• 한국농공학회:학술대회논문집
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• 한국농공학회 1998년도 학술발표회 발표논문집
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• pp.87-91
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• 1998

Unused irrigation water due to delivery losses and overflow from paddies in an irrigation system, and groundwater releases from infiltration are eventually returned to stream. The estimate of irrigation returnflow is important to streamflow modeling and water resources planning. This study was to field monitor the irrigation water use, streamflow, lateral inflow and ground water level, and to determine the return flow of irrigation water

• Korean Journal of Hydrosciences
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• 제1권
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• pp.1-14
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• 1990

The analytical diffusion model is first formulated and its characteristics are critically reviewed. The flood events during the 1985-1986 flood seasons in the IHP Pyungchang Representative Basin are routed by this model and are compared with those routed by the kinematic wave model. The present model is proven to be an excellent means of taking the backwater effects due to lateral inflow or downstream river stage variations into consideration in channel routing of flood flows. It also requires much less effort and computing time at a desired station compared to any other reliable flood routing methods.

• 한국정밀공학회:학술대회논문집
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• 한국정밀공학회 2002년도 춘계학술대회 논문집
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• pp.124-127
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• 2002

Ceil embolisation technique has been used to treat the intracranial aneurysms. Microcoils inserted into the aneurysm sac induce the blood flow stagnation inside the aneurysm sac, which causes the thrombus formation and embolisation of aneurysm. Since the intraaneurysmal flow patterns affect the embolisation process, we want to measure the flow field for different locations of coil inside the aneurysm sac . Lateral aneurysm models are manufactured using rapid prototyping, and the velocity fields are measured using particle image velocitimeter. Distally blocked models showed less flow into the aneurysm sac comparing to proximally blocked models. Also blocking the neck of aneurysm showed better inflow blocking comparing to blocking the dome of aneurysm. These results suggest that distal neck should be the preferred locations of coil for aneurysm embolisation.

• International Journal of Precision Engineering and Manufacturing
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• 제5권1호
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• pp.42-46
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• 2004

Aneurysm embolization method using coils has been widely used. When partial blocking of an aneurysm is inevitable, the locations of coils are important since they change the flow patterns inside the aneurysm, which affect the embolization process. We calculated the flow fields inside the partially blocked lateral aneurysm models for different coil locations-proximal neck, distal neck, proximal dome and distal dome. Flow into the aneurysm sac was significantly reduced in the distally blocked models, and coils at the distal neck blocked inflow more effectively comparing to those at the distal dome. This study suggests that the distal neck should be the most effective location for aneurysm embolization.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2008년도 학술발표회 논문집
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• pp.2270-2275
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• 2008

수문학적 하도추적법의 하나인 Muskingum 모형은 미 육군공병단(U.S. Army Corps of Engineers)에 의해서 미국 Ohio 주의 Muskingum 유역에 홍수조절계획으로 처음 사용되었으며 모형의 구조 및 입력자료의 단순성에 비하여 비교적 우수한 결과를 모의할 수 있는 것으로 알려져 있다. 1938년 McCarthy에 의해서 개발되었고 구간내 총저류량은 prism 저류와 wedge 저류로 구분하여 prism 저류는 유출량에 wedge 저류는 유입량과 유출량의 차에 직접 비례한다는 가정하에 추적식을 개발하였다. 이후 지속적인 연구가 이뤄져 1985년 O'Donnel은 측방유입량(lateral inflow)을 상류단의 유입량에 비례하는 형태로 3-매개변수 muskingum 모형을 제안하여 추적계수의 결정을 선형대수(linear algebra)에서 동차(homogeneous)연립방정식 해를 구하는 Cramer 법칙인 matrix 기법을 적용하였다. 본 연구에서는 홍수사상으로부터 측방유입량이 고려되고 추적계수 결정에 있어서 직접 계산이 가능한 O'Donnel(1985)이 제안한 3-매개변수 muskingum 모형을 적용하였다. 추적계수들의 결정은 직접 matrix 기법을 적용하였고 적용대상은 낙동강 유역의 낙동 지점을 상류단으로 구미 지점을 하류단으로 선정하였다. 홍수사상은 낙동강 유량측정 조사사업 2005년${\sim}$2007년 보고서에 수록된 수문자료를 선정하여 관측치와 계산치를 비교하였고 홍수사상에 적용하여 수문곡선을 추정하였으며, 각각의 매개변수가 추적구간에 어떠한 영향을 미치는지 변수간의 관계를 분석하였다. 또한, 관측치와 계산치의 적합도 검증은 평균제곱근오차(root mean squar error; RMSE)와 모형 효율성 계수(model efficiency; ME)를 산정하여 분석하였으며, 하도 구간내 저류량은 대상구간에 대한 유입량과 유출량의 가중합에 비례한다는 선형모형을 적용하였다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2023년도 학술발표회
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• pp.125-125
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• 2023

