Journal of Hydraulic Engineering · 2000 · 416 citations · 15 references
Natural ResourcesCivil EngineeringComputational Fluid DynamicsFluid DynamicsSediment TransportBed Load TransportFluvial Sediment TransportRiver HydraulicsSediment FluxSediment Transport ModelingSuspended Load TransportNumerical Modeling Of Sediment TransportNumerical Sediment Transport SimulationOpen Channel Flow ModelingSediment Settling VelocitySediment Transport EquationsSettling VelocitySuspended Sediment TransportTurbulence In Open Channels
A 3D numerical model for calculating flow and sediment transport in open channels is presented. The model solves the full Reynolds‑averaged Navier–Stokes equations with a k‑ε turbulence closure, uses a 2D Poisson equation for free‑surface elevation, simulates suspended load by a convection‑diffusion equation with empirical settling velocity, and models bed load with a nonequilibrium approach, all discretized by a finite‑volume method on an adaptive, non‑staggered grid. The suspended‑load model was tested for net entrainment and deposition, and the full 3D total‑load model was validated in a 180° channel bend with movable bed, showing generally good agreement with measurements.
A 3D numerical model for calculating flow and sediment transport in open channels is presented. The flow is calculated by solving the full Reynolds-averaged Navier-Stokes equations with the k − ε turbulence model. Special free-surface and roughness treatments are introduced for open-channel flow; in particular the water level is determined from a 2D Poisson equation derived from 2D depth-averaged momentum equations. Suspended-load transport is simulated through the general convection-diffusion equation with an empirical settling-velocity term. This equation and the flow equations are solved numerically with a finite-volume method on an adaptive, nonstaggered grid. Bed-load transport is simulated with a nonequilibrium method and the bed deformation is obtained from an overall mass-balance equation. The suspended-load model is tested for channel flow situations with net entrainment from a loose bed and with net deposition, and the full 3D total-load model is validated by calculating the flow and sediment transport in a 180° channel bend with movable bed. In all cases, the agreement with measurements is generally good.
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Bed deformation in curved alluvial channels
N. Struiksma, Kim Olesen, C. Flokstra et al. · Journal of Hydraulic Research · 1985 · 416 citations