Presenters-0166: Difference between revisions
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|CSDMS meeting abstract presentation=Turbulence, bedload, and suspended sediment transport are directly simulated by a coupled large eddy simulation of the fluid and a distinct element method for every sediment grain. This modeling system directly calculates the motion of all grains by resolved turbulence structures. The model directly calculates modification of the flow and turbulence by the grains, such as the effects of grain momentum extraction and density stratification. Simulations such as these can be used in the future to parameterize sediment transport in large-scale morphodynamic simulations. | |CSDMS meeting abstract presentation=Turbulence, bedload, and suspended sediment transport are directly simulated by a coupled large eddy simulation of the fluid and a distinct element method for every sediment grain. This modeling system directly calculates the motion of all grains by resolved turbulence structures. The model directly calculates modification of the flow and turbulence by the grains, such as the effects of grain momentum extraction and density stratification. Simulations such as these can be used in the future to parameterize sediment transport in large-scale morphodynamic simulations. | ||
|CSDMS meeting youtube code=Z2DJlKncut4 | |CSDMS meeting youtube code=Z2DJlKncut4 | ||
|CSDMS meeting youtube views={{Youtube_Z2DJlKncut4}} | |||
|CSDMS meeting participants=0 | |CSDMS meeting participants=0 | ||
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Revision as of 16:09, 28 May 2025
CSDMS 2.0: Moving Forward
Turbulence- and Particle-Resolving Numerical Modeling of Sediment Transport.
Abstract
Turbulence, bedload, and suspended sediment transport are directly simulated by a coupled large eddy simulation of the fluid and a distinct element method for every sediment grain. This modeling system directly calculates the motion of all grains by resolved turbulence structures. The model directly calculates modification of the flow and turbulence by the grains, such as the effects of grain momentum extraction and density stratification. Simulations such as these can be used in the future to parameterize sediment transport in large-scale morphodynamic simulations.
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