain is one of the main factors caused the slope unstable and sliding. Provide effective prevention and control for prevention and control of projects.

• Periodical: Applied Mechanics and Materials (Volume 722)
• Pages: 419-422
• DOI: https://doi.org/10.4028/www.scientific.net/AMM.722.419
• Online since: December 2014
• Authors: Peng Lv*, Bao Yu Li, Yu Zhang, Yun Xun Zhang
• Keywords: Control Measures, Dabaoliang, Formation Mechanism, Landslide

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