Forced silo discharge: Simulation and theory
Luis. A. Pugnaloni, Marcos A. Madrid, J. R. Darias
TL;DR
This study uses discrete element method simulations to analyze forced silo discharge through a circular orifice under overweight loading. It identifies two regimes: an initial flow rate $Q_{ m ini}$ that follows Beverloo-like free-discharge scaling and a final flow rate $Q_{ m end}$ that scales with $\sqrt{\rho_b P}$ and exhibits unusual $D_o$ and $D_s$ dependencies, consistent with viscous-like behavior under strong forcing. A work–energy framework is developed to derive a differential equation for the time evolution of the mass flow rate, incorporating gravity, overweight input, outflow, dissipation via $\mu(I)$-rheology, and pressure from Walters’ model; this approach accurately captures the initial Beverloo scaling and the qualitative pressure- and density-dependence of the final flow but struggles to reproduce the precise end-flow geometry and the $D_o$ and $D_s$ scalings, highlighting the need for nonlocal rheology or refined end-flow modeling in strongly forced granular flows. Overall, the work highlights new challenges in understanding forced granular discharges, where dissipation and confinement strongly alter flow behavior beyond classical Beverloo gas- or liquid-like pictures.
Abstract
We study, through discrete element simulations, the discharge of granular materials through a circular orifice on the base of a cylindrical silo forced by a surcharge. At the beginning of the discharge, for a high granular column, the flow rate $Q_{\rm ini}$ scales as in the Beverloo equation for free discharge. However, we find that the flow rate $Q_{\rm end}$ attained at the end of the forced discharge scales as $\sqrt{ρ_b P}D_o^3/D_s$, with $ρ_b$ the bulk density, $P$ the pressure applied by the overweight, $D_o$ the orifice diameter and $D_s$ the silo diameter. We use the work$-$energy theorem to formulate an equation for the flow rate $Q_{\rm end}$ that predicts the scalings only in part. We discuss the new challenges offered by the phenomenology of strongly forced granular flows.
