• 지질공학
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• 제27권3호
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• pp.267-274
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• 2017

암반은 암석재료 자체의 역학적 성질과 암반내에 분포하는 불연속면의 기하학적 특징에 의해 그 역학적 특성이 좌우된다. 암반사면의 경우에는 불연속면에 의해 특히 파괴면의 위치와 파괴후의 거동 등이 달라진다. 본 논문에서는 불연속면의 규모에 따라 암반사면의 파괴형태가 달라지는 점을 고려하여, 원호파괴와 평면파괴 안정해석을 위한 2개의 3D 해석방법을 개발하고 실제 사면에 적용하여 그 적용성을 검토하였다. 결과, 원호파괴의 경우, 자연건조상태에서는 안정하지만 강우에 의해 표층 함수비가 증가하면 불안정해지는 해석 결과를 얻었다. 평면파괴의 경우도 강우에 의해 불연속면 자체의 마찰각이 감소하는 영향에 의해 건조상태보다 불안정해지는 결과가 나타났다. 이상의 해석 결과로부터 실제 사면에서의 현상을 잘 반영하는 것으로 보아, 개발된 해석방법이 사면안정성 검토 또는 유지관리의 목적으로 적용가능하다고 판단된다.

• Structural Engineering and Mechanics
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• 제89권3호
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• pp.253-263
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• 2024

Slope stability is generally paid more attention to in slope protection works, especially for slope containing weak layers. Two indexes of safety factor and failure model are selected to perform slope stability. Moreover, the finite element limit analysis method comprehensively combines the advantage of the limit analysis method and the finite element method obtaining the upper and lower bounds of the safety factor and the failure mode under the slope stability limit state. In this study, taking a waste dump containing a weak layer as an engineering background, the finite element limit analysis method is adopted to explore the potential failure mode. Meanwhile, the sensitivity analysis of slope stability is performed on geometrical and geotechnical parameters of the waste dump. The results show that the failure mode of the waste dump slope is two wedges if the weak layer is located on the ground surface (Model A), while the slope can be observed as three wedges failure if the weak layer is below the ground surface (Model B). In addition, both failure modes are highly sensitive to the friction angle of the weak layer and the shear strength of waste disposal, and moderately sensitive to the heap height, the dip angle and cohesion of the weak layer, while the toe cutting has limited effect on the slope stability. Moreover, the sensitivity to the excavation of the ground depends on the location of the weak layer and failure mode.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2008년도 춘계 학술발표회 초청강연 및 논문집
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• pp.1351-1358
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• 2008

This paper presents how the load transfer mechanism of the ground anchor affects on the stability analysis of anchored slope. The finite element analysis and the conventional limit equilibrium analysis on the anchored slope were performed and compared. The limit equilibrium analysis of the anchored slope is quite open used in design practice due to the easiness of the analysis. However, the load transfer mechanism is not considered properly for the analysis. When the failure surface passes through the bonded length of an anchor, the anchor load is disregarded and the factor of safety for the anchored slope is smaller than it should be. In this study, the load transfer distribution was incorporated into the limit equilibrium stability analysis of the anchored slope and the results were compared with the results of finite element analysis.

• 자원환경지질
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• 제36권4호
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• pp.313-320
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• 2003

사면재해는 강우기에 반복적으로 발생하는 지질재해의 하나로 우리나라의 경우 연평균 약 23명 정토의 인명피해가 사면재해로 인해 발생하고 있으며, 이는 자연재해로 인한 인명피해 중 약 25％ 정도를 차지하는 수치이다. 그러나, 이러한 사면재해는 다양하고 복합한 지질 및 지형 특성과 갉은 공간적인 특성과 집중호우와 같은 기후특성에 의해 좌우되므로 사면재해 예측이나 위험성에 대한 정량적인 산정을 무척 어려운 실정이다. 따라서, GIS를 이용한 위험성분석이나 확률을 이용한 다양한 기법이 활용되고 있다. 특히, GIS를 이용한 기법은 광역적인 지역에 대하여 방대한 양의 자료를 효율적으로 처리 및 분석을 수행함으로서 사면재해 관련 연구에 폭 넓게 활용되고 있다 본 연구에서 사용된 무한사면해석기법은 사면재해의 발생여부와 관련요인간의 연관성에 대한 단순한 통계적인 분석에 의한 기존 기법의 한계점을 보완하고 사면재해발생과 관련된 역학적인 검토를 수행하기 위하여 제안되었다. 본 연구 결과에 의하면 사면재해가 발생했던 지점과의 비교를 농하여 지반이 완전히 포화된 경우, 즉 m=1인 경우 무한사면모델에서 불안정하다고 해석된 지역에서 전체 사면재해의 87.5％가 발생하였음을 보여주고 있어 사면재해에 대한 해석기법으로서의 착용가능성을 보여주고 있다.

