A microscopic method for the determination of the particle size distribution in ground minerals by means of a scanning electron microscope (SEM) was established.
1. A special sample holder, for this purpose, was used in order to take photographs of both the sample and the standard scale under the same conditions.
2. The pieces of micro-mesh sieves were used as a standard scale, and their lengths were measured precisely by an optical microscope and SEM.
3. Because this SEM is equiped with a special coil, the maximum deformation ratio of the micro photographs of the images was 3.5%.
4. Presentation of a better technique in sampling, counting and calculation of particle size analysis of quartz powder by the SEM.
5. The particle size distribution curve obtained by the SEM indicated a low proportion of the quantity of particles in the region of the small particle diameter, compared with the results of the sedimentation balance method.
6. A particle size analysis using the SEM, an optical microscope (OM) and a sedimentation balance (SB) was performed on a sample of spherical glass beads with larger particle sizes than those of the quartz powder. The particle size distribution curve based on the number of particles obtained by the OM indicated a low proportion in the region of small particle diameters compared with the curve obtained by the SEM. But the curves based on the weights of the particles obtained by the SEM, the OM and the SB were not so dissimilar.
7. It seems that the particles easily observed are overestimated by the microscopic method as compared with the sedimentation balance method.
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