• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2005년도 총회 및 춘계학술발표회
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• pp.324-327
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• 2005

지하수와 지표수를 연계하여 flow와 transport를 모의하는 프로그램인 HydroSphere를 Canada Ontario주의 Canadian Forces Base Borden에서의 실험 (Abdul ,1985) 자료를 이용하여 평가해 보았고, 유성지역 소유역에서의 강수, 지표수, 지하수의 수소동위원소 모니터링 (박준형, 고용권, 박경우, 정형재, 김교원, 2003) 자료를 이용하여 평가해 볼 예정이다.

• 한국농공학회지
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• 제37권5호
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• pp.53-61
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• 1995

Analyses of subsurface drainage effects of farmland with respect to pipe and envelop material are made by the laboratory experiments using soil box to give basic information for the subsurface drainage system planning and design. Three different diameter PVC perforated pipes and a mesh pipe are used with envelop materials such as sand, rice bran, and crushed stone. Steady state subsurface drainage flow rate increased as envelop material changed from sand to rice bran and crushed stone. This indicates that as the hydraulic conductivity of the envelop material increases, the drainage flow rate increases. On the other hand, for a given envelop material, the mesh pipe which has the largest openning area shows the largest flow rate while small diameter PVC pipes show small flow rates. This tells that as the openning area and pipe diameter increase, the flow rate increases, too. Therefore, selection of pipe and envelop material should be made in accordance with the design drainage flow rate. Unsteady state subsurface drainage flow rate with respect to time differs for different envelop material. In case the sand was used as an envelop material, the small diameter PVC pipes show larger flow rates than the large diameter PVC pipe and mesh pipe. When the rice bran was used, the mesh pipe shows the largest flow rate, while small diameter pipes show smaller flow rates. In case the crushed stone was used as an envelop material, the large diameter PVC pipe and mesh pipe show larger flow rates, while small diameter pipes show a little bit smaller flow rates. However, the variation of flow rates among different pipes is the smallest when the crushed stone is used. The flow rate curve with respect to the pipe changes little for the crushed stone envelop which has a large hydraulic conductivity, while that changes much for the sand and rice bran envelops. However, it is difficult to draw a consistent relationship between the drainage flow rate and pipe for all the envelop materials. Since the subsurface drainage experiments are made only under the restricted laboratory condition in this study, further study including field experiment is required.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2015년도 학술발표회
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• pp.281-281
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• 2015

Shallow landslide often occurs in areas of this topography where subsurface soil water flow paths give rise to excess pore-water pressures downslope. Recent hillslope hydrology studies have shown that subsurface topography has a strong impact in controlling the connectivity of saturated areas at the soil-bedrock interface. In this study, the physically based SHALSTAB model was used to evaluate the effects of three soil thicknesses (i.e. average soil layer, soil thickness to weathered soil and soil thickness to bedrock soil layer) and subsurface flow reflecting three soil thicknesses on shallow landslide prediction accuracy. Three digital elevation models (DEMs; i.e. ground surface, weathered surface and bedrock surface) and three soil thicknesses (average soil thickness, soil thickness to weathered rock and soil thickness to bedrock) at a small hillslope site in Jinbu, Kangwon Prefecture, eastern part of the Korean Peninsula, were considered. Each prediction result simulated with the SHALSTAB model was evaluated by receiver operating characteristic (ROC) analysis for modelling accuracy. The results of the ROC analysis for shallow landslide prediction using the ground surface DEM (GSTO), the weathered surface DEM and the bedrock surface DEM (BSTO) indicated that the prediction accuracy was higher using flow accumulation by the BSTO and weathered soil thickness compared to results. These results imply that 1) the effect of subsurface flow by BSTO on shallow landslide prediction especially could be larger than the effects of topography by GSTO, and 2) the effect of weathered soil thickness could be larger than the effects of average soil thickness and bedrock soil thickness on shallow landslide prediction. Therefore, we suggest that using BSTO dem and weathered soil layer can improve the accuracy of shallow landslide prediction, which should contribute to more accurately predicting shallow landslides.

