• 한국방재학회 논문집
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• 제8권2호
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• pp.129-138
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• 2008

차수성이 요구되는 제체나 댐체에 대하여 안정성을 판단하고자 할 경우 파이핑 현상발생 여부를 검토한다. 제체나 댐체는 층 다짐을 수행하면서 축조되므로 투수성은 수평방향 투수계수($k_x$)와 연직방향 투수계수($k_y$)가 서로 다른 이방성이 될 수 있다. 본 연구에서는 여러 가지 투수계수 비(k-ratio=$k_y/k_x$k)에 따른 침투해석을 수행하여 유출동수경사와 침투유속을 파악하고, 이론식에 의한 한계동수경사와 경험식에 의한 한계유속과 각각 비교.검토하여 파이핑에 미치는 영향을 검토하였다. 연구결과 투수계수 비는 한계동수경사 개념으로 파이핑 현상발생에 대한 안정성을 검토할 경우 매우 중요한 요소로 작용하나, 한계유속 개념에 대해서는 상대적으로 중요도가 매우 낮은 것으로 확인되었다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2006년도 춘계 학술발표회 논문집
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• pp.800-807
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• 2006

Sea dyke construction is simply defined that the cutting procedure of sea water flow. Sea dyke construction is more difficult than in-land construction because it’s placed on deep seabed and exposed sea wave attack. Especially, the final closure of sea dyke is most dangerous due to the fast velocity of tidal flow. The final closure section is consisted with vast rubble and heavy stone gabion, therefore the discharge velocity at land side of final close section is irregularly and sometime occur the fast discharge velocity. In this study, the seepage model test performed to evaluate seepage behavior with tidal variation of final closure and continuous sea dyke section such as discharge velocity, hydraulic gradient, and phreatic line. Based on the seepage model test results, the maximum discharge velocity of final closure section is 1.7m/sec. Also the local discharge velocity increment and vortex is occurred.

• 한국지반환경공학회 논문집
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• 제16권6호
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• pp.39-43
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• 2015

This study extends the Distributed Temperature Sensing (DTS) application to delineate the saturated zones in shallow sediment and evaluate the groundwater flow in both downward and upward directions. Dry, partially and fully saturated zones and water level in the subsurface can be recognized from this study. High resolution seepage velocity in vertical direction was estimated from the temperature data in the fully saturated zone. By a single profile, water level can be detected and seepage velocity in saturated zone can be estimated. Furthermore, thermal gradient analysis serves as a new technique to verify unsaturated and saturated zones in the subsurface. The vertical seepage velocity distribution in the recognized saturated zone is then analyzed with improvement of Bredehoeft and Papaopulos' model. This new approach provides promising potential in real-time monitoring of groundwater movement.

• 한국안전학회지
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• 제14권4호
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• pp.158-167
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• 1999

In parallel flow condition, to estimate the stability of the extended embankment constructed on a permeable foundation ground, a laboratory model test was performed due to extended materials and water level increasing velocity of a flood period. A laboratory model test was peformed for different permeability coefficients ($K_1=2.0{\times}10^{-5}cm/sec,\;K_2=1.5{\times}10^{-4}cm/sec,\;K_3=2.3{\times}10^{-3}cm/sec$) using seepage. The fluctuation of water level occurring to an extended embankment was analyzed by laboratory model tests as vary the increasing velocity of water level with 0.6cm/min, 1.2cm/min, 2.4cm/min respectively. In analysis results, the increase of water level into embankment occurs rapidly because seepage water moving along with a permeable soil flow into embankment. The larger the permeability coefficient of an extended part is the longer initial seepage distance, and the exit point of downstream slope is gradually increased and then shows unstable seepage behavior as occurring partial collapse. As the increasing velocity of water level increase, the initial seepage line is formed low, and the discharge increases. Therefore, the embankment extended by a lower permeable soil than existing embankment shows stable seepage behavior because an existing embankment plays a role as filter for an extended part.

• 한국안전학회지
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• 제11권2호
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• pp.109-115
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• 1996

The movement of water through a river embankment and its influenced upon the stability of the slope of the embankment are described. The stability of the embankment is depended upon the location of seepage line. As the seepage flow occurs in the embankment, the slope of the embankment loses its stability. Of particular interest is the stability following a rapid change of water level. The variation of seepage line in the embankment model by a fluctuation of water level is discussed. The experimental models were construction with slopes of 1 : 1.5, 1 : 2.0, 1 : 2.5 and the flow velocity was turned from 60cm/sec~90cm/sec. Based on the experimental study, the following conclusions are drawn. 1) When water level is raised, the seepage line of downstream slope Is raised rapidly as flow velocity increases. 2) For the case of permeable layer, the seepage line raised rapidly as compare with impermeable layer when water lever is raised.

