Found 65 Results For "
fluorspar powder
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CaF₂ ≥97% を含む冶金グレードの蛍石。超低不純物 (S≤0.08%、P≤0.03%) により、高純度の製鋼および溶接棒の製造が保証されます。直接採掘、安定供給、柔軟な形状(塊状/粉末)、天津港からの輸出対応。
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。
CaF₂ ≥90% を含む高純度の蛍石塊で、モンゴルの鉱床から採取されます。安定した品質、低不純物、優れたフラックス効率、および複数の粒子サイズが特徴です。天津港経由で確実に輸出できる鉱山から港までのサプライチェーン。
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:
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:
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:
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:
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: