Clogging-flowing transition of granular media in a two-dimensional vertical pipe
Y. Zhou, M. Li, Y. Guan, Y. Wang, Y. Liu, Z. Zou
TL;DR
This study reveals a nonmonotonic clogging probability $J$ for granular flow in a 2D vertical pipe, extending prior 3D findings to a planar geometry. By combining experiments with DEM simulations, it shows that both the geometric constraint $D/d$ and the interparticle friction coefficient $μ$ jointly govern the transition between clogging and flowing, enabling a $D/d$-$μ$ phase diagram with a friction-influenced flowing regime. The mechanism is anchored in arch formation: three-particle arches mediate clogging, and a simple force-torque balance criterion explains the observed nonmonotonicities, including a sharp drop near $D/d o 2.73$ due to contact-direction changes and a secondary drop near $D/d o 2.9$ due to arch geometry. The results advance predictive understanding of clogging in narrow vertical channels and highlight the critical role of non-equilibrium force states and arch geometry in 2D granular flows, with planned extensions to 3D and polydisperse systems.
Abstract
We experimentally and numerically investigate the clogging behavior of granular materials in a two-dimensional vertical pipe. The nonmonotonicity of clogging probability found in a cylindrical vertical pipe [López et al., Phys. Rev. E 102, 010902 (2020)] is also observed in the two-dimensional case. We numerically demonstrate that the clogging probability strongly correlates with the friction coefficient $μ$ in addition to the pipe-to-particle diameter ratio $D/d$. We thus construct a clogging-flowing $D/d$-$μ$ phase diagram within the $2<D/d<3$ range. Finally, by analyzing the geometrical arrangements of particles and using a simple analysis of forces and torques, we are able to predict the clogging-flowing transition in the $D/d$-$μ$ phase diagram and explain the mechanism of the observed counterintuitive nonmonotonicity in more detail. We demonstrate that for pipe clogging, friction-mediated force and torque equilibrium are essential for arch formation.
