Feldspar, any of a group of aluminosilicate minerals that contain calcium, sodium, or potassium. Feldspard make up more than half of Earth's crust, and professional literature about them constitutes a large percentage of the literature of mineralogy. Of the more than 3,000 known mineral species, less than 0.1 percent make up the bulk of Earth's crust and mantle. These and an additional score of minerals serve as the basis for naming most of the rocks exposed on Earth's surface. Description and Identifying Characteristics Feldspar is derived from the German word feld,which means field, and spar, which means crystal. This name reflects the minerals abundance, as most crystalline material found in the field is feldspar. Potassium feldspard are the feldspar minerals in which the silicate tetrahedral and aluminum tetrahedra are bound with potassium ions, rather than sodium or calcium ions as in the plagioclase feldspar subgroup. The potassium feldspar group is composed of three mineral polymorphs, each having the same chemical composition, but slightly different crystal structures. Technically these are distinct minerals, but their physical properties are so similar that they are usually only identified as potassium feldspar in the field. Using other minerals in the rock to determine the host rocks identity is often the most useful guide to their probable identity. felsic plutonic igneous rocks and metamorphic rocks Microcline
Nepheline is an important feldspathoid mineral. It is white, grey or yellow in colour with a vitreous lustre and a poor cleavage. The name Nepheline comes from the Greek word nephele, which means cloud, because it becomes strongly clouded when put in strong acid. Nepheline only forms in silica-poor rocks. It is almost never associated with quartz. It may be found in some contact metamorphosed rocks otherwise it occurs in alkaline complexes in igneous rocks. Nepheline is mostly found in the rock Nepheline Syenite in nature.
Gypsum is an evaporate mineral most commonly found in layered sedimentary deposits in association with halite, anhydrite, sulfur, calcite, and dolomite. Gypsum (CaSO4.2H2O) is very similar to Anhydrite (CaSO4). The chemical difference is that gypsum contains two waters and anhydrite is without water. Gypsum is the most common sulfate mineral.
Chemical analysis for slag chrome: Sio2 35.76 Mgo 27.88 Al2o3 24.56 Cr2o3 5.58 Fe2o3 2.00 Cao 2.28 Tio2 0.45 So3 0.65 Na2o 0.18 Mno 0.13 K2o 0.09
CaSO4.2h2o 95.30% Silica Sio2 2.90% Aluminum Al2O3 12.46% sodium Na2O 0.1% Magnesium Mgo 2.61% Potassium k2O 0.05% Titanium TiO2 0.31% Manganese Mn2O3 0.02% Calcium CaO 0.94% Phosphorus P2O3 0.02% Sulfate SO2 0% Iron Fe2O3 2.69% L.O.I 13.41%
Silica - SiO2 - 97.2 Iron - Fe2O3 - 0.36 Aluminium - Al2o3 - 0.52 Calcium - CaO - 0.76 Magnesium - MgO - 0.25 Sodium - Na2O - 0.1 Potassium - K2O - 0.14 Sulphate - SO3 - 0.11 Chloride - CI - 0.01 Loss on ig - LOI - 0.22 Moisture - 0.1
Chemical analysis: Baso4 90% min Water soluble solids 0.1% max Moisture content 1% max Size 200 mesh Physical analysis : S.G 4.1 gr / cm 3 min
LOI 33.1 SiO2 25.3 Al2O3 5.02 Fe2O3 2.86 CaO 19.6 MgO 10.6 SO3 0.26 K2O 0.28 Na2O 1.50 CI 0.01 TIOZ 0.21 NiO 0.02 ZnO 0.01 P2O3 0.05 Cr2O3 0.03 MnO .....
Silica 64.94 Aluminum 12.46 Sodium 1.99 Magnesium 2.61 Potassium 0.26 Titanium 0.31 Manganese 0.02 Calcium 0.94 Phosphorus 0.02 Sulfate 0 Iron 2.69 L.O.I 13.41
Chemical analysis for chrome: Chrome cr 54% min Silicon si 4% max Carbon c 8% max Phosphorus p 0.030 % max Sulfur s 0.030 % max.
Computer motherboard, drained battery scrap, drained battery scrap, high-grade raw magnesite lumps (magnesium carbonate), fluorspar, bauxite, talc(soapstone), kaolin, baryte, and gypsum.
