• Journal of Korea Water Resources Association
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• v.44 no.7
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• pp.553-563
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• 2011

According to the improvement of computer's performance, the development of Geographic Information System (GIS), and the activation of offering information, a distributed model for analyzing runoff has been studied a lot in recently years. The distribution model is a theoretical and physical model computing runoff as making target basin subdivided parted. In the distributed model developed by this study, the volume of runoff at the surface flow is calculated on the basis of the parameter determined by landcover data and a two-dimensional diffusion wave equation. Most of existing runoff models compute velocity and discharge of flow by applying Manning-Strickler's mean velocity equation and Manning's roughness coefficient. Manning's roughness coefficient is not matched with dimension and ambiguous at computation; Nevertheless, it is widely used in because of its convenience for use. In order to improve those problems, this study developed the runoff model by applying not only Manning-Strickler's equation but also Chezy's mean velocity equation. Furthermore, this study introduced a power law of exponential friction factor expressed by the function of roughness height. The distributed model developed in this study is applied to 6 events of fan-shape basin, oblong shape test basin and Anseongcheon basin as real field conditions. As a result the model is found to be excellent in comparison with the exiting runoff models using for practical engineering application.

• Journal of Korea Water Resources Association
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• v.49 no.6
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• pp.459-467
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• 2016

LISFLOOD-FP model in which channel flows are resolved separately from the floodplain flows using either a kinematic or diffusive wave approximation has been used to analyze flooding behavior on the lower Mankyung River influenced by backwater. A calibration and validation process was applied using the previous flood events to assess the model performance. Sensitivity analysis was conducted for main calibrated parameters, such as Manning roughness coefficient and downstream boundary condition. Also, we examined the effect of warm-up for the initial conditions. The results show that the computed hydrograph is in good agreement with measured data on the study reach, even though it was a hydrologic kinematic wave model. The sensitive analysis show that the difference between the computed results may be greater depending on the used calibrated parameters and that the sufficient calibration/validation process against various flood events is necessary. If the flood inundation simulation is performed using the validated model, it is expected to be able to contribute about river planning and policy decision-making for flood damage reduction.

• Journal of the Korean Society of Propulsion Engineers
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• v.7 no.3
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• pp.45-52
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• 2003

Detailed flowfield resulting from the secondary sonic gas injection into a divergent section of supersonic conical nozzle has been numerically investigated. The three-dimensional flowfield associated with the bow-shock/boundary-layer interaction inside the nozzle has been solved by Reynolds-averaged Navier-Stokes equations with an algebraic and $\kappa$-$\varepsilon$ turbulence model. The numerical results have been compared with the experimental results for the identical flow conditions, and it is shown that the comparison is satisfactory Effects of different injection pressures of the secondary jet on the shock/boundary-layer interactions and the overall flow structure inside the nozzle have been investigated. The vortex structures behind the shock interaction and wall pressure variations have also been studied.

• Proceedings of the Korean Society of Propulsion Engineers Conference
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• 2011.04a
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• pp.457-462
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• 2011

This paper presents a numerical investigation of deflagration to detonation transition (DDT) induced by shock wave and flame interaction in ethylene-air mixtures. Also shows the change of DDT triggering time by wall cooling effect. A model is consisted of the compressible reactive Navier-Stokes equations. And the effect of viscosity, thermal conduction, molecular diffusion, chemical reaction and wall effect are included. Using this model, the generation of hot spot by repeated shock and flame interaction, occurrence of detonation, and wall cooling effect of detonation confining boundaries are studied.

• Proceedings of the Korea Water Resources Association Conference
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• 2021.06a
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• pp.245-245
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• 2021

해양으로 유출된 5 mm 이하의 크기로 분해된 미세플라스틱이 해양 환경 오염의 주요 원인으로 자리잡았다. 최근에는 청정해역으로 알려진 남극해에서도 발견되고 있어 남극해에 잔류하는 미세플라스틱 오염 수준을 이해하기 위해 노력하고 있다. 하지만, 파랑의 효과를 고려한 남극해의 해수 순환 구조와 미세플라스틱의 고유 특성을 반영한 미세플라스틱의 거동 및 공간적 분포에 대한 복합적 이해는 상대적으로 부족하다. 남극해에서 발견된 미세플라스틱은 과학기지들의 방류수나, 조사선 등과 같은 인위적인 활동으로 인해 집적될 수 있으며, 특히 영구적으로 거주하는 과학기지에서 흘려보내는 방류수에 포함된 미세플라스틱은 과학기지 주변 해수 오염에 직접적인 영향을 줄 것으로 예상된다. 따라서, 본 연구에서는 파랑 효과에 따른 남극 킹조지 섬(King George Island)에 위치한 세종과학기지의 방류수에 포함된 미세플라스틱의 이송에 대해 모의하였다. 세종과학기지가 위치한 킹조지 섬과 넬슨 섬(Nelson Island) 사이의 멕스웰 만(Maxwell Bay)의 해수 흐름을 재현하기 위하여 해수 유동 모델(Delft3D-FLOW)이 사용되었다. 또한, 해수 유동 모델에 파랑 모델(Delft3D-WAVE)을 결합하여 파랑의 효과가 미세플라스틱의 이송에 미치는 영향을 확인하였다. 세종과학기지의 방류수가 흘러나가는 마리안 소만(Marian Cove)의 유속장을 바탕으로 이송, 확산, 입자의 침강 속도를 고려하여서, 세종과학기지에서 밀물 시 방출한 입자를 라그랑지안 입자 추적(Lagrangian Particle Tracking) 방법을 이용해 추적하였다. 해수의 밀도보다 가벼운 플라스틱의 경우 해수 표층의 흐름을 따라 소만 내부로 이송되어 해안선에 도달하고, 해수의 밀도보다 무거운 플라스틱의 경우 소만 내부로 이송되나 입자의 침강 속도로 인해 방출 위치 근처에서 집적된다. 파랑의 효과를 고려하게 되면, 고려하기 전보다 두 종류의 미세플라스틱 모두 소만 내부로 더 멀리 이송되는데, 이는 파랑으로 인한 힘(wave-induced force)이 해수 유동 모델의 운동방정식에 추가되며 파랑 에너지 분산으로 인해 해수 흐름에 변화를 준 것으로 보인다.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.5 no.4
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• pp.357-368
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• 1993

