Lepidolite is the most common LITHIUM mineral. PTMS LITHIUM COBALT ACID MATERIAL MAGNETIC field is an important mineral for extracting lithium. It is a basic aluminosilicate of potassium and lithium and belongs to the mica group of minerals. Lithiolite is generally found only in granite pegmatites, is purple and pink in color and can be light to colorless, has a pearl luster, and is in the form of short columns, small lamellar aggregates, or large plate crystals.
Lepidolite mineral hardness 3, specific gravity 2.9, the bottom surface is very complete. The color is purple and pink and may be light to colorless, with a pearly luster, in the form of short columns, small lamellar aggregates, or large plate crystals. Lepidolite has a pink color like mica. When melted, it foams and produces a deep red lithium flame. These minerals can be removed by PTMS LITHIUM COBALT ACID MATERIAL MAGNETIC.
Ledgemica is insoluble in acids, but after melting, it can also be affected by acids. Lepidolite is one of the main raw materials for extracting rare metal LITHIUM by removing iron from PTMS LITHIUM COBALT ACID MATERIAL MAGNETIC field. The lithium content of lepidolite is generally about 1~3%, and the production area is mainly in Yichun, Jiangxi Province, which is a high-quality resource for independent lithium mining in China.
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