Estuarine dams are dams constructed in estuaries for reasons such as securing freshwater resources, controlling water levels, and hydroelectric power generation. These estuarine dams alter the flow of freshwater to the coastal ocean and the tidal properties of the estuaries which has implications for the estuaries' circulation and sediment transport. A previous study has analyzed the effect of estuarine dams on 1D (along-channel) circulation and sediment transport. However, the effect of estuarine dams on the transverse variability of along-channel and across-channel circulation and sediment transport has not been studied and is not known. In this study, a coupled hydrodynamic-sediment dynamic numerical model (COAWST) was used to analyze the transverse variability of along-channel and across-channel flow and sediment transport in estuaries with estuarine dams. The estuarine dam was found to change the 3D structure of circulation and sediment transport, and the result was found to depend on the estuarine type (i.e., strongly stratified (SS) or well-mixed (WM) estuary). The SS estuary had inflow in the channel and outflow over the shoals, consistent with estuarine circulation. Longer discharge interval reduced the estuarine circulation. The WM estuary had inflow over the shoals and outflow in the channel, consistent with tide-induced circulation. As the estuarine dam was located nearer to the estuary mouth, the tide-induced circulation was reduced and replaced with estuarine circulation. The lateral circualtion was the greatest in the tide-dominated estuaries. It was reduced and changed direction due to differential advection change as the dam was located nearer the mouth. Overall, the WM estuary transverse flow structure changed the most. Lateral sediment flux was important in all estuaries, particularly for transporting sediments to the tidal flats.

• 한국물환경학회지
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• 제29권1호
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• pp.97-106
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• 2013

The temporal and spatial variations of water quality in a stratified reservoir are fully dependent on the characteristics of inflow loading from its watershed and the transport regimes of pollutants after entering the reservoir. Because of the meteorological and hydrological conditions in Korea, the pollutants loading to reservoirs are mostly occur during rainfall events. Therefore it is important to understand the characteristics of pollutants loading from upstream rivers and their spatial propagation through the stratified reservoir during the rainfall events. The objectives of this study were to characterize the water quality variations in upstream rivers of Imha Reservoir during a rainfall event, and the transport and spatial variations of pollutants in the reservoir through extensive field monitoring and laboratory analysis. The results showed that the event mean concentration (EMC) of SS, BOD, $COD_{Mn}$, T-N, T-P, $PO_4-P$ are 8.6 ~ 362.1, 2.5 ~ 5.1, 1.5 ~ 5.1, 1.1 ~ 1.9, 8.3 ~ 57.1, 5.6 ~ 25.7 times greater than the mean concentrations of these parameters during non-rainfall period. The turbidity and SS data showed good linear correlations, but the relationships between flow and SS showed large variations because of hysteresis effect during rising and falling periods of the flood. The ratio of POC to TOC were 12.6 ~ 14.7% during the non-rainfall periods, but increased up to 28.2 ~ 41.7% during the flood event. The turbid flood flow formed underflow and interflow after entering the reservoir, and delivered a great amount of non-point pollutants such as labile and refractory organic matters and nutrients to the metalimnion layer of reservoir, which is just above the thermocline. Spatially, the lateral variations of most water quality parameters were marginal but the vertical variations were significant.

