Solids flow characteristics of coal ash are investigated with the
measurement of the local solids
flux, local solids concentration, and spatial distribution of particle
size. Two sets of the solids
sampling probe are used to quantify the local solids flux at different
radial and axial locations.
The macroscopic flow structure is presented by analyzing the
radial profiles of solids flux and
the local particle size distributions, while the mesoscale flow
structure is illustrated on the basis
of probability density function of instantaneous solids concentration,
the intermittency index,
and the cluster frequency. It is found that both macroscopic and
mesoscopic structures of gas−solid flow of coal ash are different from those of commonly studied
fluid catalytic cracking and
sand particles. The differences include higher upward and downward
solids fluxes in the lower
dense region, significant particle segregation, and more uniform
annular flow. Furthermore, a
semiempirical model taking into consideration the higher slip velocity
between gas and solids
is developed to account for the radial profiles of the solids flux in
the upper dilute region of the
riser.