• 한국농공학회지
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• 제31권1호
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• pp.58-70
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• 1989

The paper compared the Bishop methed to the Fellenius method in the analysis of slope stability. Laboratory model test was carried out in the case of seepage flow considered. The results obtained from this study were summarized as follows; 1. The slice pieces of 10 were enough to analysis the slope stability. 2. The safety factor. by the Fellenius method was lower than the Bishop method by the 96 to 97% in the case of no seepage flow and by the 95 to 96% in the case of seepage flow considered. 3. Besides the parameter of soil and slope, the safety factor of slope was influenced by the height of slope. This phenomena was distinct in the height of height less than 10 meters. 4. In the case of clay, there was no difference in the safety factor of slope between Fellenius and Bishop rnethod. The safety factors of slope with the seepage flow considered were lower than those with no see-page flow. 5. The influence of cohesion on the safety factor was more significant in the Bishop method than in the Fellenius method. 6. The slope failure of model test of A and B soil samples with high permeability coefficient was taken place slightly in vicinity of toe by the concentration of stress and gradually increased 7. Under condition of same slope height, the shapper the slope, the shorter the radius and the center of critical circle appered downward and finally failure of slope occured inside the slope.

• 지질공학
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• 제27권1호
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• pp.21-29
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• 2017

광미 적치사면에서 측정된 모니터링 결과와 현장조건을 고려한 수치해석결과를 이용하여 강우시 불포화 토층내 모관흡수력변화를 비교하고 이를 토대로 사면안정해석을 수행하였다. 이를 위하여 계측기간 동안 강우강도가 가장 크게 발생된 기간(72시간)을 선정하고, 대상기간 동안의 모관흡수력과 강우자료를 분석하였다. 그리고 현장에서 측정된 강우자료를 적용하여 침투 및 사면안정해석을 수행하였다. 강우에 따른 사면내 침투거동을 해석하기 위하여 SEEP/W를 활용하고 사면내 침투깊이를 고려한 사면안정해석을 위하여 SLOPE/W를 활용하였다. 먼저 현장에서 측정된 강우자료를 적용하여 SEEP/W를 이용한 침투해석을 수행하였다. 침투해석으로 계산된 모관흡수력과 현장계측으로 측정된 모관흡수력을 비교한 결과 모관흡수력의 크기에서는 다소 차이가 있으나 시간에 따른 변화양상은 유사한 것으로 나타났다. 그리고 침투해석결과와 연동하여 SLOPE/W를 이용한 사면안정해석을 수행한 결과 강우강도가 급속하게 증가되는 시점에서 사면안전율은 크게 감소하였으며, 이후 강우가 발생되지 않는 경우 사면안전율이 회복되는 것으로 해석되었다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2006년도 춘계 학술발표회 논문집
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• pp.681-686
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• 2006

This study is to examine slope activity safety ratio on the strength of the natural sample or soil collected through field test in the slope activity region during destruction happened in the course of soil-relocating work planned for ground improvement under strict supervision at the house-building site, using Bishop's slope analysis method and investigate relationship between slope analysis theories and actual destruction so as to compare determining method of clean water of soil essential for slope activity analysis and accuracy of resulting value of clean water of soil.

• 토지주택연구
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• 제9권2호
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• pp.51-57
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• 2018

The causes of landslides are dependant on rainfall events and the soil characteristics of a slope. For the conventional slope stability, the slope stability analysis has been carried out assuming the saturated soil theory. But, in order to clearly explain a proper soil slope condition by rainfall, the research should be performed using the unsaturated soil mechanism suitable for a soil slope in the field. In the study, by using two major categories of soils in Korea, such as granite and gneiss weathered soils, landslide model test and finite element method have been compared with the difference of seepage and soil stability analysis. The hydraulic conductivity of gneiss weathered soil is slower than that of granite weathered soil, and the gneiss weathered soil contains much finer soils than the granite weathered soil. It was confirmed that the instability of the slope was progressing slowly due to the slow rate of volumetric water content of the surface layer.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1998년도 사면안정 학술발표회 논문집
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• pp.111-124
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• 1998

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2009년도 춘계 학술발표회
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• pp.620-625
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• 2009

The seismic slope stability is most often evaluated by the pseudo-static limit analysis, in which the earthquake loading is simplified as static inertial loads acting in horizontal and/or vertical directions. The transient loading is represented by constant acceleration via the pseudostatic coefficients. The result of a pseudostatic analysis is governed by the selection of the value of the pseudostatic coefficient. However, selection of the value is very difficult and often done in an ad hoc manner without a sound physical reasoning. In addition, the maximum acceleration is commonly estimated from the design guideline, which cannot accurately estimate the dynamic response of a slope. There is a need to perform a 2D dynamic analysis to properly define the dynamic response characteristics. This paper develops the modified one-dimensional seismic site response analysis. The modified site response analysis adjusts the density of the layers to simulate the change in mass and weight of the layers of the slope with depth. Multiple analyses are performed at various locations within the slope to estimate the change in seismic response of the slope. The calculated peak acceleration profiles with depth from the developed procedure are compared to those by the two-dimensional analyses. Comparisons show that the two methods result in remarkable match.