Convective Flows in Sheared Packings of Spherical Particles

TL;DR

This study reveals persistent convective flows within sheared spherical particle packings, driven by system geometry, challenging previous assumptions that such flows require particle shape anisotropy or boundary effects.

Contribution

It provides direct observations of internal convection rolls in spherical granular packings, highlighting the influence of system geometry on flow patterns in dense granular materials.

Findings

Convection rolls depend on system height and geometry.

At low heights, two counter-rotating convection rolls form.

At higher heights, a single outward-flowing convection roll dominates.

Abstract

Understanding how granular materials respond to shear stress remains a central challenge in soft matter physics. We report direct observations of persistent granular convection in the bulk shear zones of spherical particle packings -- a phenomenon previously associated primarily with particle shape anisotropy or boundary effects. By employing various bead-coloring techniques in a split-bottom geometry, we reveal internal flow fields within sheared granular packings. We find robust convection rolls, strikingly governed by system geometry: at low filling heights, two counter-rotating convection rolls emerge, while at higher filling heights, a single dominant convection roll forms, featuring radially outward flow at the surface. This transition is driven by the height-dependent broadening of the shear zone, which introduces shear rate asymmetry across its flanks. Notably, the transition occurs entirely within the open shear band regime. These findings underscore the pivotal role of system geometry in shaping secondary flow formation in dense packings of frictional particles, suggesting possible broader relevance to geophysical flow dynamics and industrial applications.