Airborne dust particles from a fluidized bed and those dispersed by a high-speed air stream through a small pipe were observed by a scanning electron microscope and measured by a cascade impactor. The powder material used in this study is ultra-fine powder of kanto loam for industrial testing (JIS Z 8901, standard dust No. 11).
Airborne dust particles from a fluidized bed are mostly aggregated. A high-speed air stream can well disperse these aggregated particles. Where the pipe diameter is 1.5mm∅ and the air velocity is 57m/sec, the particle size distribution of the dispersed airborne dust closely corresponds to that specified by the JIS. But observation by a scanning electron microscope showed that this well-dispersed airborne dust still contained aggregates. Besides it seemed that these aggregates conld be dispersed into small particles without limit. Therefore, if this dust is dispersed by too large of a dispersing effect, it is in danger of over-dispersion. For instance, the size distribution of dust dispersed by the air stream through a 1.1mm∅ pipe with a 104m/sec air velocity, in which the dispersing effect is much larger than the above-mentioned condition, was smaller than that specified by the JIS.
Therefore, when powder, such as kanto loam, which has the possibility of being dispersed into small particles without limit, is used for industrial testing powder, it is necessary to carefully examine the method of dispersing it. The method using a high-speed air stream through a small pipe is very effective for dispersing powder such as kanto loam, because airborne dust can be dispersed into the equilibrium size according to the condition of the air stream, The resulting size distribution of that is very stable.
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