Sunday, 5 November 2017

ANDALUSITE[MINERAL]

Listing Description:
Andalusite is an aluminium nesosilicate mineral with the chemical formula Al2SiO5.
The variety chiastolite commonly contains dark inclusions of carbon or clay which form a checker-board pattern when shown in cross-section.
Detailed Description:

A clear variety first found in Andalusia, Spain can be cut into a gemstone.[5] Faceted andalusite stones give a play of red, green, and yellow colors that resembles a muted form of iridescence, although the colors are actually the result of unusually strong pleochroism.
It is associated with mica schist which increases alkali content in ultimate product and so it has not been exploited economically so far.

Occurrence

Andalusite is a common regional metamorphic mineral which forms under low pressure and low to high temperatures. The minerals kyanite and sillimanite are polymorphs of andalusite, each occurring under different temperature-pressure regimes and are therefore rarely found together in the same rock. Because of this the three minerals are a useful tool to help identify the pressure-temperature paths of the host rock in which they are found. An example rock includes hornfels.
It was first described and named after the type locality in the Ronda Massif, Málaga, Andalusia, Spain in 1789.

PRICE FOR ALUMINA CONTENT

$1.7/KG OR $0.77/IB

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CORUNDUM[MINERAL]

Listing dsrption

Corundum is a crystalline form of aluminium oxide (Al2O3) typically containing traces of irontitaniumvanadium and chromium.[2][3] It is a rock-forming mineral. It is a naturally transparent material, but can have different colors when impurities are present. Transparentspecimens are used as gems, called ruby if red and padparadscha if pink-orange. All other colors are called sapphire, e.g., green sapphire for a green specimen.

Detaild description
The name "corundum" is derived from the Tamil word Kurundam, which originates from the Sanskrit word Kuruvinda meaning ruby.[6]
Because of corundum's hardness (pure corundum is defined to have 9.0 on the Mohs scale), it can scratch almost every other mineral. It is commonly used as an abrasive on everything from sandpaper to large machines used in machining metals, plastics, and wood. Some emery is a mix of corundum and other substances, and the mix is less abrasive, with an average Mohs hardness of 8.0.
In addition to its hardness, corundum is unusual for its density of 4.02 g/cm3, which is very high for a transparent mineral composed of the low-atomic mass elements aluminium and oxygen.

PRICE FOR ALUMINA CONTENT

$1.7/KG OR $0.77/IB

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KYANITE(MINERAL)

LISTING DESCRIPTION
Kyanite, whose name derives from the Greek word kuanos sometimes referred to as "kyanos", meaning deep blue, is a typically blue silicate mineral, commonly found in aluminium-rich metamorphic pegmatites and/or sedimentary rock. Kyanite in metamorphic rocks generally indicates pressures higher than 4 kilobars.
DETAILED DESACRIPTION
Although potentially stable at lower pressure and low temperature, the activity of water is usually high enough under such conditions that it is replaced by hydrous aluminosilicates such as muscovite, pyrophyllite, or kaolinite. Kyanite is also known as disthene, rhaeticite and cyanite.
Kyanite is a member of the aluminosilicate series, which also includes the polymorph andalusite and the polymorph sillimanite. Kyanite is strongly anisotropic, in that its hardness varies depending on its crystallographic direction. In Kyanite, this anisotropism can be considered an identifying characteristic.
At temperatures above 1100 °C kyanite decomposes into mullite and vitreous silica via the following reaction: 3(Al2O3·SiO2) → 3Al2O3·2SiO2 + SiO2. This transformation results in an expansion.[4]

Uses of kyanite

Kyanite is used primarily in refractory and ceramic products, including porcelain plumbing fixtures and dishware. It is also used in electronics, electrical insulators and abrasives.
Kyanite has been used as a semiprecious gemstone, which may display cat's eye chatoyancy, though this use is limited by its anisotropism and perfect cleavage. Color varieties include recently discovered orange kyanite from Tanzania.[citation needed] The orange color is due to inclusion of small amounts of manganese (Mn3+) in the structure.[5]
Kyanite is one of the index minerals that are used to estimate the temperature, depth, and pressure at which a rock undergoes metamorphism.

Notes for identification

Kyanite's elongated, columnar crystals are usually a good first indication of the mineral, as well as its color (when the specimen is blue). Associated minerals are useful as well, especially the presence of the polymorphs of staurolite, which occur frequently with kyanite. However, the most useful characteristic in identifying kyanite is its anisotropism. If one suspects a specimen to be kyanite, verifying that it has two distinctly different hardnesses on perpendicular axes is a key to identification.

Occurrence

Kyanite occurs in gneiss, schist, pegmatite, and quartz veins resulting from moderate to high-pressure regional metamorphism of principally pelitic rocks. It occurs as detrital grains in sedimentary rocks. It occurs associated with staurolite, andalusite, sillimanite, talc, hornblende, gedrite, mullite and corundum.

