Study on Analysis for Factors Inducing the Whangryeong Mountain Landslide

황령산 산사태 원인 분석에 대한 연구

  • 최정찬 (부경대학교 환경지질과학과) ;
  • 백인성 (부경대학교 환경지질과학과)
  • Published : 2002.06.01

Abstract

Recently, plane failure mode occurred frequently along the bedding plane having low angle dip about 20 degree when cutting slopes were constructed in sedimentary rock region of the Gyeongsang Basin. Landslide of the Whangryeong Mountain which was occurred at Busan Metropolitan City in 1999 belongs to the category mentioned above. Reconstruction for cutting slope of the Whangryeong Mountain has finished in 2000 and final grade of reconstructed cutting slope is 1:2.0. To analyze slope failure mode for landslide of the Whangryeong Mountain, various analyses were performed such as in-situ investigation and test, drilling, laboratory test, aerial photograph interpretation, X-ray diffraction analysis, and slope stability analysis using Stereographic Projection and Limit Equilibrium methods. As the result, it is identified that tension cracks had been developed one year before the landslide took place. The tension crack semis to be formed by merging several joint sets. It appears that failure blocks broke down along the sliding planes of different layers. Risk of plane failure is conformed as a result of stability analysis using Stereographic Projection and Limit Equilibrium methods in case that greenish gray tuffaceous shales, regared as sliding planes, are weathered. From now on, a detailed investigation is needed for the thin layers which is sensitive to weathering, and stability analysis for this layer is performed at cut slope construction site having similar geological condition.

최근 경상분지 퇴적암 지대에서 절개사면 형성 시, 20$^{\circ}$ 저각 경사의 층리면을 따른 평면파괴 양상이 빈번하게 발생하고 있다. 부산시에서 1999년 발생한 황령산 산사태도 이 범부에 속한다. 현재 황령산사면은 사면구배가 1:2.0으로 재조정 되어 2000년도에 공사가 마무리되었다. 황령산 산사태의 사면파괴형태에 대한 분석을 하기위하여 현장 암반조사 및 시험, 시추, 실내 시험, 항공사진판독, X-선 회절분석, 평사투영법 및 한계평형법을 이용한 사면 안정성 분석등이 실시되었다. 그 결과, 산사태 발생 1년 전부터 인장균열들이 연장 발달하는 것이 확인 되었고, 인장균열은 여러방향의 절리들이 합쳐저 생성된 것으로 생각된다. 파괴암체도 각각 다른 층리면을 따라 붕괴된 것으로 분석되었다. 평사투영법 및 한계평형법을 이용한 안정성 검토결과 활동면으로 작용한 녹회색 응회질 셰일층이 풍화된 경우 평면파괴의 위험성이 있는 것이 확인되었다. 향후 이와 유사한 지역에서 절개사면 건설 시, 박층의 풍화에 약한 층에 대한 세밀한 조사가 필요하며 이에 대한 안정성 분석이 수행되어야 한다.

Keywords

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