With the assumption of the diffusion dominated flow, a numerical model has been developed for undertow and turbulence structure under the breaking wave by using the $textsc{k}$-$\varepsilon$ turbulence model. Undertow is a strong mean current which moves seqwards below the level of wave trough in the surf zone. The turbulence, generated by wave breaking in the roller, spreads and dissipates downwards. The governing equations are composed of the equation of motion with the period-averaged shear stress due to waves; $textsc{k}$- and $\varepsilon$-equations with the turbulence energy Production due to wave breaking. They are discretised by the three-level fully implicit scheme, which can be solved by using Thomas algorithm. The model gives good agreements with measurements except for the station that is closest to the breaking point.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.6 no.3
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• pp.234-244
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• 1994

Longshore currents driven by monochromatic waves have been described using 2-equation $textsc{k}$-ι turbulence transport model. When using $textsc{k}$-ι closure both profiles of eddy viscosity and current velocity are found to be satisfactory. Several terms of ι equation are related to various variables concerned with turbulence mechanism. New form of turbulence frequency used in ι equation is suggested in the present approach, and non-dimensional parameters are evaluated by comparing the computational results with the laboratory measurements. Various values of a large range are applied to the non-dimensional parameters for the sensitivity test and in order to improve the predictability common values of constants are deduced, which produce similarly good computational results for the well-controlled laboratory measurements.

• The Journal of the Institute of Internet, Broadcasting and Communication
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• v.16 no.4
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• pp.53-58
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• 2016

A ray tracing method to analyze the propagation channel characteristics for a millimeter-wave indoor wireless communication system is presented. Reflected rays from planar as well as rough surfaces are included. Transmitted rays though a thin dielectric slab are considered. Maps representing received power levels and RMS delay spread from a transmitter in a rectangular room are shown. The received power levels in the empty room for bottom's roughness factors of 0 and 0.13 are represented. The simulation results are well consistent with the calculation of Friis equation with reflection coefficient. Any size of furniture the shape of plane form can be positioned anywhere in the room.

• Water for future
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• v.25 no.1
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• pp.111-119
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• 1992

This paper is concerned with the actual comparison analysis for the freshening process in the two selected experimental reservoirs. At the deep freshening reservoir, the salinity and depth of the freshwater layer were estimated by simulation technique using the quantitative equation for the two-layered flow structures. First of all, it is shown that the effects of underdrainage conduit in the lower layer were reported more effective for the control of upper layer salinity comparing with the case of no underdrainage conduit. Further the results of computation were later compared with the real observed values and the relating parameters of the salt-balance equation are conformed even though approximately. Finally it was represented that the salinity of upper layer is easily diluted not only by the tidal gate but also by the underdrainge conduit in the lower layer of the freshening reservoir.

• Proceedings of the Korea Water Resources Association Conference
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• 2016.05a
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• pp.73-73
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• 2016

1차원 Saint-Venant 방정식을 이용한 동력학적 부정류 계산모형은 하도의 지형과 흐름에 대한 물리적 특성을 잘 반영하고 있지만 하폭이 좁고 경사가 큰 하천에서는 해의 안정성 문제를 갖고 있기 때문에 홍수 예 경보를 목적으로 하는 하도추적 방법으로 항상 적합하다 할 수 없다. 본 연구에서는 이러한 동력학적 부정류 계산모형의 대안으로서 확산파 모형의 수치해법으로 볼 수 있는 Muskingmum-Cunge 모형을 남한강에 적용하여 분포형 매개변수를 추정하는 방법을 제시하였다. 먼저 남한강의 상류인 충주 조정지댐부터 여주 수위관측소까지 가용한 각각의 횡단면에 대해 최심하상고에서 제방고까지 다양한 수위를 가정하고 수면폭과, 통수단면적 그리고 동수반경을 계산한 후 Manning 식을 이용하여 유량을 산정한다. 이때 각 단면별로 유량에 대한 통수단면적과 수면폭에 대하여 회귀분석 방법을 이용해 단면별 매개변수를 추정한다. 추정된 매개변수를 Muskingum-Cunge 모형에 적용하여 상류로부터 하류까지 각 단면별로 하도추적을 수행한다. 계산된 결과는 HEC-HMS Musking-Cunge 모형과 첨두유량의 크기 및 무차원 RMS 등을 비교하였을 때 동력학적 모형의 계산결과에 잘 일치함을 알 수 있다.