• 제목/요약/키워드: Seepage rate

검색결과 69건 처리시간 0.031초

흙 수로에서 삼투손실에 관한 연구 (A Study on the Seepage Loss from Earth Canal)

  • 박상현;김시원
    • 한국농공학회지
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    • 제23권3호
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    • pp.88-95
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    • 1981
  • This study was carried out to investigate the relation between seepage losses and flow section area in earth canals. Totally 77 seepage measurement was gained by ponded method and the tested canals belong to the irrigation area of Farmland Improvement Association in each province, Korea. The results obtained from this study may be used as a reasonable criteria for the estimation of canal seepage losses in the design of irrigation systems. Obtained results are summarized as follows: 1. Average seepage rates in each Soils is 14cm/day in ML, 6. 3cm/day in CL and 24.9 cm/day in SM. 2. Water depth and water surface width in eath canals have little influenced on the seepage rate, while the seepage losses was increased in proportion as the water surface width lengthens. 3. A formula of S=C.An defining a relationship between seepage losses and flow section was derieved as follows. ML:S=O. 35 VA 1.20 (m$^3$/day/m) CL:S=O. 13 VA 0.84 SM:s=O.67VA-1.56 4. The average seepage loss rates per 1km of canal are as followings. Measured Time ML CL SM 0-4 hrs 2.2% 0.6% 4.5% 4-2 4hrs 1.0% 0.15% 2.0% In above table we may obtain the following results. The first row is suitable for the canal having short delivery time of irrigation, while the second row for the canal having long delivery time.

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Limit analysis of rectangular cavity subjected to seepage forces based on Hoek-Brown failure criterion

  • Yang, X.L.;Qin, C.B.
    • Geomechanics and Engineering
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    • 제6권5호
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    • pp.503-515
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    • 2014
  • On the basis of Hoek-Brown failure criterion, a numerical solution for the shape of collapsing block in the rectangular cavity subjected to seepage forces is obtained by upper bound theorem of limit analysis. The seepage forces obtained from the gradient of excess pore pressure distribution are taken as external loadings in the limit analysis, and the pore pressure is easily calculated with pore pressure coefficient. Thus the seepage force is incorporated into the upper bound analysis as a work rate of external force. The upper solution of the shape of collapsing block is derived by virtue of variational calculation. In order to verify the validity of the method proposed in the paper, the result when the pore pressure coefficient equals zero, and only hydrostatic pressure is taken into consideration, is compared with that of previous work. The results show good effectiveness in calculating the collapsing block shape subjected to seepage forces. The influence of parameters on the failure mechanisms is investigated.

불포화 사질토의 도로함몰 특성에 관한 실험적 연구 (Experimental Study on Road-Subsidence Characteristics in Unsaturated Sandy Soils)

  • 권기철
    • 한국도로학회논문집
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    • 제20권1호
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    • pp.19-25
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    • 2018
  • PURPOSES : The purpose of this study is to identify the road-subsidence mechanism in unsaturated sandy soils. METHODS : A series of soil chamber tests were conducted under various conditions. RESULTS : The cavity-expansion characteristics in unsaturated sandy soils due to seepage were affected by the outlet size, seepage intensity, relative density, and fine content. CONCLUSIONS : In unsaturated sandy soils, the cavity-expansion speed was affected by the outlet size, relative density, seepage intensity, and clay content; however, the cavity-expansion shape was very similar. As the outlet size and seepage intensity increased, the cavity-expansion speed increased. As the relative density increased, the cavity-expansion speed increased because of a sudden decrease in shear strength, resulting from the increased saturation (reduction of matric suction). The cavity expanded faster with the increasing clay content, up to a certain threshold. It expanded at a slower rate once it passed the threshold. Finally, it reached a stable state where the cavity did not expand due to seepage.

