Particle Pressure in a Sheared Suspension: A Bridge from Osmosis to Granular Dilatancy

Angélique Deboeuf, Georges Gauthier, Jérôme Martin, Yevgeny Yurkovetsky, and Jeffrey F. Morris
Phys. Rev. Lett. 102, 108301 – Published 9 March 2009

Abstract

The normal stress exerted by particles in a sheared suspension is measured by analogy with a method used to measure osmotic pressure in solutions. Particles in a liquid are confined by a fine screen to a gap between two vertical concentric cylinders, the inner of which rotates. Pressure in the liquid is sensed either by a manometer or by a pressure transducer across the screen. The particles are large enough so that Brownian motion and equilibrium osmotic pressure are vanishingly small. The measured pressure yields the shear-induced particle pressure Π, the nonequilibrium continuation of equilibrium osmotic pressure. For volume fractions 0.3ϕ0.5, Π is strongly dependent on ϕ, and linear in shear rate. Comparisons of the measured particle pressure with modeling and simulation show good agreement.

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  • Received 10 July 2008

DOI:https://doi.org/10.1103/PhysRevLett.102.108301

©2009 American Physical Society

Authors & Affiliations

Angélique Deboeuf, Georges Gauthier, and Jérôme Martin

  • Univ Pierre et Marie Curie-Paris6, Univ Paris-Sud, CNRS, Laboratoire FAST, Campus universitaire d’Orsay, 91405 Orsay Cedex, France

Yevgeny Yurkovetsky and Jeffrey F. Morris

  • Levich Institute and Chemical Engineering, City College of New York, New York, New York 10031, USA

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Issue

Vol. 102, Iss. 10 — 13 March 2009

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