Dolomite [CaMg(CO3)2] is an intolerable impurity in phosphate ores, due to its MgO content. In high-dolomite Florida phosphate deposits, the dolomite could, in principle, be separated without any need for crushing and grinding the material by any process that could function at a relatively coarse size. Even though the dolomite and apatite are sufficiently liberated, they have very similar densities with apatite only slightly denser than dolomite, making density separations difficult.
A sample of high-dolomite phosphate from Florida contained dolomite pebbles with a mean density of 2.51 g/cm3, and apatite pebbles ranging from 2.55 to 2.78 g/cm3. To separate the dolomite from the apatite, a unique laboratory scale jig was constructed that allows for easy alteration of effective jigging properties. This jig was operated in batch mode with a feed sized to 6.73 mm x 3.36 mm to examine the effects of key parameters, pulsation rate and jig bed depth. It was found that a pulsation rate of approximately 200 pulses/minute gave the best separation results. A pulsation rate of 100 pulses/minute resulted in incomplete separation of the dolomite and apatite, while a rate of 300 pulses/minute did not show any further improvement over a rate of 200 pulses/minute. Analysis of the jig bed at the conclusion of each test showed that most of the separation occurred in the bottom 1 inch (25 mm) of the jig bed.
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