Generalization of Chapman-Enskog yields integral viscous stress tensor for large velocity gradients that reduces to standard Navier-Stokes form for small gradients and may enable modeling of turbulence non-locality.
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Generalization of the viscous stress tensor to the case of non-small gradients of hydrodynamic velocity: a path to numerical modeling of turbulence non-locality
Generalization of Chapman-Enskog yields integral viscous stress tensor for large velocity gradients that reduces to standard Navier-Stokes form for small gradients and may enable modeling of turbulence non-locality.