• 한국방재학회 논문집
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• 제8권2호
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• pp.59-63
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• 2008

지표수 흐름은 육지 물수지 계산에 중요한 요소중에 하나이다. 그러나, 기상변화의 예측과 그로 인한 방재대책수립을 위한 대규모의 기상모형과 연계되는 육지수문모형(Land Surface Model, LSM)들은 지표수 흐름을 토양수분수지로부터 간단하게 산정하고 있다. 침투계산에서 지표수 흐름깊이를 무시하는 것은 지표면 및 지표하 물흐름 모두에 계산상 오류를 초래할 수 있다. 그러므로, 육지수문모형에서 종합적인 물과 에너지 순환 예측을 하기 위해, 지표수 흐름을 위한 1차원 확산모형과 지표하 물흐름을 위한 계산망 체적평균 토양수분이송(Volume Averaged Soil-moisture Transport Model, VAST)모형을 연계하는 대규모 지표면 및 지표하 연계 물흐름 모형이 개발되었다. 이 논문에서는, 최첨단 육지수문모형중 하나인 CLM(Common Land Model)내의 지표수리수문 모의를 위한 주요부분을 비롯하여, 지형특성에 따른 지표수 흐름과 공간적 토양수분 분포의 예측개선을 위한 새로운 지표면 및 지표하 연계 물흐름 모형에 대해 기술하였다.

• 한국가시화정보학회지
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• 제17권2호
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• pp.73-82
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• 2019

The subsurface vortex - which occurs inside the cylindrical sump - was visualized through Computational Fluid Dynamics (CFD) and experiment. The analysis of subsurface vortex inside the cylindrical sump was already carried out using CFD techniques by the first author. To understand the subsurface vortex more clearly, an experimental analysis was carried out with a 1/5th scale model; and the flow rate was calculated according to the similarity law. The experimental results of vortex visualization matches well with the CFD results. The surface roughness model and Anti Vortex Device (AVD) model have been investigated to control the subsurface vortex. For the case of average surface roughness of 1mm and 5mm, the subsurface vortex appears and the vorticity is higher when compared to that of a smooth surface condition. However, for the AVD model, the subsurface vortex is completely removed and the internal flow is stabilized.

• 한국환경복원기술학회지
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• 제14권5호
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• pp.69-79
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• 2011

This study assessed the subsurface runoff and peak flow reduction in rain gardens. The results showed that the highest water retention was found in rain garden mesocosms in which Rhododendron lateritium and Zoysia japonica were planted, followed by mesocosms in which either R. lateritium or Z. japonica was planted, and the lowest water retention rate was found in non-vegetated control treatment mesocosms(${\alpha}$ < 0.05). Although higher rainfall intensity caused a decrease of peak flow reduction in both vegetated and non-vegetated treatments, peak flow reduction was the greatest in mesocosms with mixed plants. A rain garden can be an effective tool for environment-friendly stormwater management and improving ecological functions in urban areas. Depending on the purpose such as delaying runoff or increasing infiltration, various plant types should be considered for rain garden designing.

• Journal of Mechanical Science and Technology
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• 제19권8호
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• pp.1582-1596
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• 2005

Groundwater flow and behavior have to be investigated based on heterogeneous subsurface formation since the homogeneity assumption of this formation is not valid. Over the past twenty years, stochastic approach and Monte Carlo technique have been utilized very efficiently to understand the groundwater flow behavior. However, these techniques require lots of computational and numerical efforts according to the various researchers' comments. Therefore, utilizing new techniques with much less computational efforts such as Artificial Neural Network (ANN) in the prediction of the stochastic behavior for the groundwater based on heterogeneous subsurface formation is highly appreciated. The current paper introduces the ANN technique to investigate and predict the stochastic behavior of a well draw down in a confined aquifer based on subsurface heterogeneous hydraulic conductivity. Several ANN models are developed in this research to predict the unsteady two dimensional well draw down and its stochastic characteristics in a confined aquifer. The results of this study showed that ANN method with less computational efforts was very efficiently capable of simulating and predicting the stochastic behavior of the well draw down resulted from the continuous constant pumping in the middle of a confined aquifer with subsurface heterogeneous hydraulic conductivity.

