Turbulent and viscous sediment transport – a numerical study
Sediment transport is studied as a function of the grain to fluid density ratio using two phase numerical simulations based on a discrete element method (DEM) for particles coupled to a continuum Reynolds averaged description of hydrodynamics. At a density ratio close to unity (typically under water...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2014-05-01
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| Series: | Advances in Geosciences |
| Online Access: | http://www.adv-geosci.net/37/73/2014/adgeo-37-73-2014.pdf |