1990 Volume 27 Issue 5 Pages 301-307
A method for measuring the particle size distribution of irregularly shaped and large particles in a Reynolds number which varied from 122 to 633 has been developed from the relationship between the pressure drop, ΔPi, across a fixed and a fluidized bed and the superficial velocity, ui. It is recognized by experiments that the equivalent diameter in the fixed and the fluidized bed corresponds to the volume-surface mean diameter, i. e. the specific surface.
The particle size distributions calculated by a computer analysis of the ΔPi and ui were in good agreement with the particle size distributions obtained by the weighed measurement of glass beads, crushed glass and crushed rocks.