Soil Properties regarding Geological Conditions in Landslides area

산사태 발생지역에서의 지질조건별 토질특성

  • Song, Young-Suk (Geol. & Envir. Hazards Division, Korea Institute of Geoscience & Mineral Resources (KIGAM)) ;
  • Kim, Won-Young (Geol. & Envir. Hazards Division, Korea Institute of Geoscience & Mineral Resources (KIGAM)) ;
  • Chae, Byung-Gon (Geol. & Envir. Hazards Division, Korea Institute of Geoscience & Mineral Resources (KIGAM)) ;
  • Kim, Kyeong-Su (Geol. & Envir. Hazards Division, Korea Institute of Geoscience & Mineral Resources (KIGAM))
  • 송영석 (한국지질자원연구원 지질환경재해연구부) ;
  • 김원영 (한국지질자원연구원 지질환경재해연구부) ;
  • 채병곤 (한국지질자원연구원 지질환경재해연구부) ;
  • 김경수 (한국지질자원연구원 지질환경재해연구부)
  • Published : 2005.03.25

Abstract

A lot of landslides were occurred in Gangnung, Macheon and Geochang areas by Typhoons such as RUSA(2002) and MEAMI(2003). Soil properties of these areas are investigated regarding geological conditions in this study. The shallow plane failure were occurred in Gangnung and Geochang areas, whereas the deep circle failure were occurred in Macheon area. The matrix in Gangnung and Geochang areas was composed of Granite, and the matrix in Macheon area was composed of Gabbro. The disturbed and undisturbed soils were sampled in these areas. As the results of laboratory tests using sampled soils, the coefficient of permeability in Granite region is lower than that in Gabbro region. In the cases that the silt and clay contents are included less than 4% for the soils of Granite region and less than 7% for the soils of Gabbro region, the coefficients of permeability are rapidly increased for both soils. In addition, the simple equations for predicting the coefficients of permeability are proposed using the effective particle size and the silt and clay contents according to geological condition.

Keywords