The difference of magnetization coefficient of various minerals in ore is the mineral separation process in PTMS Electromagnetic Separator magnetic field. When selected strong magnetic ores, the magnetic coefficient of strong magnetic minerals, for example, the magnetic coefficient of magnetite (X0 80,000X10-6) than its associated minerals quartz, common amphibole, pyroxene and garnet and so on than the magnetic coefficient (X0 below 20Xl0-5) several hundred times larger.
When PTMS Electromagnetic Separator separates weakly magnetic ores, the magnetic components - hematite, pyrolusite, limnite and ferrugmangite - the specific magnetic coefficient (X0 from 25×10-6 to 300X10-6) is only higher than that of non-magnetic minerals - quartz and limestone. And so on than the magnetic coefficient (X0 below 25×10-6) several times. Strongly magnetic minerals have a high specific magnetic susceptibility.
In most cases, in the magnetic field of the PTMS Electromagnetic Separator, the magnetic force acting on the mineral greatly outweighs gravity. When dealing with weakly magnetic ores, even in the magnetic separator field of high intensity (magnetic field strength up to 1800 ost), the magnetic force acting on the alkaline component exceeds gravity by a little. This is due to the fact that the specific magnetic coefficient of magnetic minerals in strongly magnetic minerals is not large.
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Dry-type PTMS MAGNETIC SEPARATOR bearing spare parts replacement skills
