Forced flow of granular media: Breakdown of the Beverloo scaling

Abstract

The Beverloo scaling for the gravity flow of granular materials through orifices has two distinct universal features. On the one hand, the flow rate is independent of the height of the granular column. On the other hand, less well-known yet more striking, the flow rate is fairly insensitive to the material properties of the grains (density, Young's modulus, friction coefficient, etc.). We show that both universal features are lost if work is done on the system at a high rate. In contrast to viscous fluids, the flow rate increases during discharge if a constant pressure is applied to the free surface of a granular column. Moreover, the flow rate becomes sensitive to the material properties. Nevertheless, a new universal feature emerges: the dissipated power scaled by the mean pressure and the flow rate follows a master curve for forced and unforced conditions and for all material properties studied. We show that this feature can be explained if the granular flow in the silo is assumed to be a quasistatic shear flow under the $\mu (I)$-rheology.

6 pages, 4 figures

References in corpus (3)

• The granular silo as a continuum plastic flow: the hour-glass vs the clepsydra
• The sands of time run faster near the end
• A differential equation for the flow rate during silo discharge: Beyond the Beverloo rule

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• Average outpouring velocity and flow rate of grains discharged from a tilted quasi-2D silo