A Study on Characteristics of Rainfall Triggering Landslides and Geometry of Slopes in Chuncheon during 2006

2006년 춘천지역 산사태 유발 강우와 사면의 기하 특성에 관한 연구

  • 유남재 (강원대학교 토목공학과) ;
  • 이용원 (강원대학교 산업대학원 토목공학과) ;
  • 김호진 (강원대학교 대학원 토목공학과)
  • Published : 2010.08.31

Abstract

This paper is results of analyzing the characteristics of rainfall triggering landslides and geometry of slopes, caused by the heavy rainfall and antecedent precipitation by Typhoons Ewiniar and Bilis at Chuncheon area in Gangwondo around July in 2006. As results of analyzing the characteristics of rainfall, landslides in 131 sites were found to happen due to the heavy rainfall having the maximum intensity of rainfall in an hour during July 15 and antecedent precipitation during July 12 to 14 causing the ground to be weak by increasing the degree of saturation previously. From results of analyzing the geometrical characteristics of 131 slopes where landslides occurred, the slope width were in the range of 6~10m. The average slope length and angle were 46m and $51.8^{\circ}$, which was relatively steep slope, respectively. Landlises occurred in the elevation of 400 - 500 m with the most probable frequency.

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