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Volume 27 Issue 1
Feb 2016
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Jiwei Jiang, Wei Xiang, Wei Zhang, Jiajun Pan. Deformation forecasting of huangtupo riverside landslide in the case of frequent microseisms. Journal of Earth Science, 2016, 27(1): 160-166. doi: 10.1007/s12583-016-0617-4
Citation: Jiwei Jiang, Wei Xiang, Wei Zhang, Jiajun Pan. Deformation forecasting of huangtupo riverside landslide in the case of frequent microseisms. Journal of Earth Science, 2016, 27(1): 160-166. doi: 10.1007/s12583-016-0617-4

Deformation forecasting of huangtupo riverside landslide in the case of frequent microseisms

doi: 10.1007/s12583-016-0617-4
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  • Corresponding author: Jiwei Jiang, jiangjw1023@163.com
  • Received Date: 09 Apr 2014
  • Accepted Date: 05 Sep 2014
  • Publish Date: 01 Feb 2016
  • Ever since the impoundment of Three Gorges Reservoir (TGR), the seismicity in head region of TGR has increased significantly. Coupled with wide fluctuation of water level each year, it becomes more important to study the deformation forecasting of landslides beside TGR. As a famous active landslide beside TGR, Huangtupo riverside landslide is selected for a case study. Based on long term water level fluctuation and seismic monitoring, three typical adverse conditions are determined. With the established 3D numerical landslide model, seepage-dynamic coupling calculation is conducted under the seismic intensity of V degree. Results are as follows: 1. the dynamic water pressure formed by water level fluctuation will intensify the deformation of landslide; 2. under seismic load, the dynamic hysteresis is significant in defective geological bodies, such as weak layer and slip zone soil, because of much higher damping ratios, the seismic accelerate would be amplified in these elements; 3. microseisms are not intense enough to cause the landslide instability suddenly, but long term deformation accumulation effect of landslide should be paid more attention; 4. in numerical simulation, the factors of unbalance force and excess pore pressure also can be used in forecasting deformation tendency of landslide.

     

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