Comparison of turbulence schemes for prediction of wave-induced near-bed sediment suspension above a plane bed

被引:0
作者
Chi Zhang
Jin-hai Zheng
Yi-gang Wang
Meng-tao Zhang
Dong-sheng Jeng
Ji-sheng Zhang
机构
[1] Hohai University,State Key Laboratory of Hydrology
[2] Hohai University,Water Resources and Hydraulic Engineering
[3] Shanghai Jiao Tong University,College of Harbor, Coastal and Offshore Engineering
[4] University of Dundee,Center for Marine Geotechnical Engineering Research
来源
China Ocean Engineering | 2011年 / 25卷
关键词
sediment transport; wave boundary layer; turbulence scheme;
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中图分类号
学科分类号
摘要
Based on a wave bottom boundary layer model and a sediment advection-diffusion model, seven turbulence schemes are compared regarding their performances in prediction of near-bed sediment suspension beneath waves above a plane bed. These turbulence algorithms include six empirical eddy viscosity schemes and one standard two-equation k-ɛ model. In particular, different combinations of typical empirical formulas for the eddy viscosity profile and for the wave friction factor are examined. Numerical results are compared with four laboratory data sets, consisting of one wave boundary layer hydrodynamics experiment and three sediment suspension experiments under linear waves and the Stokes second-order waves. It is shown that predictions of near-bed sediment suspension are very sensitive to the choices of the empirical formulas in turbulence schemes. Simple empirical turbulence schemes are possible to perform equally well as the two-equation k-ɛ model. Among the empirical schemes, the turbulence scheme, combining the exponential formula for eddy viscosity and Swart formula for wave friction factor, is the most accurate. It maintains the simplicity and yields identically good predictions as the k-ɛ model does in terms of the wave-averaged sediment concentration.
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页码:395 / 412
页数:17
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共 70 条
  • [1] Absi R.(2010)Concentration profiles for fine and coarse sediments suspended by waves over ripples: An analytical study with the 1-DV gradient diffusion model Adv. Water Resour. 33 411-418
  • [2] Amoudry L.(2005)Schmidt number and near-bed boundary condition effects on a two-phase dilute sediment transport model J. Geophys. Res. 110 C09003-2001
  • [3] Hsu T. J.(2008)Two-phase model for sand transport in sheet flow regime J. Geophys. Res. 113 C03001-25
  • [4] Liu P. L. F.(2004)Modelling sheet-flow sediment transport in wave-bottom boundary layers using discrete-element modeling Philosophical Transactions of the Royal Society of London, Ser. A 362 1987-36
  • [5] Amoudry L.(2005)Modelling and measurement of sediment transport by waves in the vortex ripple regime J. Geophys. Res. 110 1-198
  • [6] Hsu T. J.(2008)Advances in the study of moving sediments and evolving seabeds Surv. Geophys. 29 1-306
  • [7] Liu P. L. F.(1997)Comparisons between sediment transport models and observations made in wave and current flows above plane beds Coast. Eng. 31 163-1997
  • [8] Calantoni J.(1976)A sediment transport model for straight alluvial channels Nordic Hydrology 7 293-371
  • [9] Holland K. T.(1979)Combined wave and current interaction with a rough bottom J. Geophys. Res. 84 1808-2091
  • [10] Drake T. G.(2004)Observed and predicted bed forms and their effect on suspended sand concentrations Coast. Eng. 51 351-43