Physics of Compaction of Fine Cohesive Particles

A. Castellanos, J. M. Valverde, and M. A. S. Quintanilla
Phys. Rev. Lett. 94, 075501 – Published 22 February 2005

Abstract

Fluidized fractal clusters of fine particles display critical-like dynamics at the jamming transition, characterized by a power law relating consolidation stress with volume fraction increment [σ^c(Δϕ)β]. At a critical stress clusters are disrupted and there is a crossover to a logarithmic law (Δϕ=νlogσ^c) resembling the phenomenology of soils. We measure λΔ(1/ϕ)/logσ^cBog0.2, where Bog is the ratio of interparticle attractive force (in the fluidlike regime) to particle weight. This law suggests that compaction is ruled by the internal packing structure of the jammed clusters at nearly zero consolidation.

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  • Received 9 November 2004

DOI:https://doi.org/10.1103/PhysRevLett.94.075501

©2005 American Physical Society

Authors & Affiliations

A. Castellanos, J. M. Valverde, and M. A. S. Quintanilla

  • Departamento de Electronica y Electromagnetismo, Universidad de Sevilla, Avenida Reina Mercedes s/n, 41012 Sevilla, Spain

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Issue

Vol. 94, Iss. 7 — 25 February 2005

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