International audienceAfter a quick overview of recent research on sediment transport by shear flow and ripple and dune formation, original numerical results are presented from two-phase flow modelling of the interaction between a viscous flow and a bed of particles. Good agreement is found with previous experiments or numerical simulation, notably for the particle flux and velocity profiles within the moving layer. Bed instability is also found, giving rise to ripples whose characteristics are discussed
A numerical model for the general description of the sediment transport under oscillatory sheet flow...
A theory of turbulent shear flow over a sand bed is developed addressing the instability principle o...
This study investigated the initiation of bedforms from a flat sand bed and the transition between t...
A linear stability analysis for dune and ripple formation is presented that implements a rotational ...
International audienceWe propose a two-phase model having a Newtonian rheology for the fluid phase a...
Sediment transport is studied as a function of the grain to fluid density ratio using two phase nume...
When beds constituted of sediment particles are submitted to shearing ows, the particles at the surf...
In most natural watercourses the bed consists of alluvial material. If, in this case, the impact of ...
Sediment bedload transport and bedform formation are considered for both steady and oscillatory flow...
International audienceWe propose a two-phase model having a Newtonian rheology for the fluid phase a...
Sediment transport is induced by the interaction between turbulence and the solid particles that com...
Most models of sediment transport are based on the hypothesis of a weak interaction between the flui...
We investigate the process of ripple formation in a viscous fluid when a sand bed is submitted to a ...
Alluvial open channel beds often exhibit statistically periodic irregularities, known as dunes. Dune...
We investigate the process of ripple formation when a sand bed is submitted to a steady and turbulen...
A numerical model for the general description of the sediment transport under oscillatory sheet flow...
A theory of turbulent shear flow over a sand bed is developed addressing the instability principle o...
This study investigated the initiation of bedforms from a flat sand bed and the transition between t...
A linear stability analysis for dune and ripple formation is presented that implements a rotational ...
International audienceWe propose a two-phase model having a Newtonian rheology for the fluid phase a...
Sediment transport is studied as a function of the grain to fluid density ratio using two phase nume...
When beds constituted of sediment particles are submitted to shearing ows, the particles at the surf...
In most natural watercourses the bed consists of alluvial material. If, in this case, the impact of ...
Sediment bedload transport and bedform formation are considered for both steady and oscillatory flow...
International audienceWe propose a two-phase model having a Newtonian rheology for the fluid phase a...
Sediment transport is induced by the interaction between turbulence and the solid particles that com...
Most models of sediment transport are based on the hypothesis of a weak interaction between the flui...
We investigate the process of ripple formation in a viscous fluid when a sand bed is submitted to a ...
Alluvial open channel beds often exhibit statistically periodic irregularities, known as dunes. Dune...
We investigate the process of ripple formation when a sand bed is submitted to a steady and turbulen...
A numerical model for the general description of the sediment transport under oscillatory sheet flow...
A theory of turbulent shear flow over a sand bed is developed addressing the instability principle o...
This study investigated the initiation of bedforms from a flat sand bed and the transition between t...