Ilmenite, chrome ore, petroleum products.
Leather goods, bags, chrome ore, manganese ore, iron ore, barite, wheat straw, corn silage, rod grass, marble.
Cashewnut, spices from India, manganese ore, iron ore.
Gypsum is an evaporite 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 Uses of Gypsum Gypsum uses include: manufacture of wallboard, cement, plaster of Paris, soil conditioning, a hardening retarder in Portland cement. Varieties of gypsum known as satin spar and alabaster are used for a variety of ornamental purposes; however, their low hardness limits their durability.
Feldspar, any of a group of aluminosilicate minerals that contain calcium, sodium, or potassium. Feldspard make up more than half of Earth 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 crust and mantle. These and an additional score of minerals serve as the basis for naming most of the rocks exposed on Earth surface. Description and Identifying Characteristics Feldsparis 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
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
kaolin, also called china clay, soft white clay that is an essential ingredient in the manufacture of china and porcelain and is widely used in the making of paper, rubber, paint, and many other products. Kaolin is named after the hill in China (Kao-ling) from which it was mined for centuries. Samples of kaolin were first sent to Europe by a French Jesuit missionary around 1700 as examples of the materials used by the Chinese in the manufacture of porcelain. In its natural state kaolin is a white, soft powder consisting principally of the mineral kaolinite, which, under the electron microscope, is seen to consist of roughly hexagonal, platy crystals ranging in size from about 0.1 micrometre to 10 micrometres or even larger. These crystals may take vermicular and booklike forms, and occasionally macroscopic forms approaching millimetre size are found. Kaolin as found in nature usually contains varying amounts of other minerals such as muscovite, quartz, feldspar, and anatase. In addition, crude kaolin is frequently stained yellow by iron hydroxide pigments. It is often necessary to bleach the clay chemically to remove the iron pigment and to wash it with water to remove the other minerals in order to prepare kaolin for commercial use.
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.
crushed and DE-metalize Electric are furnace slag.size 10-20 mm (ASTM C 136/C136M 2014)
Ladle Furnace slag powder available in ABU DHABI
crushed and DE-metalize Electric are furnace slag.size 5-10 mm (ASTM C 136/C136M 2014)
crushed and DE-metalize Electric are furnace slag.size 0-5 mm (ASTM C 136/C136M 2014)
We are export wood saw dust. 1 powder pack in jambo bage 2 1mm up to 10mm, 20mm 30mm as on buyers and importers choice which size he required. We have popular, pine , akasha wood sawdust. We can supply 3000 ton per month.
type(A) type(B) type(C) sio2 67 73 63-67 al2o3 30-1 19-21 28-30 fe2o3 0.2 0.8 0.1 - 0.5 tio2 - 0.3 0.2 cao 0.2 0.56 0.7 mgo 0.4 0.3 - 0.7 0.9 -1 k2o 0.7 2 - 3.1 4.5 - 5 na2o 0.5 0.5 - 1 0.9 - 1.2 so3 0.01 - - color white to cream white to gray white to cream fired strenght 150 380 500 (kg/cm2) dry strenght 25 8 17.
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
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 .....
Egypt, Algeria, Iran orgin availble. Various P205 % values of 24%, 26%, 27%, 28%, 30%, & 36% available. Bulk Quantity from 12500 MT to 25,000 MT. Smaller quantity of 2500 MT to 5000 MT containerized shipments in bags.
Light granules of 0-4mm / 4-10mm / 10-25mm Density: 300-710 kg/m3 Country of origin: iran. Production 200, 000 m3 per annum.
Barite, guar gum, bentonite, granular anhydrous calcium chloride, calcium chloride perils potassium chloride.
