Consideration on the Influence of Seismic Shaking on Forest Slope Stability and Landslide Warning Rainfall in the Aftermath of the Strong Earthquake

DOI HANDLE Open Access
  • Kubota Tetsuya
    Laboratory of Erosion Control, Division of Forest Environmental Sciences, Department of Agro–environmental Sciences, Faculty of Agriculture,Kyushu University
  • Nakamura Go
    Nagase Brothers Inc.
  • Shinohara Yoshinori
    Laboratory of Erosion Control, Division of Forest Environmental Sciences, Department of Agro–environmental Sciences, Faculty of Agriculture, Kyushu University
  • Aditian Aril
    Laboratory of Erosion Control, Division of Forest Environmental Sciences, Department of Agro–environmental,Graduate School of Bioresource and Bioenvironmental Sciences, Kyushu University

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Abstract

The research concerning about the warning rainfall criteria of landslides after strong earthquakes is conducted associated with the great earthquake in Eastern Japan in 2011 (M=9.0). After this kind of strong earthquake, soil strength of the slopes in the region that were exposed to the strong seismic forces is generally reduced by seismic shaking (vibration). In this situation, the revised rainfall criteria for landslides are required. On this point of view, the response of landslide to rainfall under this weaken soil condition was studied. Hence, the impact of rainfall events on the specific landslide slopes that experienced the strong seismic shaking is analyzed using numerical simulation method i.e. finite element method (FEM) in order to evaluate the critical rainfall threshold for landslide occurrence. Consequently, we obtained following results. In the result of FEM analysis, the cracks induced by the earthquake are effective to increase the seepage and render the slopes instable. The slope deterioration mentioned above due to the impact of earthquake causes temporarily 40~50% reduction of critical rainfall for landslide occurrence, corresponding to decrease in safety factor “Fs” of the slopes from Fs=1.02~1.04 to Fs=0.83~0.95. This reduction rate of critical rainfall is as same level as in the earlier researches based on field observations.

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Details 詳細情報について

  • CRID
    1390290699661578240
  • NII Article ID
    120005411079
  • NII Book ID
    AA00247166
  • DOI
    10.5109/1434407
  • HANDLE
    2324/1434407
  • ISSN
    00236152
  • Text Lang
    en
  • Data Source
    • JaLC
    • IRDB
    • Crossref
    • CiNii Articles

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