Implementing a plastic rheology (using the μ(I)-rheology [5]) in a 2D Navier-Stokes solver, we simulate the continuum counterpart of the granular silo. Doing so, we observe a constant flow rate during the discharge and recover the Beverloo scaling. The results suggest that the constant discharge rate is due to the existence of a friction-dependent yield stress. Discrete simulations are performed using the contact dynamics algorithm. Systematic comparison of the velocity field and the inner deformations shows a good agreement between the two approaches. © 2013 AIP Publishing LLC.
CITATION STYLE
Staron, L., Lagreóe, P. Y., & Popinet, S. (2013). Discharge of a granular silo as a visco-plastic flow. In AIP Conference Proceedings (Vol. 1542, pp. 1290–1293). https://doi.org/10.1063/1.4812175
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