• 제목/요약/키워드: Seepage pressure

검색결과 174건 처리시간 0.021초

강우시 토사사면내의 간극수압변화에 관한 실험적 고찰 (A Experimental Study on the Variation of the Pore-water Pressure in the Soil Slope during the Rainfall)

  • 정의중;김홍택;장현익;김경석;강인규
    • 한국지반환경공학회 논문집
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    • 제9권1호
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    • pp.33-40
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    • 2008
  • 본 연구는 강우시 토사사면의 침투거동 특성을 규명하기 위한 기초연구로서 강우재현장치를 활용하여 실내모형실험을 실시하여 유한사면내의 간극수압의 변화를 측정하였으며, 이를 바탕으로 강우지속시간에 따른 강우시 유한사면내의 침투거동 특성을 분석하였다. 분석결과 강우가 지속적으로 발생됨에 따라 사면내의 간극수압은 점차 증가하는 것을 알 수 있으며, 강우초기에는 사면 중앙부 표면에서 간극수압이 크고 강우가 점차 지속됨에 따라 사면내로 강우가 침투하여 사면붕괴 직전에는 사면내부의 간극수압이 크게 증가되는 것을 알 수 있었다. 본 연구에서 실시한 실내실험은 계측기의 민감도가 높고 조작이 용이하지 못하여 많은 실험결과를 얻지 못하였으며, 향후 다양한 사면경사에서의 유한사면에 대한 강우시 침투거동 특성에 대해 실험적 연구가 필요하다고 생각된다.

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해저면의 수직 지진 진동에 의해 유발된 해진에 대한 해상 개단 강관 말뚝 기초의 거동 (Response of Open-ended Pipe Pile Foundation at Offshore Sites to Seaquake Induced by the Vertical Seismic Excitation of the Seafloor)

  • 최용규;남문석
    • 한국지진공학회논문집
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    • 제2권1호
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    • pp.11-21
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    • 1998
  • 해상에 설치된 기초말뚝의 경우 지진의 3가지 성분 즉, 지반의 수평운도, 지반의 연직진동에 의해 발생된 상부구조물과의 피드백 (feedback)에 의한 말뚝의 연직진동, 그리고 지반의 연직진동에 의해 유발된 해진(seaquake)의 진동이 말뚝 기초의 거동에 영향을 미친다. 본 연구에서는 유발된 해진의 진동을 해저면에서 유사화된 sine 정현파 형상의 동수압으로 모델링하였다. 해진(seaquake) 작용중 약 220m 이상의 심해에 설치된 개단 말뚝의 지지력은, 지반내에 유발된 과도한 과잉 간극수압으로 인하여, 심각하게 저감도었으며, 관내토 폐쇄력도 80% 이상 감소되었다. 해진중 관내토 선단 하부에서 발생된 과도한 과잉 간극수압으로 인하여 관내토내에 과도한 상향의 침투력이 유발되어 관내토 폐색이 손상되었다. 약 220m 이하의 천해에 설치된 개단말뚝의 지지력은 해진에 의해 약 10% 감소하였으며, 관내토의 폐쇄력은 5%이하만큼 감소하였다.

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The ground response curve of underwater tunnels, excavated in a strain-softening rock mass

  • Fahimifar, Ahmad;Ghadami, Hamed;Ahmadvand, Masoud
    • Geomechanics and Engineering
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    • 제8권3호
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    • pp.323-359
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    • 2015
  • This paper presents an elasto-plastic model for determination of the ground response curve of a circular underwater tunnel excavated in elastic-strain softening rock mass compatible with a nonlinear Hoek-Brown yield criterion. The finite difference method (FDM) was used to propose a new solution to calculate pore water pressure, stress, and strain distributions on periphery of circular tunnels in axisymmetric and plain strain conditions. In the proposed solution, a modified non-radial flow pattern, for the hydraulic analysis, is utilized. To evaluate the effect of gravitational loads and variations of pore water pressure, the equations concerning different directions around the tunnel (crown, wall, and floor) are derived. Regarding the strain-softening behavior of the rock mass, the stepwise method is executed for the plastic zone in which parameters of strength, dilatancy, stresses, strains, and deformation are different from their elasto-plastic boundary values as compared to the tunnel boundary values. Besides, the analytical equations are developed for the elastic zone. The accuracy and application of the proposed method is demonstrated by a number of examples. The results present the effects of seepage body forces, gravitational loads and dilatancy angle on ground response curve appropriately.