성토층 하부의 자갈층 유·무에 따른 침투특성 변화 (Seepage Characteristics of Embankment as with/without Gravel Layer under the Earth Fill)

  • 이행우;장병욱;장웅희;김시운
    • 한국농공학회논문집
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    • 제47권4호
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    • pp.53-61
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    • 2005
  • A series of laboratory tests was carried out fur analyzing of seepage characteristics of two-layers embankment model which consists of gravel and earth fill layers. Gravel layers were built under the earth fill for a half and one-third width of earth fill of the model. Permeability of earth fill was ranged between $5.00\times10^{-5}\~3.00\times10^{-4}\;m/s$.. The tests were performed with hydraulic gradients(i), $0.10\~0.55$. From the test results, hydraulic head of earth fill with gravel layer was 1.6 times higher than that of earth fill without gravel layer. Seepage rate was increased up to $4\~22$ times and safety factor for piping was decreased to $13\~43\;\%$ comparing the earth fill with gravel layer to that without gravel layer. The gravel layer under the earth fill could, in general, give some serious seepage problems to seadike embankment.

수두손실률, 투수계수 및 공극비의 상호관계를 통한 제체의 다짐상태 평가 (The Estimation of Compacted State on Sea Dike Embankment with the Interrelationships Between the Hydraulic Head Loss Rate, the Hydraulic Conductivity and the Void Ratio)

  • 임성훈
    • 한국농공학회논문집
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    • 제57권1호
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    • pp.11-23
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    • 2015
  • In this study the laboratory test for hydraulic conductivity and the seepage analysis with finite element method on measurement section of sea dike embankment were performed for the purpose of estimating the relative density of embankment from the measured pore water pressures, and both results of the test and the analysis were coupled with the method of estimating seepage blocking state with the hydraulic head loss rate in sea dike embankment. The relationship of void ratio vs hydraulic head loss rate was obtained by setting hydraulic conductivity as common ordinate on the relationships between the void ratio and the hydraulic conductivity and between the hydraulic conductivity and the hydraulic head loss rate. The void ratio on the segment between measuring points was calculated from the coupled relationship of the void ratio vs the hydraulic conductivity. The allowable upper and lower limits of hydraulic head loss rate and those of void ratio on the safety were generated from the coupled relationship between the laboratory compaction test and the sedimentation test. Current hydraulic head loss rate and void ratio were evaluated in the allowable range between upper and lower limits.

Analytical study on seepage behavior of a small-scale capillary barrier system under lateral no-flow condition

  • Byeong-Su Kim
    • Geomechanics and Engineering
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    • 제35권1호
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    • pp.13-27
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    • 2023
  • The model production for large-scale (lateral length ≥ 2.0 m) capillary barrier (CB) model tests is time and cost-intensive. To address these limitations, the framework of a small-scale CB (SSCB) model test under the lateral no-flow condition has been established. In this study, to validate the experimental methodology of the SSCB model test, a series of seepage analyses on the SSCB model test and engineered slopes in the same and additional test conditions was performed. First, the seepage behavior and diversion length (LD) of the CB system were investigated under three rainfall conditions. In the seepage analysis for the engineered slopes with different slope angles and sand layer thicknesses, the LD increased with the increase in the slope angle and sand layer thickness, although the increase rate of the LD with the sand layer thickness exhibited an upper limit. The LD values from the seepage analysis agreed well with the results estimated from the laboratory SSCB mode test. Therefore, it can be concluded that the experimental methodology of the SSCB model test is one of the promising alternatives to efficiently evaluate the water-shielding performance of the CB system for an engineered slope.

