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fluorspar powder
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Fluorspar Tingkat Metalurgi dengan CaF₂ ≥97%. Pengotor yang sangat rendah (S≤0,08%, P≤0,03%) memastikan pembuatan baja & produksi batang las dengan kemurnian tinggi. Sumber tambang langsung, pasokan stabil, bentuk fleksibel (benjolan/bubuk), dan siap ekspor dari Pelabuhan Tianjin.
Gumpalan fluorspar tingkat asam 98% dengan kemurnian tinggi dengan pengotor rendah (SiO₂≤1,2%, S≤0,02%). Ideal untuk produksi fluorokimia dan peleburan baja. Ukuran khusus, pasokan massal dari Pelabuhan Tianjin dengan harga kompetitif.
Gumpalan fluorspar dengan kemurnian tinggi dengan CaF₂ ≥90%, bersumber dari endapan Mongolia. Menampilkan kualitas yang stabil, pengotor rendah, efisiensi fluks yang sangat baik, dan berbagai ukuran partikel. Rantai pasokan tambang-ke-pelabuhan dengan ekspor yang andal melalui Pelabuhan Tianjin.
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:
Fluorspar metalurgi asal Mongolia dengan 75% CaF₂. Memastikan fluks pembuatan baja yang efisien, pengotor yang terkontrol, dan pasokan yang stabil. Tersedia dalam bentuk gumpalan/bubuk dengan kemasan fleksibel & syarat ekspor.
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: