Granular materials exhibit several regimes of behavior: plastic, inertial,
fluidized, and entrained flow, hut not all materials can pass through all o
f these states. Our concern is with the criteria that determine the transit
ion from one regime to another and with the boundaries to the various flow
regimes that these criteria define. Experimentally we have focused on fine,
cohesive powders, where the interparticle cohesive force dominates over gr
avitational force and where entrained air can cause moving powder to become
fluidized. [S0031-9007(98)08339-2].