Some peculiar features of granular materials (smooth, identical spheres) in rapid flow are the normal pressure differences and the related anisotropy of the velocity distribution function $f^{\mathrm{}\left(1\right)\mathrm{}}.$ Kinetic theories have been proposed that account for the anisotropy, mostly based on a generalization of the Chapman-Enskog expansion [N. Sela and I. Goldhirsch, J. Fluid Mech. 361, 41 (1998)]. In the present paper, we approach the problem differently by means of the method of moments; previously, similar theories have been constructed for the nearly elastic behavior of granular matter but were not able to predict the normal pressures differences. To overcome these restrictions, we use as an approximation of the $f^{\mathrm{}\left(1\right)\mathrm{}}$ a truncated series expansion in Hermite polynomials around the Maxwellian distribution function. We used the approximated $f^{\mathrm{}\left(1\right)\mathrm{}}$ to evaluate the collisional source term and calculated all the resulting integrals; also, the difference in the mean velocity of the two colliding particles has been taken into account. To simulate the granular flows, all the second-order moment balances are considered together with the mass and momentum balances. In balance equations of the $N\mathrm{th}$-order moments, the $\mathrm{}(N+1\mathrm{})\mathrm{}\mathrm{th}$-order moments (and their derivatives) appear: we therefore introduced closure equations to express them as functions of lower-order moments by a generalization of the “elementary kinetic theory,” instead of the classical procedure of neglecting the $\mathrm{}(N+1\mathrm{})\mathrm{}\mathrm{th}$-order moments and their derivatives. We applied the model to the translational flow on an inclined chute obtaining the profiles of the solid volumetric fraction, the mean velocity, and all the second-order moments. The theoretical results have been compared with experimental data [E. Azanza, F. Chevoir, and P. Moucheront, J. Fluid Mech. 400, 199 (1999); T. G. Drake, J. Fluid Mech. 225, 121 (1991)] and all the features of the flow are reflected by the model: the decreasing exponential profile of the solid volumetric fraction, the parabolic shape of the mean velocity, the constancy of the granular temperature and of its components. Besides, the model predicts the normal pressures differences, typical of the granular materials.

• Received 15 March 2002

DOI:https://doi.org/10.1103/PhysRevE.66.041304