2004
DOI: 10.1103/physreve.69.061303
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Inherent rheology of a granular fluid in uniform shear flow

Abstract: In contrast to normal fluids, a granular fluid under shear supports a steady state with uniform temperature and density since the collisional cooling can compensate locally for viscous heating. It is shown that the hydrodynamic description of this steady state is inherently non-Newtonian. As a consequence, the Newtonian shear viscosity cannot be determined from experiments or simulation of uniform shear flow. For a given degree of inelasticity, the complete nonlinear dependence of the shear viscosity on the sh… Show more

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Cited by 109 publications
(207 citation statements)
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“…Specifically, this is even more necessary if γ ≥ 0 (and this happens when the viscous heating dominates over collisional cooling [32]), since in this case the Knudsen number is always greater than the one for γ < 0 [42]. Such a description of the Couette flow beyond the NS domain was carried out in Ref.…”
Section: Introductionmentioning
confidence: 99%
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“…Specifically, this is even more necessary if γ ≥ 0 (and this happens when the viscous heating dominates over collisional cooling [32]), since in this case the Knudsen number is always greater than the one for γ < 0 [42]. Such a description of the Couette flow beyond the NS domain was carried out in Ref.…”
Section: Introductionmentioning
confidence: 99%
“…The accuracy of this latter approach has been confirmed by computer simulations in the cases of the diffusion [28,29] and shear viscosity [30,31] coefficients. On the other hand, the practical applicability of the NS equations is limited to small spatial gradients, while many steady granular flows do not fulfill in general this condition, due to the coupling between inelasticity and gradients [1,32].…”
Section: Introductionmentioning
confidence: 99%
“…This occurs in many important applications for granular fluids [40]. In the limiting case where the low-degree gradients can be controlled by boundary or initial conditions and made small, a further Taylor series expansion can be given…”
Section: Concept Of a Normal Solution And Hydrodynamicsmentioning
confidence: 99%
“…For ordinary (elastic) gases this can be controlled by the initial or boundary conditions. However, in the case of granular fluids the situation is more complicated since in some cases (e.g., steady states such as the simple shear flow problem [40]) the boundary conditions imply a relationship between dissipation and gradients so that both cannot be chosen independently. In these cases, the Navier-Stokes approximation only holds for nearly elastic particles [40].…”
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confidence: 99%
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