On the role of the Knudsen layer in rapid granular flows
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Publication:5308061
DOI10.1017/S0022112007006489zbMath1119.76069arXivcond-mat/0703349OpenAlexW2146042839MaRDI QIDQ5308061
Christine M. Hrenya, Janine E. Galvin, R. D. Wildman
Publication date: 26 September 2007
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://arxiv.org/abs/cond-mat/0703349
Related Items (9)
Convection in three-dimensional vibrofluidized granular beds ⋮ Steady base states for Navier–Stokes granular hydrodynamics with boundary heating and shear ⋮ Multivariate Gaussian Extended Quadrature Method of Moments for Turbulent Disperse Multiphase Flow ⋮ Experimental investigation and kinetic-theory-based model of a rapid granular shear flow ⋮ Evidence of higher-order effects in thermally driven rapid granular flows ⋮ Conditional quadrature method of moments for kinetic equations ⋮ Steady base states for non-Newtonian granular hydrodynamics ⋮ Higher-order quadrature-based moment methods for kinetic equations ⋮ Non-equilibrium dynamics of dense gas under tight confinement
Cites Work
- Comparison of kinetic theory predictions with experimental results for a vibrated three-dimensional granular bed
- Comparison of Burnett and DSMC predictions of pressure distributions and normal stress in one-dimensional, strongly nonisothermal gases
- Dilute granular flow around an immersed cylinder
- Size segregation in rapid, granular flows with continuous size distributions
- Binary mixtures of inelastic spheres: Simplified constitutive theory
- Hydrodynamic equations for rapid flows of smooth inelastic spheres, to Burnett order
- Velocity distribution function for a dilute granular material in shear flow
- R<scp>APID</scp> G<scp>RANULAR</scp> F<scp>LOWS</scp>
- On the role of non-equipartition in the dynamics of rapidly flowing granular mixtures
- Hydrodynamic model for a vibrofluidized granular bed
- A BVP solver based on residual control and the Maltab PSE
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