PRICE FOR ALUMINA CONTENT

$1.7/KG OR $0.77/IB

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SILLIMENITE MINERAL

Sillimanite is an alumino-silicate mineral with the chemical formula Al2SiO5. Sillimanite is named after the American chemist Benjamin Silliman (1779-1864). It was first described in 1824 for an occurrence in Chester, Middlesex County, Connecticut, USA.
Detailed Description:

Packaing details:

Sillimanite is one of three alumino-silicate polymorphs, the other two being andalusite and kyanite. A common variety of sillimanite is known as fibrolite, so named because the mineral appears like a bunch of fibres twisted together when viewed in thin section or even by the naked eye. Both the fibrous and traditional forms of sillimanite are common in metamorphosed sedimentary rocks. It is an index mineral indicating high temperature but variable pressure. Example rocks include gneiss and granulite. It occurs with andalusite, kyanite, potassium feldspar, almandine, cordierite, biotite and quartz in schist, gneiss, hornfels and also rarely in pegmatites.
Sillimanite has been found in Brandywine Springs, New Castle County, Delaware, USA. It was named by the State Legislature in 1977 as the state mineral of Delaware by suggestion of the Delaware Mineralogical Society, Inc.
Natural sillimanite rocks cut into the required shape and size are used mainly in glass industries. Sillimanite is the best raw material for the manufacture of high alumina refractories or 55-60% alumina bricks. But its use on large scale is not possible due to its fine grading and high cost. Dumortierite and mullite are similar mineral species used in quality porcelain.


PRICE FOR ALUMINA CONTENT

$1.7/KG OR $0.77/IB

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Tuesday, 10 October 2017

BAUXITE

Bauxite is not a mineral. It is a rock formed from a laterite soil that has been severely leached of silica and other soluble materials in a wet tropical or subtropical climate. It is the primary ore of aluminum. Almost all of the aluminum that has ever been produced has been extracted from bauxite. 

Detailed description

Bauxite does not have a specific composition. It is a mixture of hydrous aluminum oxides, aluminum hydroxides, clay minerals and insoluble materials such as 
quartz, hematite, magnetite, siderite and goethite. The aluminum minerals in bauxite can include: gibbsite Al(OH)3, boehmite AlO(OH), and, diaspore, AlO(OH). 


Physical Properties of Bauxite

 

Bauxite is typically a soft (H:1-3), white to gray to reddish brown material with a pisolitic structure, earthy luster and a low specific gravity (SG: 2.0-2.5). These properties are useful for identifying bauxite; however, they have nothing to do with bauxite's value or usefulness. This is because bauxite is almost always processed into another material with physical properties that are distinctly different from bauxite. 

Physical Properties of Bauxite

Chemical Classification
Color
white, gray, sometimes stained yellow, orange red, pink, brown or yellow by iron or included iron minerals
Streak
usually white but iron stain can discolor
Luster
dull, earthy
Diaphaneity
opaque
Cleavage
none
Mohs Hardness
1 to 3
Specific Gravity
2 to 2.5
Diagnostic Properties
often exhibits pisolitic structure, color
Chemical Composition
variable but always rich in aluminum oxides and aluminum hydroxides
Crystal System
n/a
Uses
primary ore of aluminum, also used as an abrasive


Bauxite Used for Aluminum Production

 

Bauxite is the principal ore of aluminum. The first step in producing aluminum is to crush the bauxite and purify it using the Bayer Process. In the Bayer Process the bauxite is washed in a hot solution of sodium hydroxide which leaches aluminum from the bauxite. The aluminum is precipitated out of solution in the form of aluminum hydroxide, Al(OH)3. The aluminum hydroxide is then calcined to form alumina, Al2O3. 

Aluminum is smelted from the alumina using the Hall-Heroult Process. In the Hall-Heroult Process the alumina is dissolved in a molten bath of cryolite (Na3AlF6). Molten aluminum is removed from the solution by electrolysis. This process uses an enormous amount of electricity. Aluminum is usually produced where electricity costs are very low. 


Use of Bauxite as an Abrasive

 

Calcined alumina is a synthetic 
corundum, which is a very hard material (9 on the Mohs Hardness Scale). Calcined alumina is crushed, separated by size and used as an abrasive. Aluminum oxide sandpaper, polishing powders and polishing suspensions are made from calcined alumina. 

Sintered bauxite is often used as an sand-blasting abrasive. It is produced by crushing bauxite to a powder and then fusing it into spherical beads at very high temperature. These beads are very hard and very durable. The beads are then sorted by size for use in different types of sandblasting equipment and for different sandblasting applications. Their round shape reduces wear on the delivery equipment. 


