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Found 65 Results For "
fluorspar powder
"
Vloeispaat van metallurgische kwaliteit met CaF₂ ≥97%. Ultra-lage onzuiverheden (S≤0,08%, P≤0,03%) zorgen voor een zeer zuivere staalproductie en productie van lasstaven. Directe mijnbron, stabiele aanvoer, flexibele vormen (klonten/poeder) en klaar voor export vanuit de haven van Tianjin.
Zeer zuivere vloeispaatklontjes van 98% zuurgraad met lage onzuiverheden (SiO₂≤1,2%, S≤0,02%). Ideaal voor fluorchemische productie en staalsmelten. Aangepaste maatvoering, bulklevering vanuit de haven van Tianjin met concurrerende prijzen.
Zeer zuivere vloeispaatklonten met CaF₂ ≥90%, afkomstig uit Mongoolse afzettingen. Beschikt over stabiele kwaliteit, lage onzuiverheden, uitstekende vloei-efficiëntie en meerdere deeltjesgroottes. Toeleveringsketen van mijn tot haven met betrouwbare export via de haven van 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:
Metallurgisch vloeispaat van Mongolische oorsprong met 75% CaF₂. Zorgt voor een efficiënt vloeimiddel bij de staalproductie, gecontroleerde onzuiverheden en een stabiele aanvoer. Verkrijgbaar in klontjes-/poedervormen met flexibele verpakkings- en exportvoorwaarden.
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:
