Journal of the Korean GEO-environmental Society (한국지반환경공학회 논문집)

Korean Geo-Environmental Society (한국지반환경공학회)
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Variation of Landslide Risk with Parameters

매개변수에 따른 산사태 위험도의 변화

  • Lee, Jundae (Department of Civil Engineering, Semyung University) ;
  • Kwon, Youngcheul (Department of Civil Engineering and Management, Tohoku Institute of Technology) ;
  • Bae, Wooseok (NANO-GEO ENC Co. Ltd.)
  • Received : 2017.11.02
  • Accepted : 2017.12.08
  • Published : 2018.01.01
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Abstract

In this study we performed risk evaluation based on parameters using the SINMAP, GIS-based extended program in order to predict ground disaster that is frequent recently. As for the risk evaluation, in order to understand the effects of parameters, we defined that the ranges of internal friction angles and T/R values as important variables had three and four patterns, respectively. The results of the interpretation were compared with those of the existing landslide in order to identify landslide flow and to evaluate the applicability of the parameters. The analysis of the geomorphologic saturated zone showed that the boundary saturated zone and the saturated zone were almost consistent with the site of avalanche of earth and rocks and the area of underground water convergence was correlated to the area where collapse started, indicating that the geomorphologic saturated zone may serve as an index for estimating possibility of landslide when used with slope distribution, colluvial soil, and structures inducing landslide in combination. When the lower limit of the internal friction angle increased more, the upper threshold decreased by 50 to 70% and the influence on the stability index was higher, but the influence was declined within the range of lower wetness index. The analysis of changes based on wetness index range showed that all the groups have similar SI distribution, except for the one in which mean altitude values are applied, indicating that the results are susceptible more by the internal friction angle than by the wetness index.

본 연구에서는 최근 발생하는 지반재해를 사전에 예측하기 위해 널리 사용되고 있는 GIS의 기반의 확장프로그램인 SINMAP을 이용하여 매개변수에 따른 위험도 평가를 수행하였다. 위험도평가는 매개변수의 영향을 파악하기 위해 중요변수인 내부마찰각과 T/R 값의 범위를 각각 3가지와 4가지 패턴으로 결정하였으며, 해석결과를 기존 산사태 결과와 비교하여 산사태 거동을 규명하고 매개변수의 적용성을 평가하였다. 지형학적 습윤대를 분석한 결과, 한계습윤대와 포화대가 토석류 영역과 거의 일치하고 있으며 지하수 수렴부가 붕괴시점부와 상관관계가 있는 것으로 나타나 지형학적 습윤대가 경사분포나 붕적토층의 존재여부, 산사태 유발구조물 등과 복합적으로 산사태 발생 가능성을 평가하기 위한 지표로 사용될 수 있을 것으로 판단된다. 내부마찰각의 하한계가 증가함에 따라 상한계불안정영역이 50~70%까지 감소되어 안정지수에 미치는 영향력이 큰 경향을 보였으나 낮은 습윤지수 범위에서는 그 영향력이 줄어드는 양상을 나타내었다. 습윤지수의 범위에 따른 변화를 분석한 결과, 고도평균값을 적용한 경우를 제외하면 모든 Group에서 유사한 안정지수 분포를 보이고 있어 습윤지수보다는 내부마찰각에 민감한 양상을 나타내고 있음을 알 수 있다.

Keywords

References

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