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1 Introduction Coastal seabeds constituted of non-cohesive sediments are covered by a large diversity of bedforms with sizes ranging from several centimeters in length up to several tenths of meters. Such bedforms interact with the flow in many different ways and their quantitative prediction on the basis of physical process-based models remain a scientifically challenging task (Nielsen, 1988).
Abstract One of the most enigmatic science questions concerning inertial particle transport by a turbulent boundary layer flow is the value of the turbulent Schmidt number defined as the ratio of turbulent eddy viscosity to particle concentration diffusivity.
Sandy river beds are dominated by rhythmic features known as dunes. Experimental investigations of turbulent flow and sediment transport over dunes have predominantly focused on equilibrium flows that are rare in natural rivers.
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