Few correlations exist to describe the effect of particle shape on the
relationship between superficial velocity and void fraction in homoge
neous fluid beds. Limestone, quartz, bottom ash and pea gravel particl
es were fluidized with water and a data bank of void fractions and flu
idizing velocities was compiled. Each particle type was image analyzed
to yield average shape descriptors, namely aspect ratio, fractal dime
nsion, polygonal harmonic persistences and delta (Piper's) angles. Reg
ression showed that the slope of a log (superficial velocity) versus l
og (void fraction) plot can be fitted using a function of a shape desc
riptor, with the persistence of the third harmonic being the descripto
r yielding the best fit.