토사절토사면의 침투특성에 관한 연구 (A Study on the Infiltration Characteristics of Soil Cut-Slope)

  • 이정엽;구호본;김승현;배규진
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2005년도 춘계 학술발표회 논문집
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    • pp.735-738
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    • 2005
  • The purpose of this study is the infiltration characteristics of soil cut-slope by rainfall. Stability analysis of soil cut-slopes has been conducted by limit equilibrium method on Seep/w and finite element method on Slope/w. Result is same as following. First. the hour when seepage line and groundwater in contact is proportionate from rainfall rate condition and upper natural slope gradient condition which is identical. Second, when seepage line and groundwater is contact, seepage line moves gradually at soil cut-slope surface. Finally, seepage line is formed similarly with soil cut-slope gradient. Third, when rainfall is ended, from the recording upper natural slope where the hour will pass it is stabilized

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실험(實驗)과 FEM기법(技法)을 사용(使用)하여 구(求)한 침투유량(浸透流量)의 비교(比較) (Comparison of Seepage Quantity Calculated by Experiments and Finite Element Method)

  • 진병익;김재홍
    • 대한토목학회논문집
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    • 제5권2호
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    • pp.83-90
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    • 1985
  • 본(本) 논문(論文)은 제체(堤體)의 중앙심벽형(中央心壁型) model을 제작(製作)해서 상류측(上流側) 각(各) 수위(水位)의 변화(變化)에 대한 침투유량(浸透流量)을 실험(實驗)을 통하여 구하고, 이 때의 침윤선형상(浸潤線形狀)과 Equipotential line에 대하여도 고찰(考察)한 것이다. 또한 실험(實驗)에서 얻은 자료(資料)를 FEM기법(技法)을 사용하여 구한 유선망(流線網)의 각요소별(各要素別) Flow-rate에 대한 유속(流速)과 침투유량(浸透流量)을 실험치(實驗値)와 근사리론공식(近似理論公式)에서 산출(算出)된 값과 비교검토(比較檢討)하였다. 침투수량(浸透水量)은 고수위시(高水位時)에서는 실험치(實驗値)보다 FEM 값이 적게 나타났으며, 저수위시(低水位時)에는 거의 비슷한 값이었다. 그리고, 유선망(流線網)이 형성(形成)된 각(各) 요소별(要素別) Flow-rate 는 X, Z 축(軸)은 수위변화(水位變化)가 있어 흐름에 따른 유속(流速)이 크나 Y 축(軸)의 유속(流速)은 무시할 수 있을 정도의 적은 값이었다.

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확률론적 댐 침투거동 해석 (Stochastic Seepage Analysis of Dam)

  • 조성은
    • 한국지반공학회논문집
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    • 제22권4호
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    • pp.73-83
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    • 2006
  • 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. 지반의 불포화 수리특성은 변동성과 불확실성을 내포하고 있으며, 이는 침투수량 및 간극수압 분포 등 댐체 및 제방의 침투거동에 영향을 미친다. 본 연구에서는 댐의 심벽재료에 대한 함수특성곡선과 투수계수를 구하는 실내실험을 수행하였다. 그리고, 불포화수리특성이 댐체의 침투 거동에 미치는 영향을 살펴보기 위하여 입력물성의 확률론적 분포를 고려한 수치해석을 수행하였다. 해석결과 Fredlund와 Xing 함수특성곡선식과 Campbell의 투수계 수식에서 변수 a와 n은 값이 클수록, n과 p는 값이 작을수록 정상상태에서의 침투수량이 많았다.

진부지역 토석류발생 사면에 대한 침투 및 사면안정 연계해석 (Seepage and Slope Stability Analysis on the Site of Debris-flow at Jinbu Area)

  • 전경재;윤찬영;서흥석
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2009년도 세계 도시지반공학 심포지엄
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    • pp.369-376
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    • 2009
  • Field investigation was performed right after the occurrence of debris flow at Jinbu area. Geomorphic and geotechnical characteristics were investigated and rain fall data were collected. Based on these data, seepage and slope stability analysis was performed to verify the behavior of ground water and factor of safety of the slope according to the rainfall intensity and time. As a results, the minimum value of factor of safety achieved in long time after the moment of maximum precipitation rate. And it is confirmed that the factor of safety is susceptible to ground water level rather than rainfall intensity.

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