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- W2323183504 abstract "Numerical analysis was carried out to obtain the near-bottom flow velocity and the suspended sediment concentration in the wave and current co-existing system. The near-bottom flow velocity was computed by the turbulent boundary layer theory. The shear stress was evaluated by using the time-independent eddy viscosity proposed by Grant-Madsen.Suspended sediment concentration was computed by the turbulent diffusion theory. The diffusion coefficient was evaluated by using the horizontal and vertical components of flow velocity. The results for near-bottom flow velocity were compared with the laboratory data obtained by Asano et al. For opposing current, as the depth-averaged current velocity exceeds to 1/10-1/5 of the maximum bottom velocity in wave field, the direction of sediment transport is reversed." @default.
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- W2323183504 date "1990-05-20" @default.
- W2323183504 modified "2023-09-23" @default.
- W2323183504 title "SUSPENDED SEDIMENT CONCENTRATION AND SEDIMENT TRANSPORT RATE IN WAVE AND CURRENT CO-EXISTING SYSTEM" @default.
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- W2323183504 doi "https://doi.org/10.2208/jscej.1990.417_165" @default.
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