›› 2013, Vol. 34 ›› Issue (S1): 252-258.

• Geotechnical Engineering • Previous Articles     Next Articles

Analysis of formation mechanism and three-dimensional stability of large scale terrace of earthquake landslide

DONG Jin-yu1,WANG Dong2,YANG Ji-hong1,HUANG Zhi-quan1   

  1. 1. College of Resources and Environment, North China University of Water Resources and Electric Power, Zhengzhou 450011, China; 2. College of Civil Engineering, Shijiazhuang Tiedao University , Shijiazhuang 050043, China
  • Received:2013-05-10 Online:2013-08-30 Published:2014-06-09

Abstract: Through in-situ investigation, the terrace model of Duba river is generalized. According to the geomorphic characteristics and hydrogeological investigation, Chenjiaba seismically induced landslide is located on the terrace the river; sliding surface is formed by long-term immersion of groundwater. Geological structures of sliding mass and the residua on terrace as well as the attitude of bedrock exposed at the front and posterior margin of the landslide are compared respectively; so failure mode of this landslide is determined; while the severe earthquake occurred, silty clay of the sliding surface are weakened by groundwater, which resulted in the sliding of unconsolidated accumulative formation on the terrace. The finite-difference and strength-reduction method is adopted to compute its stability factors under natural, rainstorm, seismic conditions. And three dimensional shapes of potential unstable body under different conditions are put forward.

Key words: earthquake landslide, formation mechanism, terrace, unconsolidated accumulative formation, three-dimentional strength-reduction method

CLC Number: 

  • TU 452
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