Origin of geometric cohesion in non-convex granular materials: interplay between interdigitation and rotational constraints enhancing frictional stability
Jonathan Barés, Arnaud Regazzi, David Aponte, Sylvain Buonomo, Mathieu Renouf, Nicolas Estrada, Emilien Azéma
TL;DR
This work addresses how non-convex, non-interlocking grains achieve mechanical stability through geometry. It uses 3D X-ray tomography of cylindrical piles of polypod particles across varied friction, concavity, and branch counts, and introduces a stability indicator $\mathcal{S}$ that blends interdigitation, rotational constraint, and friction to quantify geometrical cohesion. The results show that stability is not simply tied to crystalline order or packing fraction; instead, central locking of multiple contacts and reconformability govern robustness, with $\mathcal{S}$ tracking the observed collapse ratio $\mathcal{R}$. These findings provide concrete design rules—such as extending branch length—to maximize geometric cohesion and offer a locally computable metric for strength that could extend to a broad class of concave granular particles.
Abstract
We present a series of experiments investigating the local microstructure of cylindrical piles composed of highly concave particles. By systematically varying particle geometry -- from spheres to strongly non-convex polypods -- as well as frictional properties and the number of branches, we explore how these parameters, together with the preparation protocol, shape the internal structure of the system. Using X-ray tomography combined with a dedicated image-analysis pipeline, we accurately extract the position, orientation, and contacts of every particle in each pile. This allows us to quantify the evolution of key structural observables as a function of particle geometry and preparation method. In particular, we measure the distributions of local packing fraction, coordination number, number of neighbors, and contact locations, along with particle-particle positional and orientational correlations. More importantly, we construct a new stability indicator that correlates perfectly with the observed pile stabilities, enabling us to identify the fundamental mechanisms responsible for \textit{geometrically induced cohesion} in granular systems composed of non-interlocking particle shapes: interdigitation, rotational constraint, friction-mediated cohesion, and the ability of a pile to re-stabilize.
