• 한국해안해양공학회지
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• 제9권3호
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• pp.125-131
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• 1997

해빈 보존공법중 배수층설지 공법의 타당성 분석을 위하여 파랑모형과 침투류모형을 결합한 복합모형을 구성하여 수치실험을 수행하였다 파랑모형으로는 Shuto(1972)의 해석해를 사용하였고, 침투류모형으로는 포화-비포화흐름의 지배방정식인 Richards식을 사용하였다. 구성된 복합모형의 민감도 분석에 의하면 포화투수계수가 해빈내부의 지하수 흐름장에 가장 민감한 영향을 미치고 있음을 알 수 있었다. 또한 보다 많은 현지의 실측자료들이 수집 된다면 개발된 모형은 해빈내에 배수층 설치시 필요로 되는 제요소 해석에 효율적으로 이용될 수 있을 것이다

• 한국해안·해양공학회논문집
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• 제20권4호
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• pp.363-371
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• 2008

본 연구에서는 투과성잠제 주변의 파동장 해석을 위한 2-D 수치해석기법과 3-D 수치해석기법에 의한 결과를 비교하기 위하여 투과성구조물에 의한 유체저항(관성저항, 층류저항 및 난류저항)을 고려할 수 있는 수치해석기법을 이용하고, 난류모델로서 LES 모델을 도입하여 기존에 수행되었던 수리모형실험과의 비교를 통하여 검증하였다. 수치해석결과로부터 투과성잠제의 배후에서 2-D해석에 의한 결과가 3-D해석의 경우보다 높은 파고분포를 나타내었으며, 잠제 주변의 평균류에 대해서도 비교, 논의하였다.

• 한국가시화정보학회지
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• 제11권2호
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• pp.46-54
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• 2013

Study of the wave structure and shear layer in the vicinity of a wall mounted cavity is done by time averaged colour schlieren and time resolved instantaneous shadowgraph technique in an M=1.7 flowfield. Effect of change of cavity width on flow structure is investigated by using constant length to depth (L/D) ratio cavity models with varying length to width (L/W) ratio of 0.83 to 4. The time averaged shock wave structure was observed to change with change in cavity width. Dependence of the shock angle at the leading edge on the shear layer width is also evident from the images obtained. Unsteadiness in the flow field in terms of shear layer dynamics and quasi steady nature of shock waves was evident from the images obtained during instantaneous shadowgraph experiments. Apart from the leading and trailing edge shocks, several other waves and flow features were observed. These flow features and the associated physical phenomena are discussed in details and presented in the paper.

• 한국해양공학회지
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• 제23권1호
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• pp.43-47
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• 2009

This paper compares theoretical wave profile and particle kinematics with experimental results generated by a 2 D wave tank. Particle velocity fields of compound waves were acquired using a PIV technique. Synchronization was applied to acquire images of the wave fields, and the time gap between these images was controlled by the user. This technique was applied to investigate the wave breaking mechanism, and the wave profile and velocity distribution in a wave breaking field was obtained.

• Advances in aircraft and spacecraft science
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• 제4권4호
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• pp.487-501
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• 2017

The main purpose of the paper is to analyze effect of geometrical parameters of the reentry capsules such as radius of the spherical cap, shoulder radius, back shell inclination angle and overall length on the flow field characteristics. The numerical simulation with viscous flow past ARD (Atmospheric Reentry Demonstrator), Soyuz (Russian) and OREX (Orbital Reentry EXperimental) reentry capsules for freestream Mach numbers range of 2.0-5.0 is carried out by solving time-dependent, axisymmetric, compressible laminar Navier-Stokes equations. These reentry capsules appear as bell, head light and saucer in shape. The flow field features around the reentry capsules such as bow shock wave, sonic line, expansion fan and recirculating flow region are well captured by the present numerical simulations. A low pressure is observed immediately downstream of the base region of the capsule which can be attributed to fill-up in the growing space between the shock wave and the reentry module. The back shell angle and the radius of the shoulder over the capsule are having a significant effect on the wall pressure distribution. The effects of geometrical parameters of the reentry capsules will useful input for the calculation of ballistic coefficient of the reentry module.

