Mar 06, 2023
Ceramic Refractory Insulation - Fire Bricks ( Alumina 55%)
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Potash Feldspar
FELDSPAR IS ONE OF THE MOST COMMON MINERALS USED IN THE CERAMIC AND GLASS INDUSTRIES. IT IS AN ALKALI-BEARING ALUMINOSILICATE CORRESPONDING TO THE EMPIRICAL FORMULA R20, AJO3, 6SIO2, WHERE R REPRESENTS AN ALKALI METAL. AS NONE OF THE FELDSPAR GROUP OF MINERALS IS FOUND PURE, POTASH FELDSPAR ALWAYS CONTAINS SOME SODA FELDSPAR AND VICE-VERSA WITH VARYING AMOUNTS OF FREE QUARTZ, IRON OXIDE AND TRACES OF LIME AND MAGNESIA RESULTING IN A RANGE OF COLORS.
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DOLOMITE
DOLOMITE IS A NATURALLY OCCURRING MINERAL COMPOSED OF CALCIUM MAGNESIUM CARBONATE (CAMG(CO₃)₂). IT IS FOUND IN SEDIMENTARY ROCK FORMATIONS AND IS KNOWN FOR ITS CRYSTALLINE STRUCTURE, HIGH PURITY, AND EXCELLENT CHEMICAL PROPERTIES. DOLOMITE OCCURS IN WHITE, GRAY, PINK, OR BROWN COLORS, DEPENDING ON ITS MINERAL COMPOSITION AND IMPURITIES. WE AT VASTTRADEZI TAKE PRIDE IN SUPPLYING HIGH-QUALITY DOLOMITE, MEETING THE DIVERSE NEEDS OF INDUSTRIES WORLDWIDE. OUR DOLOMITE IS KNOWN FOR ITS HIGH PURITY, EXCELLENT WHITENESS, AND OPTIMAL CHEMICAL COMPOSITION, MAKING IT IDEAL FOR APPLICATIONS IN STEEL, GLASS, CERAMICS, CONSTRUCTION, AND ETC...
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SODA FELDSPAR
FELDSPAR IS ONE OF THE MOST COMMON MINERALS USED IN THE CERAMIC AND GLASS INDUSTRIES. IT IS AN ALKALI-BEARING ALUMINOSILICATE CORRESPONDING TO THE EMPIRICAL FORMULA R20, AJO3, 6SIO2, WHERE R REPRESENTS AN ALKALI METAL. AS NONE OF THE FELDSPAR GROUP OF MINERALS IS FOUND PURE, POTASH FELDSPAR ALWAYS CONTAINS SOME SODA FELDSPAR AND VICE-VERSA WITH VARYING AMOUNTS OF FREE QUARTZ, IRON OXIDE AND TRACES OF LIME AND MAGNESIA RESULTING IN A RANGE OF COLORS.
12.00
QUARTZ
QUARTZ IS A SILICA (SILICON DIOXIDE)-BASED HARD, CRYSTALLINE MINERAL. SIO2 IS THE OVERALL CHEMICAL FORMULA OF SILICON DIOXIDE. THE ATOMS ARE CONNECTED IN A CONTINUOUS FRAMEWORK OF SIO4 SILICON–OXYGEN TETRAHEDRA, WITH EACH OXYGEN BEING SHARED BETWEEN TWO TETRAHEDRA. AS A RESULT, QUARTZ IS CATEGORIZED AS AN OXIDE MINERAL COMPOSITIONALLY AND AS A FRAMEWORK SILICATE MINERAL ARCHITECTURALLY. AFTER FELDSPAR, QUARTZ IS THE SECOND MOST COMMON MINERAL IN THE CONTINENTAL CRUST OF EARTH. THERE ARE TWO TYPES OF QUARTZ: THE CHIRAL NORMAL Α-QUARTZ AND THE HIGH-TEMPERATURE Β-QUARTZ. THE TRANSITION TEMPERATURE OF Α-QUARTZ TO Β-QUARTZ IS 573 °C (846 K; 1,063 °F), WHICH OCCURS SUDDENLY.
16.00
Kaolin Clay
Al2O3 2SiO2·2H2O
KAOLIN / CHINA CLAY - KAOLIN IS A DEPOSIT OF NATURALLY OCCURRING MINERALS COMPRISING HYDRATED ALUMINUM SILICATE. THESE MINERALS, COMMONLY KNOWN AS WHITE CLAY OR CHINA CLAY, HAVE FAVORABLE QUALITIES THAT MAKE THEM IDEAL FOR INDUSTRIAL AND COMMERCIAL PURPOSES. AS A RESULT, THE KAOLIN MINING AND PROCESSING PROCEDURES TAKE THE NATURE OF THE CRUDE RESOURCES AND THE FINAL USE OF THE PRODUCTS INTO ACCOUNT.
27.00
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