• 한국지반신소재학회논문집
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• 제5권1호
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• pp.25-32
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• 2006

방조제 공사는 바다를 막아 바닷물의 흐름을 차단해가는 과정으로 육상공사와는 달리 수심이 깊고 파랑이 심한 바다에서 이루어지는 공사이기 때문에 축조재료의 유실이 많고 심할 경우 방조제가 붕괴되는 위험이 큰 공사이다. 특히, 방조제의 끝막이 단면은 대규모 사석과 돌망태 등을 이용하여 시공하므로, 구성 재료가 불규칙하고 간극이 크기 때문에 일반적인 지반내의 침투흐름보다 상당히 빠른 침투가 발생된다. 본 연구에서는 방조제 끝막이 후 축조된 사석단면과 후속공정을 통하여 축조되는 방조제단면에 대한 실내 침투모형시험을 수행하여 침투거동을 예측 및 분석하였다. 다양한 조위변화를 재현하여 근고공 필터매트 시공에 따른 사석단면내의 유속변화, 침윤선 분포 등을 계측하여 침투거동을 분석하였다. 실내 침투모형시험 결과, 끝막이 사석단면의 침투유속은 최대 1.7m/sec 발생하였으며, 근고공 필터매트 시공에 따라 최대 침투유속이 23.7% 감소하였다.

• 한국안전학회지
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• 제15권1호
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• pp.146-152
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• 2000

To estimate the behavior of reinforced and unreinforced embankment constructed on a impermeable foundation ground, a laboratory model test was performed for two types of soils and water level increasing velocity of a flood period. The experiment models were constructed with slopes of water level is 1.25cm/min, 2.5cm/min each. From model test results, as the slope of reinforced and unreinforced embankment was the slower, the more seepage line rised. In the unreinforced embankment, the rising velocity of water level was the faster, the larger the embankment failure was. And the reinforced embankment with geotextile was the more safe than the unreinforced embankment for seepage force.

• 대한토목학회논문집
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• 제14권5호
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• pp.1253-1263
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• 1994

수평흐름에 의한 제체내의 비정상침투류를 실험을 통하여 구명한 것으로 흐름의 속도와 수위의 변동에 따른 제체내에서의 침투류영향을 고려하므로써 하천제방의 안정성증대에 목적을 두었다. 실험은 투수계수가 서로 다른 3가지 모델($K_1=3.52{\times}10^{-1}cm/sec$, $K_2=1.94{\times}10^{-1}cm/sec$, $K_3=4.19{\times}10^{-2}cm/sec$)에 대하여, 각기 흐름의 속도를 60, 70, 80, 90 cm/sec로 변화시키고 동시에 수위를 상승 또는 하강시키는 방법으로 제체내에 발생하는 수위변화를 실험을 통하여 분석하였다. 분석결과 제체내의 침투현상은 제체의 투수계수가 크고, 흐름의 속도가 작을수록 유속의 변화에 따른 영향을 많이 받음을 알 수 있으며, 제외지 수위의 상승과 강하에 따른 배면부 및 표면부에서의 수위가 유속의 영향에 따라 변화함을 알 수 있다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2008년도 추계 학술발표회
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• pp.1727-1734
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• 2008

After the final closure of sea dyke, seepage behaviour of embankment is highly changed by variation of water head different between tide wave and controlled water level at fresh lake. Especially, the seepage behaviour of bottom protection layer of final closure section is more important factor for structural and functional stability of sea dyke, because of the bottom protection layer of final closure section is penetrated sea side to fresh lake. Even though bottom protection layer was filled with dredged fine sand, it has a high permeability. In this paper, mainly described about the seepage velocity and borehole image of bottom protection layer filled with dredged sand after final closure. Various in-situ tests such as BIPS (Borehole Image Processing System) and ABI (Acoustic Borehole Imager) survey, wave velocity measuring, and color tracer survey were conducted to evaluate the seepage behavior of bottom protection layer. Based on the in-situ tests, the bottom protection layer of final closure section was almost filled with dredged sand which is slightly coarse grain sand and there have sea water flow by water head different between tide wave and controlled water level at fresh lake. Also, comply with tracer survey results, the sea water flow path was not exist or generated in the bottom protection layer. However, because of this result not only short term survey but also just one test borehole survey results, additional long term and other borehole tests are needed.

• 한국지반환경공학회 논문집
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• 제2권2호
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• pp.51-58
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• 2001

본 연구에서는 보강제체와 무보강제체의 침투거동을 평가하기 위하여 실내모형실험을 실시하였다. 제체침투시험은 사면경사가 1:1.5, 1:2.0이고 수위상승속도가 1.25cm/min, 2.5cm/min, 수위는 15cm, 25cm, 35cm인 조건에서 실시하였다. 모형실험결과 보강재를 사용한 제체의 경우 지하수의 흐름과 상승 때문에 어느 정도의 침하와 수평방향변위가 발생하였으나, 무보강제체에서 나타난 커다란 활동파괴는 발생되지 않았다. 그리고 수위상승속도 변화에 따른 제체의 침투거동분석결과 Geotextile로 보강된 제체가 무보강제체보다 최종침하량이 감소하는 것으로 나타나 Geotextile을 설치한 제체가 비교적 물의 침투력에 대해 안정한 것으로 나타났다.