Use of Bauxite as a Proppant

 

Sintered bauxite is also used as an oil field proppant. In drilling for 
oil and natural gas the reservoir rock is often fractured by pumping fluids into the well under very high pressures. The pressure builds up to very high levels that cause the reservoir rock to fracture. When fracturing occurs water and suspended particles, known as "proppants" rush into the fractures and push them open. When the pumps are turned off the fractures close trapping the proppant particles in the reservoir. If an adequate number of crush-resistant particles remain in the reservoir the fractures will be "propped" open allowing for a flow of oil or natural gas out of the rocks and into the well. This process is known as hydraulic fracturing. 

Powdered bauxite can be fused into tiny beads at very high temperatures. These beads have a very high crush resistance and that makes them suitable as a proppant. They can be produced in almost any size and in a range of specific gravity. The specific gravity of the beads and their size can be matched to the viscosity of the hydraulic fracturing fluid and to the size of fractures that are expected to develop in the rock. Manufactured proppants provide a wide selection of grain size and specific gravity compared to a natural proppant known as 
frac sand. 


Substitutes for Bauxite


 

World bauxite resources are adequate for decades of production at current rates. Other materials could be used instead of bauxite for alumina production. Clay minerals, alunite, anorthosite, power plant ash and 
oil shale could be used to produce alumina but at higher costs, using different processes. Silicon carbide could be used in place of bauxite-based abrasives. Synthetic mullite could be used in place of bauxite-based refractories. 

Price

$1.7/kg

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ALUMINUM INGOT

 Aluminium (UK: /ˌæljʉˈmɪniəm/  ( listenAL-yew-MIN-ee-əm) or aluminum (US: /əˈluːmɨnəm/  ( listenə-LOO-mi-nəm) is a silvery white member of the boron group of chemical elements. It has the symbol Al and its atomic number is 13. It is not soluble in water under normal circumstances. Aluminium is the most abundant metal in the Earth's crust, and the third most abundant element, after oxygen and silicon. It makes up about 8% by weight of the Earth's solid surface. Aluminium is too reactive chemically to occur in nature as a free metal. Instead, it is found combined in over 270 different minerals. The chief source of aluminium is bauxite ore.

Price
$1.8/KG


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ALUMINUM FLAKE POWDER

Aluminium (UK: /ˌæljʉˈmɪniəm/  ( listenAL-yew-MIN-ee-əm) or aluminum (US: /əˈluːmɨnəm/  ( listenə-LOO-mi-nəm) is a silvery white member of the boron group of chemical elements. It has the symbol Al and its atomic number is 13. It is not soluble in water under normal circumstances. Aluminium is the most abundant metal in the Earth's crust, and the third most abundant element, after oxygen and silicon. It makes up about 8% by weight of the Earth's solid surface. Aluminium is too reactive chemically to occur in nature as a free metal. Instead, it is found combined in over 270 different minerals. The chief source of aluminium is bauxite ore.
  
Detailed description:

Aluminium is remarkable for the metal's low density and for its ability to resist corrosion due to the phenomenon of passivation. Structural components made from aluminium and its alloys are vital to the aerospace industry and are very important in other areas of transportation and building. Its reactive nature makes it useful as a catalyst or additive in chemical mixtures, including ammonium nitrate explosives, to enhance blast power.

Price
$1.72/kg

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Monday, 9 October 2017

CASSITERITE[SnO2]

Listing description

Cassiterite is a tin oxide mineralSnO2. It is generally opaque, but it is translucent in thin crystals. Its luster and multiple crystal faces produce a desirable gem.
Detailed description
Cassiterite has been the chief tin ore throughout ancient history and remains the most important source of tin today.
Most sources of cassiterite today are found in alluvial or placer deposits containing the resistant weathered grains. The best sources of primary cassiterite are found in the tin mines of Bolivia, where it is found in hydrothermal veins. Rwanda has a nascent cassiterite mining industry. Fighting over cassiterite deposits (particularly in Walikale) is a major cause of the conflict waged in eastern parts of the Democratic Republic of the Congo.[6][7] This has led to cassiterite being considered a conflict mineral.
Cassiterite is a widespread minor constituent of igneous rocks. The Bolivian veins and the old exhausted workings of CornwallEngland, are concentrated in high temperature quartz veins and pegmatitesassociated with granitic intrusives. The veins commonly contain tourmalinetopazfluoriteapatitewolframitemolybdenite, and arsenopyrite. The mineral occurs extensively in Cornwall as surface deposits on Bodmin Moor, for example, where there are extensive traces of an hydraulic mining method known as streaming. The current major tin production comes from placer or alluvial deposits in MalaysiaThailandIndonesia, the Maakhir region of Somalia, and RussiaHydraulic mining methods are used to concentrate mined ore, a process which relies on the high specific gravity of the SnO2 ore, of about 7.0.

PRICE

$21.198/KG

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