Computation of dust lifting behind a shock wave sliding along the layer. Verification of the model

The problem of dust lifting behind a shock wave is solved within the framework of the equilibrium model of mechanics of heterogeneous media. Verification of the model proposed is performed. It is shown that different flow patterns are formed in layers with different shapes of the edge and constant- or variable-amplitude shock waves. Allowance for turbulence of the mixture leads to origination of a high-velocity near-wall trickle at the edge of the layer, and the particles are lifted to a greater height.