Rainfall induced instability of mechanically stabilized earth embankments

  • Roy, Debasis;Chiranjeevi, K.;Singh, Raghvendra;Baidya, Dilip K.
    • Geomechanics and Engineering
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    • 제1권3호
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    • pp.193-204
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    • 2009
  • A 10.4-m high highway embankment retained behind mechanically stabilized earth (MSE) walls is under construction in the northeastern part of the Indian state of Bihar. The structure is constructed with compacted, micaceous, grey, silty sand, reinforced with polyester (PET) geogrids, and faced with reinforced cement concrete fascia panels. The connections between the fascia panels and the geogrids failed on several occasions during the monsoon seasons of 2007 and 2008 following episodes of heavy rainfall, when the embankment was still under construction. However, during these incidents the MSE embankment itself remained by and large stable and the collateral damages were minimal. The observational data during these incidents presented an opportunity to develop and calibrate a simple procedure for estimating rainfall induced pore water pressure development within MSE embankments constructed with backfill materials that do not allow unimpeded seepage. A simple analytical finite element model was developed for the purpose. The modeling results were found to agree with the observational and meteorological records from the site. These results also indicated that the threshold rainwater infiltration flux needed for the development of pore water pressure within an MSE embankment is a monotonically increasing function of the hydraulic conductivity of backfill. Specifically for the MSE embankment upon which this study is based, the analytical results indicated that the instabilities could have been avoided by having in place a chimney drain immediately behind the fascia panels.

수두손실률의 경시변화에 의한 방조제 제체의 점진적인 차수상태 변화 감시 (The Monitoring on Gradual Change of Seepage Blocking State with the Hydraulic Head Loss Rate Change According to Passage of time in Sea Dike Embankment)

  • 임성훈
    • 한국농공학회논문집
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    • 제57권1호
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    • pp.1-9
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    • 2015
  • In this study it was adopted on sea dike monitoring that the safety monitoring with statistical limits which was adapted usually on safety monitoring by measuring pressures, stresses or deformations. And also the hydraulic head loss rate change according to passage of time was calculated for the purpose of safety monitoring. Safety monitoring by setting the statistical limit on the measured pore water pressure graphs need to be supplemented with an additional method of monitoring because the difference between the rise and fall of the tide was irregular. Safety monitoring by the limits set from values predicted by linear regression and standard errors on the hydraulic head loss graph was not affected by irregularity of tide. But if the condition of an embankment is changed gradually and slowly, it will not be detected on the hydraulic head loss graph. The graph of hydraulic head loss rate for every 24 hours vs date showed clearly that the sea water blocking state was getting better or not even though it was changed gradually and slowly.

Numerical Study of Unsaturated Infinite Slope Stability regarding Suction Stress under Rainfall-induced Infiltration Conditions

  • Song, Young-Suk;Hwang, Woong-Ki
    • 지질공학
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    • 제24권1호
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    • pp.1-8
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    • 2014
  • Numerical stability analysis of an unsaturated infinite slope under rainfall-induced infiltration conditions was performed using generalized effective stress to unify both saturated and unsaturated conditions The soil-water characteristic curve (SWCC) of sand with a relative density of 75% was initially measured for both drying and wetting processes. The hydraulic conductivity function (HCF) and suction stress characteristic curve (SSCC) were subsequently estimated. Under the rainfall-induced infiltration conditions, transient seepage analysis of an unsaturated infinite slope was performed using the finite element analysis program, SEEP/W. Based on these results, the stability of an unsaturated infinite slope under rainfall-induced infiltration conditions was examined in relation to suction stress. According to the results, the negative pore-water pressure and water content within the slope soil changed over time due to the infiltration. In addition, the variation of the negative pore-water pressure and water content led to a variation in suction stress and a subsequent change in the slope's factor of safety during the rainfall period.

