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The present work extends the results of Cantero et al.[1] and Shringarpure et al.[2] to the cases of sediment-laden saline currents. The flow is modeled as a channel flow where the forcing is exerted by salinity and suspended sediments. The resulting set of equations are solved by direct numerical simulation (DNS) for shear Reynolds number Reτ = 180. The DNS results show that by increasing the forcing...
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