• 한국재난정보학회 논문집
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• 제14권4호
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• pp.421-429
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• 2018

연구목적 : 본 연구는 기후변화에 따른 강우량 및 강우패턴을 분석하여 강우시 비탈면 거동을 파악하기 위해 강우사상을 합리적으로 적용하여 절토부 비탈면 안정성해석에 활용하고자 수치해석기법을 이용하여 비탈면 높이별, 강우사상별 침투해석을 실시하여 강우사상 및 강우지속시간에 따른 지하수위 변화를 고려한 비탈면 안정성검토를 실시하였다. 연구결과 : 강우사상(Uniform Rainfall, US Army Corps., Huff 4분위법 중 1/4법 및 4/4법)에 따른 화강풍화토 비탈면의 수치해석결과 비탈면이 높을수록 침투된 강우가 지하수위까지 빠르게 도달하지 못하여 지하수위 상승은 작아지고, 비탈면의 안전율도 작게 분석되었다. 결론 : 초기강우강도가 제일 큰 강우패턴 Case 3조건인 Huff 4분위법 중 1/4법에서 지하수위 상승량이 제일 크게 나타났으며, 안전율은 가장 작게 나타났다.

• 한국지반환경공학회 논문집
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• 제12권10호
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• pp.29-38
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• 2011

현행 사면 안정 해석 시 지하수위 결정방법은 강우에 의한 침투과정에 의한 불포화구간을 제대로 반영하고 있지 못하고 있다. 본 연구에서는 강우에 의한 지표면 상부침투에 의한 포화대 증가에 따른 사면의 안전율 변화를 실내모형실험을 통해 검증하고자 하였다. 강우침투로 인한 흙의 전단강도 저하를 정확히 파악하기 위해 실내 사면모형실험을 통해 함수비 변화를 측정하고, 이에 따른 강도정수의 변화를 파악하였다. 포화깊이 3.0m에서 4.5m로 변할 때 안전율이 가장 크게 변화되는 것을 알 수 있었으며, 이는 설계기준에서 제시한 지하수위 (-)3.0m은 다소 과소 설계된다는 것을 판단할 수 있다. 또한, 지표면 포화로 해석할 경우는 과다 설계되므로 사면의 설계 시 강우 침투에 관한 실험 및 해석이 필요함을 알 수 있다.

• 산업기술연구
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• 제26권B호
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• pp.43-51
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• 2006

Through the result of calculating the deviation between the value calculated from two-dimensional number formula, one-dimensional number interpretation, and curving part water surface type calculation method, we could confirmed that the deviation is reduced more than 50% when we use curving part water surface type calculation method. Also it was confirmed that there occurs the reduction rate of maximum 59% as the result of comparing with one-dimensional number interpretation since the reduction rate of safe room height was 20%, in 500 CMS of flood water quantity when we planted the construction of levee by curving part water surface type calculation method. And therefore, we have confirmed that the curving water surface type calculation method can be used as a simple formula in rivers with water quantity less than 500 CMS that flows in and out in Jess than 90 degree angle.

• 한국토양비료학회지
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• 제40권3호
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• pp.208-213
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• 2007

1985년부터 1991년까지 일 강우량 80 mm 이상일 때의 유거량 자료를 이용하여 집중강우시 물유출 양상을 구명하였다. 지표유거가 발생하는 유거 발생 최소 강우량은 지표피복과 경사장에 따라 결정되는 것으로 나타났으며 토성과 경사각에 따라서는 별 차이를 나타내지 않았다. 유거 발생 최소 강우량을 기준으로 그 이후의 유거량은 강우량에 따라 직선적으로 증가하였다. 그러나 이 때의 기울기 즉, 유거율은 토성, 지표 피복형태, 경사각, 경사장에 따라 달라졌다. 유거율은 토성이 세립질로 침투속도가느릴 수록 커졌으며 콩 재배에 비해 물흐름에 대한 저항이 작은 나지에서 컸다. 또한 유거율은 경사각의 제곱근에 비례하여 증가하였으며 경사장이 길어짐에 따라 특정값에 수렴하면서 감소하였다. 이러한 결과를 바탕으로 집중강우 시 유거량을 모사할 수 있는 식을 다음과 같이 개발하였다. $$Runoff=a(s^{0.5}+l^b)(Rainfall-80(1-e^{-bl}))------(9)$$ 이 식에서 a는 토양의 침투특성과 관련된 토양계수, b는 지표 피복의 영향을 나타내는 지표피복계수, s는 경사각(radian), l은 경사장(m)이다. a는 토성에 따라 0.5~0.6으로 나타났으며 세립질일 수록 값이 컸다. b는 피복조건에 따라 나지에서 0.06, 콩 재배시 0.5 정도로 평가되었다.

