Shear-induced horizontal buoyancy from depth-averaged non-Boussinesq channel flow equals the divergence of a Korteweg stress tensor whose coefficients depend on Prandtl and Grashof numbers, with a transition at Pr = 1/2.
Brenner, Conduction-only transport phenomena in compressible bivelocity fluids: Diffuse interfaces and ko- rteweg stresses, Phys
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A hydrodynamic origin of Korteweg stresses from shear-induced horizontal buoyancy
Shear-induced horizontal buoyancy from depth-averaged non-Boussinesq channel flow equals the divergence of a Korteweg stress tensor whose coefficients depend on Prandtl and Grashof numbers, with a transition at Pr = 1/2.