• 한국해양공학회지
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• 제31권2호
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• pp.121-129
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• 2017

The present study numerically investigated the influence of the waveform distribution on the tsunami-vegetation interaction using a non-reflected wave generation system for various tsunami waveforms in a two-dimensional numerical wave tank. First, it was possible to determine the wave attenuation mechanism due to the tsunami-vegetation interaction from the spatial waveform, flow field, vorticity field, and wave height distribution. The combination of fluid resistance in the vegetation and a large gap and creates a vortex according to the flow velocity difference in and out of the vegetation zone. Thus, the energy of a tsunami was increasingly reduced, resulting in a gradual reduction in wave height. Compared to existing approximation theories, the double volumetric ratio of the waveform increased the reflection coefficient of the tsunami-vegetation interaction by 34%, while decreasing the transfer coefficient and energy attenuation coefficient by 25% and 13%, respectively. Therefore, the hydraulic characteristics of a tsunami is highly likely to be underestimated if the solitary wave of the approximation theory is applied for the tsunami.

• 한국습지학회지
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• 제23권2호
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• pp.107-115
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• 2021

서해 개야수로 인근의 파랑전파, 해수유동, 퇴적물이동을 분석하기 위해서 각종 인공구조물 설치 전(CASE1W)과 후(CASE2W)로 분류하고, CASE1W와 CASE2W에 대한 계산결과를 비교하였다. 파랑전파에 대해서는 SWAN 수치모형을 이용하여 입사파와 반사파의 결과를 도출하였고, 해수유동에 대해서는 FLOW2DH 수치모형을 이용하여 해수유동에 따른 유속 결과를 도출하였다. SWAN 수치모형과 FLOW2DH 수치모형의 결과는 퇴적물이동을 예측하는 SEDTRAN 수치모형의 입력조건이 되어 개야수로 인근의 최대 저면전단응력과 부유사 농도분포를 계산하였다. SWAN 수치모형 계산결과, CASE2W의 경우 약 7 km 길이의 북측 도류제에 의해서 입사파가 회절 및 중첩되고, 반사파가 생성되어 개야수로 인근의 파고를 CASE1W에 비해 40~50 % 증가시켰다. FLOW2DH 수치모형 계산결과, 북방파제, 북측 도류제 및 금란도에 의해서 개야수로의 유속이 CASE1W과 대비하여 CASE2W가 10~30 % 빠르게 계산되었다. SEDTRAN 수침모형의 계산결과, 복합 파랑장(입사파, 반사파, 조석)에 따른 해양환경과 각종 인공구조물의 설치에 의해서 개야수로의 최대 저면전단응력이 1.0 N/m² 이상인 구간과 부유사농도가 80 mg/L 이상인 구간이 넓게 분포되었다는 것은 개야수로에 퇴적현상이 발생한 것이라고 판단된다.

• 한국해양공학회지
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• 제34권2호
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• pp.128-135
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• 2020

When high waves and storm surge strike simultaneously, the characteristics of the fluid field change drastically from overtopping according to the wave runup height to overflow through a transition state that combines overtopping and overflows. However, an estimation model or evaluation method has not yet been established because there is not enough engineering data. This study developed a wave overtopping-overflow transition model based on a full-scale experiment involving wave overtopping and overflow transition, which appropriately reproduced the effect of waves or the temporal change in inundation flow. Using this model to perform a calculation for the wave overtopping and overflow transition process under typical circumstances, this study determined the wave runup height and features of the inundation flow under time series changes as an example.

• 한국항해항만학회:학술대회논문집
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• 한국항해항만학회 2000년도 춘계학술대회논문집
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• pp.75-81
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• 2000

Water waves propagate over irregular bottom bathymetry are transformed by refraction, diffraction, shoaling, reflection etc. Principal factor of wave transform is bottom bathymetry, but in case of current field, current is another important factor which effect wave transformation. The governing equation of this study is develop as wave-current equation type to investigate the effect of wave-current interaction. This wave-current model was applied to the Kwangan beach which is located at Pusan. The numerical simulation results of this model show the characteristics of wave transformation and flow pattern around the Kwangan beach fairly well.

• 한국해양공학회지
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• 제15권2호
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• pp.6-10
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• 2001

Water waves propagate over irregular bottom bathymetry are transformed by refraction, diffraction, shoaling, reflection etc. Principal factor of wave transform is bottom bathymetry, but in case of current field, current is another important factor which effect wave transformation. The governing equation of this study is develope as wave-current equation type to investigate the effect of wave-current interaction. It starts from Berkhoff's(1972) mild slope equation and is transformed to time-dependent hyperbolic type equation by using variational principal. Finally the governing equation is shown as a parabolic type equation by splitting method. This wave-current model was applied to the kwangan beach which is located at Pusan. The numerical simulation results of this model show the characteristics of wave transformation and flow pattern around the Kwangan beach fairly well.