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The existence forms of iron in potassium albite are relatively complex, mainly in the following cases: mainly hematite and limonite, in the form of micro-fine stars scattered in gangue or mica minerals, the particle size is generally coarser, this aggregate is easy to distinguish; PTMS magnetic separator can remove the iron (FE2O3) in potassium albite.

PTMS magnetic separation

 
The iron oxide formed by iron staining permeates the surface of potassium feldspar, or distributes along cracks, intermineral and cleavage fractures of potassium feldspar. The iron oxide formed by iron staining greatly increases the difficulty of iron removal by PTMS magnetic separator. Gangue minerals containing iron, such as ferrotitanite, biotite, tourmaline, hornblende, epidote, epidote, pyrite, etc.,

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Although the content of such minerals is generally low, it has a greater impact on the quality of feldspar concentrate, and such minerals are difficult to be removed by traditional single processing methods, which leads to the emergence of PTMS magnetic separator iron removal process, increasing the cost of mineral processing. Because the iron minerals, biotite, hornblende and tourmaline in feldspar have certain magnetic properties, they can be separated from feldspar under the action of an applied magnetic field.
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