蛍石 CaF2 98%

Fluorite, chemically calcium fluoride (CaF₂), is a typical halide mineral and the primary global feedstock for fluorine supply across fluorochemical, metallurgical, glass and ceramic industries. It forms endogenously from magmatic hydrothermal activity. During magma cooling, magma-separated hydrothermal fluids are rich in fluoride constituents. As these fluids migrate upward through rock fractures, gradual drops in temperature and pressure trigger a chemical reaction:

CaF₂ ≥98%、不純物が少なく、品質が安定した高品質のモンゴル産酸性グレードの蛍石です。フッ酸、フッ素化学品、フッ化アルミニウム、リチウム電池材料の製造に最適です。

不純物の少ない（SiO₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂₂≤1.2% ≤1.2%、S≤0.02%）≤0.02%）高純度 98% の酸性グレードの蛍石塊です。フッ素化学品の製造や鉄鋼の精錬に最適です。カスタムサイズ、天津港からの大量供給を競争力のある価格で提供します。