• Title/Summary/Keyword: 파랑과 흐름 공존

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파ㆍ흐름 공존장 수치모델의 적용성

  • 이창호;김헌태;류청로;이인철
    • Proceedings of the Korean Society of Fisheries Technology Conference
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    • 2003.05a
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    • pp.166-167
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    • 2003
  • 파랑ㆍ흐름의 공존장에서 그 간섭작용은 Tidal inlet 와 하구부근와 같은 천해영역에서 중요한 물리적 현상이다. 이러한 파ㆍ흐름간섭현상은 파랑의 파고, 스펙트럼과 파향등을 현저하게 변화시키고, 하구와 inlet부근에 출현하는 사주(砂洲)등의 발생기구 및 해빈 안정화에 관계하는 중요한 요인이기 때문에 이에 대한 적절한 해석이 필요하다. 본 보고에서는 확장형 부시네스크방정식을 토대로 한 수치모델을 통하여 파ㆍ흐름 공존장에서의 적용성을 검토하고자 한다. (중략)

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Development of a 3-D Coupled Hydro-Morphodynamic Model between Numerical Wave Tank and Morphodynamic Model under Wave-Current Interaction (파랑-흐름의 상호작용 하에서 지형변동에 관한 3차원 연성 수치모델의 개발)

  • Lee, Woo-Dong;Hur, Dong-Soo
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.34 no.5
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    • pp.1463-1476
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    • 2014
  • In order to understand hydrodynamic and morphodynamic characteristics under wave-current interactions in an estuary, a coupled model for two-way analysis between existing 3-d numerical wave tank and newly-developed 3-d morphodynamic model has been suggested. Comparing to existing experimental results it is revealed that computed results of the newly-suggested model are in good agreement with each laboratory test result for wave height distribution, vertical flow profile and topographical change around ocean floor pipeline in wave-current coexisting field. Also the numerical result for suspended sediment concentration is verified in comparison with experimental result in solitary wave field. Finally, it is shown that the 3-D coupled Hydro-Morphodynamic model suggested in this study is applicable to morphological change under wave-current interaction in an estuary.

A General Formula of Total Sediment Transport Rate for Waves and Currents (범용 파랑.흐름 공존시의 비점착성 퇴적물이동 예측식)

  • Kim, Hyo-Seob;Jang, Chang-Hwan
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.21 no.6
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    • pp.462-469
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    • 2009
  • This study suggests a general formula of non-cohesive sediment transport rates for waves and currents which is also valid for wave only or current only condition. On-offshore sediment transport rates with the second order Stokes wave in the shallow water are calculated as the pickup rate times the distance. The formula depicts reasonably that high waves move material offshore, and low waves move material onshore. Also the formula, as is the case the waves with long period tend to move material onshore, shows good results.

Characteristics of Suspended Sediment Transport in Wave and Current Co-Existing System (파랑과 흐름이 공존하는 영역에서의 평형 및 비평형 부유사이동특성)

  • ;Ichiro Deguchi
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.3 no.4
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    • pp.209-216
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    • 1991
  • Characteristics of suspended sediment concentration of equilibrium and non-equilibrium state caused by waves and currents are investigated by conducting a movable bed experiments in wave tanks. In the region where a downward flux of suspended sediment is larger than a upward flux, time-averaged vertical distribution of suspended sediment does not indicate logarithmic distribution. A new numerical procedure for predicting time-averaged suspended sediment concentration is also proposed based on two-dimensional advective diffusion equation by applying a split-operator approach. It is found that the unposed procedure can predict measured distribution of suspended sediment satisfactorily.

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Nonlinear Interaction among Wave, Current and Submerged Breakwater (파랑-흐름-잠제의 비선형 상호간섭 해석)

  • Park, Su-Ho;Lee, Jung-Hoo
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.36 no.6
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    • pp.1037-1048
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    • 2016
  • In this study, nonlinear wave interaction in the presence of a uniform current is studied using numerical model, named CADMAS-SURF which is based on the Navier-Stokes equations coupled with Volume of Fluid for tracking free surface deformation. The original CADMAS-SURF developed for interaction of wave with structure is modified/extended to simulate nonlinear fluid dynamic motions within wave-current coexisting field. The capability of Numerical Wave-Current Tank (NWCT) in this study is validated by comparing with available existing laboratory experiments for both wave-following and wave-opposing current. The numerical results for interaction between wave and current are shown to be in good agreement with experimental data. Then, this study focused on the dynamic motions of the water velocity, surface elevation and vorticity within combined wave-current field in demonstrating complex nonlinear physical phenomena due to interaction between wave and current. In addition, NWCT is applied to simulate a more complex wave-current-structure field for wave propagating over a submerged breakwater associated with current. Detailed discussion including characteristics of velocity and vorticity fields and the relation between free surface and vorticity are given.