On the effect of void ratio and particle breakage on saturated hydraulic conductivity of tailing materials

  • Ma, Changkun;Zhang, Chao;Chen, Qinglin;Pan, Zhenkai;Ma, Lei
    • Geomechanics and Engineering
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    • 제25권2호
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    • pp.159-170
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    • 2021
  • Particle size of tailings in different areas of dams varies due to sedimentation and separation. Saturated hydraulic conductivity of high-stacked talings materials are seriously affected by void ratio and particle breakage. Conjoined consolidation permeability tests were carried out using a self-developed high-stress permeability and consolidation apparatus. The hydraulic conductivity decreases nonlinearly with the increase of consolidation pressure. The seepage pattern of coarse-particle tailings is channel flow, and the seepage pattern of fine-particle tailings is scattered flow. The change rate of hydraulic conductivity of tailings with different particle sizes under high consolidation pressure tends to be identical. A hydraulic conductivity hysteresis is found in coarse-particle tailings. The hydraulic conductivity hysteresis is more obvious when the water head is lower. A new hydraulic conductivity-void ratio equation was derived by introducing the concept of effective void ratio and breakage index. The equation integrated the hydraulic conductivity equation with different particle sizes over a wide range of consolidation pressures.

불포화 수리특성에 대한 댐체 침투 거동의 민감도 분석 (Sensitivity of Seepage Behavior of Dam to Unsaturated Soil Properties)

  • 조성은
    • 한국지반공학회논문집
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    • 제21권3호
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    • pp.119-131
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    • 2005
  • 댐 안정성 평가를 위하여 불포화 이론을 이용한 침투해석 기법이 널리 사용되고 있으나 지반의 불포화 거동에 대한 인식 부족과 실험절차의 번거로움으로 인하여 입력 물성치에 대한 체계적인 실험과 평가가 일반화되지 못하고 있는 실정이다. 불포화 수리특성에 따라 침투수량 및 간극수압 분포 등 댐체 및 제방의 침투거동이 달라지나 국내 지반에 대한 실험자료 부족으로 대부분 단순 추정에 의한 값을 사용하고 있다 본 연구에서는 불포화 수리특성이 댐체의 침투 거동에 미치는 영향을 살펴보기 위하여 함수특성곡선과 투수계수곡선에 대하여 고찰하고 수치해석을 수행하였다. 해석결과 변수 a와 n은 값이 클수록, m은 값이 작을수록 중력에 의한 침윤선의 하강이 빨리 발생하였다. 유한차분 형식에 의해 개략적으로 계산한 민감도는 침윤선 부근에서 가장 크게 나타났고 시간에 따른 민감도의 변화에는 함수특성곡선의 기울기와 관련된 n값이 가장 큰 영향을 주었다.

강우침투실험을 통한 불포화 풍화토 지반의 강우 침투속도 분석 (Analysis of Seepage Velocity in Unsaturated Weathered Soils Using Rainfall Infiltration Test)

  • 김훈;신호성;김윤태;박덕근;민덕기
    • 한국지반공학회논문집
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    • 제28권2호
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    • pp.71-78
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    • 2012
  • 본 연구에서는 실내 강우침투실험을 통하여 강우강도에 따른 지반 내 침투속도를 산정하였으며, 침투특성을 분석하여 보았다. 또한 수치해석을 이용한 해석결과와 비교 검증을 수행하였으며, 시간에 따른 간극수압과 포화도 그리고 유출속도의 변화는 대체로 잘 일치함을 보였다. 강우강도에 따른 침투속도는 실내실험과 수치해석에서 선형적으로 증가하는 경향을 나타냈으며, 강우강도가 지반의 포화투수계수에 근접시 침투속도가 급격히 증가하였다. 또한 강우 침투시 습윤전선의 상부는 부분적으로 포화되어 침투하는 경향을 보였다. 따라서 실제 지반에서 습윤전선은 비교적 빠르게 진행하여 사면의 불안정을 초래할 것으로 판단된다.

지오텍스타일로 보강된 농업용 저수지 제체의 붕괴거동 (Behavior of Failure of Agricultural Reservoirs Embankment Reinforced by Geotextile under Overtopping Condition)

  • 이달원;노재진
    • 한국농공학회논문집
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    • 제56권2호
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    • pp.59-64
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    • 2014
  • In this study, the large scale test was performed to investigate the behavior of failure for the embankment and spillway transitional zone by overtopping. The pore water pressure, earth pressure, settlement and failure pattern of covering embankment with geotextile were compared and analyzed. The pore water pressure showed a small change in the spillway transition zone and core, indicating that the geotextile efficiently reinforced the embankment. The earth pressure decreased the infiltration of the pore water only in inclined cores type to secure local stability. The behavior of failure started from the bottom and gradually progressed upwards. After the intermediate overtopping period (100 min), width and depth of the seepage erosion were very small due to the effect of geotextile which delayed failure. Therefore, the reinforced method by geotxtile was a very effective method to respond to the emergency due to overtopping.