DETERMINATION OF DISPERSION IN ANISOTROPIC MICA AND WOLLASTONITE PARTICLES USING THE LAYER SEDIMENTATION METHOD

摘要

The results of studying the dispersion composition of muscovite mica and wollastonite, whose particle shape is significantly anisometric, are described. A simple method for sedimentation analysis is proposed, which makes it possible quickly and with great accuracy to determine the particle distribution based on their sedimentation diameters. Relationships are obtained which can be used to estimate the geometrical sizes of particles for the considered materials.