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This study described a preliminary experimental setup to identify how near-bed turbulence interacts with and moves sediment. The turbulence generated by a vertically oscillating grid was made to interact with a homogeneous horizontal sediment layer. Near-spherical particles were used throughout with two types of sediment at comparable sediment size dd ≈ 700 μm. The interaction characteristics were investigated by employing the PIV technique to measure the velocity field of the displaced sediment grains (within the transverse plane of the bed surface) during the interaction. Measurement of the velocity of the displaced sediment grains was restricted to the

The Interaction of Oscillating-Grid Turbulence with a Sediment Layer