Journal of Fluid Mechanics



Stability of plane Couette flow of a granular material


MEHEBOOB ALAM a1p1 and PRABHU R. NOTT a2
a1 Department of Mechanical Engineering, Indian Institute of Science, Bangalore 560012, India
a2 Department of Chemical Engineering, Indian Institute of Science, Bangalore 560012, India; e-mail: prnott@chemeng.iisc.ernet.in

Abstract

This paper presents a linear stability analysis of plane Couette flow of a granular material using a kinetic-theory-based model for the rheology of the medium. The stability analysis, restricted to two-dimensional disturbances, is carried out for three illustrative sets of grain and wall properties which correspond to the walls being perfectly adiabatic, and sources and sinks of fluctuational energy. When the walls are not adiabatic and the Couette gap H is sufficiently large, the base state of steady fully developed flow consists of a slowly deforming ‘plug’ layer where the bulk density is close to that of maximum packing and a rapidly shearing layer where the bulk density is considerably lower. The plug is adjacent to the wall when the latter acts as a sink of energy and is centred at the symmetry axis when it acts as a source of energy. For each set of properties, stability is determined for a range of H and the mean solids fraction [bar, vee]. For a given value of [bar, vee], the flow is stable if H is sufficiently small; as H increases it is susceptible to instabilities in the form of cross-stream layering waves with no variation in the flow direction, and stationary and travelling waves with variation in the flow and gradient directions. The layering instability prevails over a substantial range of H and [bar, vee] for all sets of wall properties. However, it grows far slower than the strong stationary and travelling wave instabilities which become active at larger H. When the walls act as energy sinks, the strong travelling wave instability is absent altogether, and instead there are relatively slow growing long-wave instabilities. For the case of adiabatic walls there is another stationary instability for dilute flows when the grain collisions are quasi-elastic; these modes become stable when grain collisions are perfectly elastic or very inelastic. Instability of all modes is driven by the inelasticity of grain collisions.

(Received August 25 1997)
(Revised July 13 1998)


Correspondence:
p1 Current address: Department of Applied Maths and Engineering Sciences, University of California, San Diego, La Jolla, CA 92093, USA.


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