• Geomechanics and Engineering
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• 제8권4호
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• pp.511-521
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• 2015

It is a common failure type that high-filled embankment slope sideslips. The deformation mechanism and factors influencing the sideslip of embankment slope is the key to reduce the probability of this kind of engineering disaster. Taking Liujiawan high-filled embankment slope as an example, the deformation and failure characteristics of embankment slope and sheet-pile wall are studied, and the factors influencing instability are analyzed, then the correlation of deformation rate of the anti-slide plies and each factor is calculated with multivariate linear regression analysis. The result shows that: (1) The length of anchoring segment is not long enough, and displacement direction of embankment and retaining structure are perpendicular to the trend of the highway; (2) The length of the cantilever segment is so large that the active earth pressures behind the piles are very large. Additionally, the surface drainage is not smooth, which leads to form a potential sliding zone between bottom of the backfill and the primary surface; (3) The thickness of the backfill and the length of the anti-slide pile cantilever segment have positive correlation with the deformation whereas the thickness of anti-slide pile through mudstone has a negative correlation with the deformation. On the other hand the surface water is a little disadvantage on the embankment stability.

• Bulletin of the Korean Chemical Society
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• 제26권10호
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• pp.1565-1568
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• 2005

A surface renewable pH electrode was prepared by utilizing composite electrode technique. Iridium oxide micro-fine particles was prepared by hydrolysis of $(NH_4)_2IrCl_6$ at elevated temperature. The iridium oxide particles were mixed with well-dispersed carbon black and then filtered. The mixture was suspended in DMF containing PVC as a binder. The mixture was precipitated rapidly by adding large amount of water. The precipitate was ground and pressure-molded to iridium oxide composite electrode material. The electrode showed linear response between pH 1-13 with 50 to 60 mV/pH slope. The electrode maintained the pH response without appreciable slope drift for 170 days if stored in deionized water. The electrode surface can be renewed reproducibly by simple grinding process whenever contaminated or deactivated.

• 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.

• 한국방재학회 논문집
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• 제6권4호통권23호
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• pp.57-65
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• 2006

본 연구에서는 본류와 지류가 만나는 합류구간, 만곡 및 사행구간이 있는 자연하천과 동일한수리모형을 제작하고 합류부를 중심으로 본류와 지류의 유량비 변화에 따라 모형의 합류부 횡단면에서 발생하는 수위차의 변화를 분석하였다. 합류이전의 최하류단면 수위를 기준으로 하는 합류부 각 단면의 최대수위 변화에 미치는 유량비의 영향은 합류부 하류구간보다 상류구간에서 더 크게 나타난다. 횡단면의 최소수위에 대한 최대수위의 변화는 합류부 중심에 가까울수록 증가하며 합류부 중심 직하류에서 최대를 보인다. 또한 합류구간 횡단면의 수면경사는 단면형태에 따라 영향을 받으며 본류에 대한 지류의 유량비가 감소할수록 수면경사도 감소한다. 기존에 제안된 일정한 곡률반경과 정형화된 단면에서 도출된 횡단면 수위차 산정 공식이 평창강과 동일하게 제작된 모형수로에서 실측값과 약 60%의 차이를 보인 반면 본 연구에서는 실측값과 약 10%의 차이를 보이는 수위차 산정 공식을 제안하였다.

• Geomechanics and Engineering
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• 제19권1호
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• pp.1-9
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• 2019

Shallow failures occur frequently in both engineered and natural slopes in expansive soils. Rainfall infiltration is the most predominant triggering factor that contributes to slope failures in both expansive soils and clayey soils. However, slope failures in expansive soils have some distinct characteristics in comparison to slopes in conventional clayey soils. They typically undergo shallow failures with gentle sliding retrogression characteristics. The shallow sliding mass near the slope surface is typically in a state of unsaturated condition and will exhibit significant volume changes with increasing water content during rainfall periods. Many other properties or characteristics change such as the shear strength, matric suction including stress distribution change with respect to depth and time. All these parameters have a significant contribution to the expansive soil slopes instability and are difficult to take into consideration in slope stability analysis using traditional slope stability analysis methods based on principles of saturated soil mechanics. In this paper, commercial software VADOSE/W that can account for climatic factors is used to predict variation of matric suction with respect to time for an expansive soil cut slope in China, which is reported in the literature. The variation of factor of safety with respect to time for this slope is computed using SLOPE/W by taking account of shear strength reduction associated with loss of matric suction extending state-of-the art understanding of the mechanics of unsaturated soils.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2004년도 춘계학술발표회
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• pp.580-585
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• 2004

The purpose of this study is the stability evaluation of soil slope according to inclination of upper natural slope. Upper natural slope breeds loss of slope by inflow in slope of surface water by rainfal1 and f1uctuation of amount of materials in slope through method of cutting slope according to degree of inclination. Basis of standard inclination does not consider of inclination of upper natural slope and is presented uniformly. Therefore, in this study, analyzed stability of inclination of upper natural slope through limit equilibrium analysis. Result is same as following. First, safety factor through limit equilibrium analysis is almost direct decrease when gradient of soil slope is 1:1.2, 1:1.5. However, when gradient of soil slope is 1:1.0, 1:0.7, if sinclination of upper natural slope are $20^{\circ}$, it shows tendency that decrease of safety factor becomes low rapidly. Second, when when gradient of soil slope is fixed, inclination of upper natural slope increase tendency(maximum 3.0 times) that decrease of safety factor.