The Local Scour around Submarine Pipelines in the Interaction Region Combined with Waves and Currents (파랑과 정상흐름의 공존역에서 해저관로 주변의 국부세굴)

  • Kim, Kyoung-Ho;Lee, Ho-Jin;Kim, Wan-Shik
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.20 no.5
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    • pp.510-521
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    • 2008
  • In the study, experiments are performed in the interaction region combined with wave and current to investigate the characteristics of local scour around submarine pipelines. Wave generator and current generator are used for the experiments and two current directions were used; co-direction and counter direction to the wave. The local scour depths around the pipeline are obtained according to the various pipe diameters(D), wave periods(T), wave heights(H), and current velocities(V). The experiments show that the maximum equilibrium local scour depth increases with pipe diameter, wave period, wave height, and current velocity. Using the experimental results, the correlations of scour depth and parameters such as Shields parameter($\theta$), Froude number(Fr), period parameter, Keulegan-Carpenter number(KC), Ursell number($U_R$), modified Ursell number($U_{RP}$) and ratio of velocities($U_{c}/(U_{c}+U_{m})$) are analyzed. In the interaction region combined with waves and currents, Froude number and Shields parameter are found the main parameters to cause the local scour around the submarine pipelines and this means that current governs the scour within any limits of the currents.

Wave Modeling considering Water Level Changes and Currents Effects (수위변화와 흐름효과를 고려한 파랑모델링)

  • Eum, Ho-Sik;Kang, Tae-Soon;Nam, Soo-Yong;Jeong, Won-Moo
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.28 no.6
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    • pp.383-396
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    • 2016
  • In this study, wave model was conducted on the presence or absence of water level changes and currents effects in coastal waters coexisting with waves and currents, then the results were compared. The flow field applied the results of the RIAMOM model and the wave model applied the SWAN model. Among ECMWF, NCEP and JMA, wind data applied JMA data sets which agreed well with the observed data comparatively. Numerical simulation was conducted for 8 months from January to August 2016. For each case, the deviation of wave height was calculated for the high wave of more than 2.5 m for comparison with observed data. As a result, the deviation of wave height was not significant both considering water level changes and currents effects or not at wave observation stations installed in deep waters. However, a significant deviation of wave height of 5~10% was obtained depending on water level changes and currents effects at the comparison point in shallow waters.

Numerical Simulation of Solute Transport in Coastal Areas (해안지역에서의 용존성 물질의 이송확산 거동 수치모의)

  • Kim, Dae-Hong
    • Ecology and Resilient Infrastructure
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    • v.1 no.1
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    • pp.1-7
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    • 2014
  • In this study, a numerical simulation technique for coastal area where wave and current interactions are observed is proposed. Considering the spatial scale of coastal area and the coastal processes such as wave, current, shoaling, wave breaking, and inundation processes, boussinesq equation model is used. A depth-integrated transport model based on the consistent assumption with the boussinesq equation model is used for the prediction of solute transport. To solve the equations, finite volume method with an approximate riemann solver is used. The proposed model is applied to a coastal area and reasonable computational results are obtained.

The Local Scour around a Slender Pile in Combined Waves and Current (파랑과 흐름이 결합된 공존역에서 파일 주변의 국부세굴)

  • Park, Jong-Hwan;Kim, Kyoung-Ho
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.22 no.6
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    • pp.405-414
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    • 2010
  • In the study, experiments are performed in the mixing region combined wave and current to investigate the characteristics of local scour around a slender pile. Wave generator and current generator are used for the experiments and currents are co-directions with the waves. The local scour depths around the pipeline are obtained according to the various pipe diameters, wave periods, wave heights, and current velocities. The experiments show that the maximum equilibrium local scour depth increases with pipe diameter, wave period, wave height, and current velocity. Using the experimental results, the correlations of scour depth and parameters such as Shields parameter ($\theta$), Froude number (Fr), Keulegan-Carpenter number (KC), Ursell number ($U_R$), modified Ursell number ($U_{RP}$) and ratio of velocities ($U_c/U_c+U_m$) are analyzed. In the mixing region combined with waves and currents, The Froude number of single parameters is the main parameter to cause the local scour around a slender pile due to waves and current and this means that current governs the scour within any limits of the currents.

Proposal of Empirical Formula for Bedform Size on West Coast of Korea (서해안의 해저표면형상 예측 경험식 제안)

  • Kim, Hyoseob;Yoo, Hojun;Jang, Changhwan
    • Journal of Wetlands Research
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    • v.14 no.4
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    • pp.457-469
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    • 2012
  • Bedform data at 4 shallow zones in the Yellow Sea where waves as well as tidal range are high and bed material is relatively coarse were collected and analyzed here. Water depths in the study area where the bedform data were collected are 10 ~ 65 meters, and ripple lengths well developed are between 6 ~ 13 meters. Existing empirical formula for prediction of ripple length as for coexistence of waves and currents include Khelifa and Ouellet(2000) and Soulsby(2005), both of which have been based on laboratory measurements, or field measurements at different physical environment from the Yellow Sea with respect to tidal range, wave strength, and bed material. New scaling factors are proposed here for better prediction of the ripple length on coastal zone in the Yellow Sea.