Meso-scale structures that take the form of clusters and streamers are comm
only observed in dilute gas-particle flows, such as those encountered in ri
sers. Continuum equations for gas-particle flows, coupled with constitutive
equations for particle-phase stress deduced from kinetic theory of granula
r materials, can capture the formation of such meso-scale structures. These
structures arise as a result of an inertial instability associated with th
e relative motion between the gas and particle phases, and an instability d
ue to damping of the fluctuating motion of particles by the interstitial fl
uid and inelastic collisions between particles. It is demonstrated that the
mesoscale structures are too small, and hence too expensive, to be resolve
d completely in simulation of gas-particle flows in large process vessels.
At the same time, failure to resolve completely the meso-scale structures i
n a simulation leads to grossly inaccurate estimates of inter-phase drag, p
roduction/dissipation of pseudo-thermal energy associated with particle flu
ctuations, the effective particle-phase pressure and the effective viscosit
ies. It is established that coarse-grid simulation of gas-particle flows mu
st include sub-grid models, to account for the effects of the unresolved me
soscale structures. An approach to developing a plausible sub-grid model is
proposed.