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The effect of boundaries on the plane Couette flow of granular materials: a bifurcation analysis

Published online by Cambridge University Press:  25 October 1999

P. R. NOTT
Affiliation:
Department of Chemical Engineering, Indian Institute of Science, Bangalore 560012, India
M. ALAM
Affiliation:
Department of Chemical Engineering, Indian Institute of Science, Bangalore 560012, India
K. AGRAWAL
Affiliation:
Department of Chemical Engineering, Princeton University, Princeton, NJ 08544, USA
R. JACKSON
Affiliation:
Department of Chemical Engineering, Princeton University, Princeton, NJ 08544, USA
S. SUNDARESAN
Affiliation:
Department of Chemical Engineering, Princeton University, Princeton, NJ 08544, USA

Abstract

The tendency of granular materials in rapid shear ow to form non-uniform structures is well documented in the literature. Through a linear stability analysis of the solution of continuum equations for rapid shear flow of a uniform granular material, performed by Savage (1992) and others subsequently, it has been shown that an infinite plane shearing motion may be unstable in the Lyapunov sense, provided the mean volume fraction of particles is above a critical value. This instability leads to the formation of alternating layers of high and low particle concentrations oriented parallel to the plane of shear. Computer simulations, on the other hand, reveal that non-uniform structures are possible even when the mean volume fraction of particles is small. In the present study, we have examined the structure of fully developed layered solutions, by making use of numerical continuation techniques and bifurcation theory. It is shown that the continuum equations do predict the existence of layered solutions of high amplitude even when the uniform state is linearly stable. An analysis of the effect of bounding walls on the bifurcation structure reveals that the nature of the wall boundary conditions plays a pivotal role in selecting that branch of non-uniform solutions which emerges as the primary branch. This demonstrates unequivocally that the results on the stability of bounded shear flow of granular materials presented previously by Wang et al. (1996) are, in general, based on erroneous base states.

Type
Research Article
Copyright
© 1999 Cambridge University Press

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