wet high intensity magnetic separator

Light minerals mainly refer to feldspar. The Al in feldspar is sometimes replaced by Fe, and its content can be as high as 0.5% to 0.7%. In addition, there are Muscovite, kaolinite, dolomite, calcite, etc., in these minerals, Fe is in the form of isomorphic crystal lattice, because its density is similar to quartz, so the separation is quite difficult, the need for PTMS magnetic separation.

PTMS magnetic separation

 
In the film iron, the particles in the quartz sand are white in pure condition, and brown, gray, yellow and even red after pollution. The pollution of quartz particles is mainly iron pollution and mud pollution. During the ore-forming process, some minerals are produced in thin films or particles inside or on the surface of quartz minerals, and iron is eliminated by the process of PTMS magnetic separation.

what is magnetic separation method？

 
In fact, the so-called thin film iron mostly refers to this situation, in the connective body or lattice, the different minerals in the quartz sand are basically in a state of monomer dissociation, but the situation of the particles in the quartz sand and other iron-bearing minerals together still exists, the connective body is mostly dark minerals, some wrapped in the interior of its particles, some embedded in the edge of the particles, becoming a mineral aggregate. This is called wrapping iron. PTMS magnetic separation can remove coated iron.
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