Talc, common silicate mineral that is distinguished from almost all other minerals by its extreme softness (it has the lowest rating on the Mohs scale of hardness). Its soapy or greasy feel accounts for the namesoapstone given to compact aggregates of talc and other rock-forming minerals. Dense aggregates of high-purity talc are called steatite. Since ancient times, soapstones have been employed for carvings, ornaments, and utensils; Assyrian cylinder seals, Egyptian scarabs, and Chinese statuary are notable examples. Soapstones are resistant to most reagents and to moderate heat; thus, they are especially suitable for sinks and countertops. Talc is also used in lubricants, leather dressings, toilet and dusting powders, and certain marking pencils. It is used as a filler in ceramics, paint, paper, roofing materials, plastic, and rubber; as a carrier in insecticides; and as a mild abrasive in the polishing of cereal grains such as rice and corn.
Silicon dioxide, also known as silica (from the Latin silex), is a chemical compound that is an oxide of silicon with thechemical formula SiO2. It has been known since ancient times. Silica is most commonly found in nature as quartz, as well as in various living organisms. In many parts of the world, silica is the major constituent of sand. Silica is one of the most complex and most abundant families of materials, existing both as several minerals and being produced synthetically. Notable examples include fused quartz, crystal, fumed silica, silica gel, and aerogels. Applications range from structural materials to microelectronics to components used in the food industry.
Bentonite is an absorbent aluminium phyllosilicate clay consisting mostly of montmorillonite. It was named by Wilbur C. Knight in 1898 after the Cretaceous Benton Shale near Rock River, Wyoming. The different types of bentonite are each named after the respective dominant element, such as potassium (K), sodium (Na), calcium (Ca), and aluminium (Al). Experts debate a number of nomenclatorial problems with the classification of bentonite clays. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin. For industrial purposes, two main classes of bentonite exist: sodium and calcium bentonite. In stratigraphy and tephrochronology, completely devitrified (weathered volcanic glass) ash-fall beds are commonly referred to as K-bentonites when the dominant clay species is illite. In addition to montmorillonite and illite anther common clay species that is sometimes dominant is kaolinite. Kaolinite-dominated clays are commonly referred to as tonsteins and are typically associated withcoal.
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our company can offer you Barite. Barite or baryte is a mineral containing barium sulfate. Its name is originally derived from the Greek word barys meaning heavy. This mineral belongs to the Barite Mineral Group along with anglesite, celestine and anhydrite. It has quite a beautiful appearance. This mineral ore is also known as Heavy Spar, Barytine, Schwerspath, Barytite and Baryte. It is the main source of barium. Aggregates of barite and sand is called rose rock which appears reddish in due to its iron content. It's commonly known as barite rose.
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Zirconium silicate, also zirconium orthosilicate, (ZrSiO4) is a chemical compound, a silicate of zirconium. It occurs in nature as the zircon, a silicate mineral. Zirconium silicate is also sometimes known as zircon flour. Zirconium silicate is usually colorless, but impurities induce various colorations. It is insoluble in water, acids, alkali andaqua regia. Hardness is 7.5 on the Mohs scale. Uses: Zirconium silicate is used for manufacturing refractory materials for applications where resistance to corrosion by alkalimaterials is required. It is also used in production of some ceramics, enamels, and ceramic glazes. In enamels and glazes it serves as an opacifier. It can be also present in some cements. Another use of zirconium silicate is as beads for milling and grinding. Thin films of zirconium silicate and hafnium silicate produced by chemical vapor deposition, most often MOCVD, can be used as a high-k dielectric as a replacement for silicon dioxide in semiconductors. Zirconium silicates have also been studied for potential use in medical applications. For example, ZS-9 is a zirconium silicate that was designed specifically to trap potassium ions over other ions throughout the gastrointestinal tract. It is undergoing clinical trials for the treatment of hyperkalemia. Zirconium disillicate is used in some Dental Crowns because of its hardness and because it is chemically nonreactive.
Calcium carbonate is a chemical compound with the formula CaCO3. It is a common substance found in rocks as theminerals calcite and aragonite (most notably as limestone) and is the main component of pearls and the shells of marine organisms, snails, and eggs. Calcium carbonate is the active ingredient in agricultural lime and is created when calcium ions in hard water react with carbonate ions to create limescale. It is medicinally used as a calcium supplement or as an antacid, but excessive consumption can be hazardous.
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