Apparent non-locality in dense suspension flows is an artifact of conventional stress averaging; dissipative stress and geometric mixing restore local μ(J) rheology.
Berzi, On granular flows: From kinetic theory to in- ertial rheology and nonlocal constitutive models, Phys
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Non-Local Particle Flows Become Local When Considering Dissipative Stress
Apparent non-locality in dense suspension flows is an artifact of conventional stress averaging; dissipative stress and geometric mixing restore local μ(J) rheology.