INTRODUCTION

When a granular material is sheared at a sufficiently high rate, the shear stress and the normal stress required to maintain its motion are observed to vary with the square of the shear rate (Bagnold (1954), Savage (1972), Savage & McKeown (1983), Savage & Sayed (1984), Hanes & Inman (1985a)). The interpretation of these observations is that, at high shear rates, the dominant mechanism of momentum transfer is collisions between grains, with the interstitial liquid or gas playing a relatively minor role.

There is an obvious analogy between the colliding macroscopic grains of a sheared granular material and the agitated molecules of a dense gas. There are also several important differences: collisions between grains are inevitably inelastic; typical grain flows involve spatial variations over far fewer grains than their molecular counterparts; and, consequently, the influence of boundaries is far more pervasive.

Exploiting the analogy, methods from the kinetic theory of dense gases have been adopted and extended to derive balance laws, constitutive relations, and boundary conditions for systems of macroscopic, dissipative, grains. Jenkins (1987) provides a brief review of this activity.