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Silica sand is one of the most common types of sand found in the world. It is used for a wide range of applications. Silica sand is used industrially processing, for making glass, as a filler, and for making molds and castings. The process of producing silica sand involves washing the silica in a modern plant with a magnetic separator, separating the silica into different fraction sizes with a low % of iron and titanium. Various fractional sizes of silica can be produced on demand..
Our standard powder particle sizes average in the range of - 325 mesh, - 100 mesh, 10-50 microns and submicron (< 1 micron). We can also provide many materials in the nanoscale range. We also produce Silicon as rod, ingot, pieces, pellets, disc, granules, wire, and in compound forms, such as oxide. Other shapes are available by request.
Kaolin is derived from the mineral kaolinite that comes from the earth's crust. It is an aluminum silicate represented as Al,O, 2SiO2-2H,O. Kaolin (Chinese clay) is a hydrated aluminum silicate crystalline mineral (kaolinite), formed from weathered granite that once sat beneath the Earth's surface. It is one of the most common minerals on Earth and is easily recognized by its fine particle size and plate-like structure. The world's largest: reserves of premium kaolin are located in the United States and Brazil. Kutch reserves are good in India too.
Bauxite is a sedimentary rock with a relatively high aluminium content. It is the world's main source of aluminium and gallium. Bauxite consists mostly of the aluminium minerals gibbsite (Al(OH)3), boehmite (Y-AlO(OH)) and diaspore (α-AlO(OH)), mixed with the two iron oxides goethite (FeO(OH)) and haematite (Fe2O3), the aluminium clay mineral kaolinite (Al2Si2O5(OH)4) and small amounts of anatase (TiO2) and ilmenite (FeTiO3 or FeO.TiO2).[1] Bauxite appears dull in luster and is reddish-brown, white, or tan.
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