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Silicon and aluminogenin of potassium sodium feldspar were removed using the PTMS Electromagnetic Separator protocol
published date: 2024/5/2

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A common feldspar mineral, more common in pegmatite and feldsic igneous rocks such as granite, also seen in primary metamorphic rocks, and as spontaneous potassium sodium feldspase in some sedimentary rocks. Potassium sodium feldspar generally constitutes brittle glassy crystals of various colors. The PTMS magnetic separator can remove the iron (FE2O3) from the potassium feldspar, which can be used to make glass and ceramics, but it is mainly a mineral magnetic separation.

PTMS magnetic separation


Potassium sodium feldspar is the sodium mineral of the solid solution series and alkaline feldspar series. With three oblique frame shape, silicon and aluminum are tetrahedral coordination, forming a large vacancy (i. e., dot matrix orientation), mainly occupied by cationic sodium. Although all silicogenin and aluminogenin have tetrahedral orientation in the PTMS Electromagnetic Separator scheme, the specific orientation are different.

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The distribution of silicon and alumogenin is highly ordered at low temperature, and it is much more dysregulated at high temperatures of about 1100℃. Using PTMS Electromagnetic Separator solution to remove, potassium sodium feldspar mineral in addition to industrial materials, in the ceramic industry accounted for more than 30%, but also widely used in chemical industry and other work.
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CHINA CLAY PTMS magnetic separation 20240502

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