• 한국수자원학회논문집
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• 제45권1호
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• pp.39-52
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• 2012

유역내에서 발생하는 유출은 지표 유출과 지표하 유출이 있으며, 서로 상호작용 상태를 유지하게 된다. 일반적으로 지표와 지표하 둘 중 한 가지 알고리즘으로 해석이 힘든 유역에 대해 지표와 지표하 사이의 동적인 관계를 상세하게 모의해야 하는 경우 상호작용에 관한 요소를 고려하여야 한다. 동적인 상호작용 시스템의 구동에서는 시 공간적인 매개변수가 중요하며, 적절한 모의를 위해시 공간적인 매개변수는 시스템 상에서 지표와 지표하 항에 대한 복합적인 메카니즘으로 구성되어야 한다. 본 연구에서는 이러한 지표 및 지표하 유출의상호작용에 관한 알고리즘을 위해 2차원 확산파 방정식을 이용하여 지표 유출을 해석하고, Darcy의 법칙과 Dupuit-Forchheimer의 가정을 이용한 Boussinesq 방정식을 적용하여 포화상태의 지표하 유출의 알고리즘을 구성하였다. 커플링 방정식으로 공간에 대해서는 유한체적법을 사용하고, 시간에 대해서는 Crank-Nicolson 방법을 이용하였으며, 지표와 지표하 흐름의 상호작용에 대해서는 질량보존의 법칙에 기반하여 구성하였다. 이상의 과정을 통하여 지표 유출해석, 지표하 유출해석, 상호작용, 수치해석 부분의 4가지 주요 모듈을 만들었으며, 4가지 주요 모듈을 통합하여 복합유역의 지표 및 지표하 유출해석 모듈을 개발하였다.

• 유체기계공업학회:학술대회논문집
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• 유체기계공업학회 2005년도 연구개발 발표회 논문집
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• pp.593-597
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• 2005

In order to study the characteristics of the subsurface vortex the flow fields of the three pump sump models were analysed by the numerical simulation. The calculation results show that there are circulation flows in the pump sump model and maximum vorticity strength which make iso-surface from the wall to the pump inlet could be used for predicting the subsurface vortex generation. Also, the flow field for the sump model with anti-vortex devices simulated and the results shows that there is no vorticity value which make iso-surface from the sump wall to the pump inlet.

• 대한지리학회지
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• 제41권6호
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• pp.670-681
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• 2006

본 연구는 산림이 잘 보존되고 있는 경기도 구리시 동구릉 지역 내의 완사면 곡두부 지점에서의 호우시 지중수 유출과 지형형성 프로세스를 규명하고자 실시되었다. 본 연구 결과 'U자골' 곡두부의 경우 20mm 이하의 강우시에는 지하수위 변화가 거의 없었으나 곡두사면과 그 상부 지점에서는 총강우량과 강우강도에 의해서 지하수위가 크게 변화하고 있는 것으로 나타났으며, 그 변동 폭은 선행강우량과 그 경과시간, 그리고 강우지속시간과 밀접한 관계가 있는 것으로 확인되었다. 이러한 현상에 영향을 미치는 요인으로는 강우시 형성된 사면의 유출특성, 즉 지하수위 상승에 기인한 복귀류 발생과 'U자골' 곡두사면을 따라 빠르게 흐르는 측방류를 들 수 있으며 이러한 지중수의 흐름은 'U자골' 지형발달에 중대한 영향을 미친다. 사면 곡두부 지형은 지중수에 의해 변형되고 있음을 알 수 있다.