• 대한의용생체공학회:의공학회지
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• 제25권4호
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• pp.295-300
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• 2004

코일을 동맥류에 삽입하여 동맥류 내부 유동 정체를 유발하므로 동맥류를 치료 방법이 최근 많이 사용되고있다. 동맥류의 내부를 코일로 완전히 채우지 못하고 부분 폐색할 경우가 발생하며, 동맥류의 부분 폐색 위치에 따라 혈류 유동이 변하므로 이는 동맥류 내부의 혈전 형성에 영향을 미필 수 있다. 또한 동맥류가 발생한 모혈관의 형상에 따라 동맥류로 유입되는 유동 특성이 변하므로, 모혈관의 형상에 따라 효율적인 동맥류 폐색을 위한 코일의 위치가 변할 수 있다. 효율적인 동맥류 폐색을 위한 코일 위치를 제시하기 위하여 내경 동맥에서 발생한 측방 동맥류의 부분 폐색위치와 내경 동맥의 형상에 따른 동맥류 내부 유동장을 수치해석을 이용하여 해석하였다. 3차원 맥동 유동장은 혈액의 비뉴톤성 점성 특성을 고려하여 계산되었다. 또한 동맥류 폐색에 영향을 미치는 유체역학적 인자인 동맥류 유입 유량 및 벽전단응력을 계산하였다. 코일은 동맥류 목에 삽입하였을 경우에는 천정부에 삽입한 경우에 비해 동맥류 내부로 혈류의 유입을 감소되었다. 임계 벽전단응력 이하의 저 전단응력지역은 곡선형 모혈관에 비해 직선형 모혈관에서 컸으며, 원위부 목 폐색 모델에서 가장 크게 나타났다. 따라서 동맥류 원위부 목은 동맥류 내부로의 혈류 유입이 감소하고, 저 전단응력 지역을 크게하는 코일 위치이므로, 이 위치는 동맥류 색전술시 혈전의 형성으로 인한 동맥류 폐색에 적합한 위치로 예상된다.

• 한국물환경학회지
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• 제27권5호
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• pp.699-709
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• 2011

The uses of multi-dimensional hydrodynamic and water quality models are increasing to support a sustainable management of large dam reservoirs in Korea. Any modeling study requires selection of a proper spatial dimension of the model based on the characteristics of spatial variability of concerned simulation variables. For example, a laterally averaged two-dimensional (2D) model, which has been widely used in many large dam reservoirs in Korea, assumes that the lateral variations of hydrodynamic and water quality variables are negligible. However, there has been limited studies to give a justification of the assumption. The objectives of this study were to present the characteristics of spatial variations of water quality variables through intensive field monitoring in Daechung Reservoir, and provide information on a proper spatial dimension for different water quality parameters. The monitoring results showed that the lateral variations of water temperature are marginal, but those of DO, pH, and conductivity could be significant depending on the hydrological conditions and local algal biomass. In particular, the phytoplankton (Chl-a) and nutrient concentrations showed a significant lateral variation at R2 (Daejeongri) during low flow periods in 2008 possibly because of slow lateral mixing of tributary inflow from So-oak Stream and wind driven patchiness.

• 한국수자원학회논문집
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• 제49권5호
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• pp.391-398
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• 2016

하천의 합류부 구간은 본류와 지류에서 유입되는 유량의 크기가 달라 복잡한 흐름을 형성하게 되며 이러한 흐름으로 인한 국부적인 구간에서의 하상변동 및 하안침식은 하도의 평면적 변화를 야기할 수 있다. 본 연구에서는 이러한 합류부 구간에서의 평면적 하도변화를 분석하기 위해 남한강과 금당천 합류부 지점을 대상으로 하상 퇴적 및 하안침식에 의한 하안선 이동을 2차원 수치모형인 CCHE2D를 활용하여 모의하였다. 모의결과, 본류의 좌안에서는 합류 전 구간에 비해 합류 후 구간에서의 하안선 이동 현상이 더 크게 발생한 것을 확인할 수 있었다. 또한 지류에서의 하안침식은 거의 발생하지 않으며, 지류 좌안과 합류 전 본류 우안에서는 유속 저하와 퇴적으로 인해 하안선이 제외지 쪽으로 이동하는 것을 확인하였다.