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). sediment transport occurs in a thin layer at the surface of the static bed. and is c... https://foldlyers.shop/product-category/cable-clamps-clips/