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.
we produce high-quality ceramic tiles and porcelain tiles (All Types of Floor and Wall Tiles) Since the beginning of 2018, we have been involved in the most modern tile manufacturers in the Middle East, which in large formats also produce slabs up to 16 - 320 cm with a thickness of 6 to 25 mm. our tiles can be delivered to any country in the world.
Since mid 2015, we have been producing high-quality ceramic tiles and porcelain tiles (All Types of Floor and Wall Tiles) Since the beginning of 2018, we have been involved in the most modern tile manufacturers in the Middle East, which in large formats also produce slabs up to 160 320 cm with a thickness of 6 to 25 mm. our tiles can be delivered to any country in the world.
We have been manufacturer of limestone for over 20 years.
we can offer you Bentonite. 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.
we can offer you Ball Clay. Ball clays are kaolinitic sedimentary clays that commonly consist of 20-80% kaolinite, 10-25% mica, 6-65% quartz. Localized seams in the same deposit have variations in composition, including the quantity of the major minerals, accessory minerals and carbonaceous materials such as lignite. They are fine-grained and plastic in nature, and, unlike most earthenware clays, produce a fine quality white-coloured pottery body when fired, which is the key to their popularity with potters. Ball clays are relatively scarce deposits due to the combination of geological factors needed for their formation and preservation. They are mined in parts of the Eastern United States and from three sites in Devon and Dorset in South West England. They are commonly used in the construction of many ceramic articles, where their primary role, apart from their white colour, is to either to impart plasticity or to aid rheological stability during the shaping processes.
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.
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.
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.
Long alkyd 160x is a high viscosity resin. Gives good color, radiant gloss, excellent brush-ability, and rapid set and through drying. Long alkyd 160x, is soya bean oil, yellowing resistance, high brush ability, excellent pigment wetting, high gloss retention, good adhesive and mechanical properties. Suggested in decorative enamel paints for internal and external applications. Solids% (+1-1)60 - solventwhite spirit, oil typesoya bean oil, oil length55 Color gardener - hellige3 max. 50% in white spirit , viscosity (gardener hotdt a 2)z3-z5, acid value (on solids)
Long alkyd 170x is a high viscosity resin. Gives good color, radiant gloss, excellent brush-ability, and rapid set and through drying. Long alkyd 170x, is based on soya bean oil, yellowing resistance, high brush ability, excellent pigment wetting, high gloss retention good adhesive and mechanical properties. Suggested in decorative enamel paints for internal and external applications. Solids% (+1-1) 70 , solventwhite spirit, oil typesoya bean oil, oil length62, color gardener - hellige 3 max. 50% in white spirit, viscosity (gardener hotdt a 25c)z2-z4 Acid value (on solids)
Medium alkyd 160x is a high viscosity resin. Gives good color, radiant gloss, excellent brush-ability, and rapid set and through drying. Medium alkyd 160x, is soya bean oil, yellowing resistance, fast drying and high performance for enamel and industrial paints. Excellent outdoor durability, high glossy finishing. It is also suggested for road marking and quick dry paints. Solids% (+1-1) 50, solventwhite spirit, oil type soya bean oil, oil length 48, color gardener - hellige 3 max, viscosity (gardener hotdt a 25c) z2-z4, acid value (on solids)
Based on cocunut oil fatty acids. Short alkyd 150p exhibit excellent hardness, yellowing resistance in nitrocellulose coating , it imparts good flexibility. Short alkyd 150p, is cofa resin, yellowing resistance, high durability, excellent pigment wetting, high gloss retention, dry fast and high reactive when cross linked with polyisocianates. It is also suggested to use with pu coating. Solids% (+1-1) 68, hydroxyl value 120-130, solvent xylene, oil typecofa, oil length38 Color gardener - hellige1 max, viscosity (gardener hotdt a 25c) z-z2, acid value (on solids)10-15
Type: Plain, Melamine, Paper, Aluminum, UV, PVC Wood: Poplar, Hardwood, Combi Glue: E1, E2, MR Size: 4x8, 6x12, 3x12, 6x8 Grade: Low, Medium, High Thickness: 2mm to 35mm Export standard pallet packing
Petro chemicals base oil , white spirit , bitumen , sulphur granules , urea , soda ash , furnace oil sulphur wdg , fertilizer products wollastonite , gypsum , limestone , bentonite food products : dates , pistachios , figs , almonds , saffron.
Pre mix plaster products cement plaster (machine used), variousdecorative plasters for buidings, gypsum plaster ffor internal plastering, tile fixing adhesives, tile joint fillers, swimming pool/ stone fixing adhesives, insulation plaster, aquostic plasters, gliterlite (glittering plaster for prestigious projects), complete building constructioon.
Bauxite, rock largely composed of a mixture of hydrous aluminium oxides. Bauxite is the principal ore of aluminium. bauxite. Related Topics: ore laterite gibbsite boehmite diaspore. Gibbsite (alumina trihydrate), boehmite, and diaspore (alumina monohydrates) are the main ore minerals. Bauxite is a high-aluminum-content rock. Bauxite - Cement Grade Specification Parameters Percentage AL O : Min 36% Fe O : 34% SiO : 6% LOI : 20% Moisture 8% Size 0 to 100 mm Origin Maharashtra, India.
Quartzite is a very hard rock composed predominantly of an interlocking mosaic of quartz crystals. The grainy, sandpaper-like surface is glassy in appearance. Minor amounts of former cementing materials, iron oxide, silica, carbonate and clay, often migrate during recrystallization, causing streaks and lenses to form within the quartzite. To be classified as a quartzite by the British Geological Survey, a metamorphic rock must contain at least 80% quartz by volume Parameters Percentage Silica (SiOâ??) 97.00% Alumina (AlO) 1.00% Moisture 1.00% Size 10 to 40 mm, 20 to 70 mm, 40 to 80 mm Origin Maharashtra, India.
Quartzite is a very hard rock composed predominantly of an interlocking mosaic of quartz crystals. The grainy, sandpaper-like surface is glassy in appearance. Minor amounts of former cementing materials, iron oxide, silica, carbonate and clay, often migrate during recrystallization, causing streaks and lenses to form within the quartzite. To be classified as a quartzite by the British Geological Survey, a metamorphic rock must contain at least 80% quartz by volume Parameters Percentage Silica (SiO) : 97.00% Alumina (Al - O) : 1.00% Moisture : 1.00% Size : 10 to 40 mm, 20 to 70 mm, 40 to 80 mm Origin ; Maharashtra, India.
