An extremely hard mineral, aluminum oxide, Al2O3, sometimes containing iron, magnesia, or silica, that occurs in gem varieties such as ruby and sapphire and in a common black, brown, or blue form used chiefly in abrasives.
[Tamil kuruntam.]
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An extremely hard mineral, aluminum oxide, Al2O3, sometimes containing iron, magnesia, or silica, that occurs in gem varieties such as ruby and sapphire and in a common black, brown, or blue form used chiefly in abrasives.
[Tamil kuruntam.]
A mineral with the ideal composition Al2O3. It is one of a large group of isostructural compounds including hematite (Fe2O3) and ilmenite (FeTiO3), all of which crystallize in the hexagonal crystal system, trigonal subsystem. Corundum has the high hardness of 9 on Mohs scale and is therefore commonly used as an abrasive, either alone or in the form of the rock called emery, which consists principally of the minerals corundum and magnetite. Crystals occurring in igneous rocks usually have an elongated barrellike shape, while crystals from metamorphic rocks are generally tabular. The specific gravity is approximately 3.98. See also Hematite; Ilmenite.
Pure corundum is transparent and colorless, but most specimens contain some transition elements substituting for aluminum, resulting in the presence of color. Substitution of chromium results in a deep red color; such red corundum is known as ruby. The term “sapphire” is used in both a restricted sense for the “cornflower blue” variety containing iron and titanium, and in a general sense for gem-quality corundums of any color other than red. Star ruby and star sapphire contain tiny needies of the mineral rutile. See also Ruby; Sapphire.
Corundum occurs as a rock-forming mineral in both metamorphic and igneous rocks, but only in those which are relatively poor in silica, and never in association with free silica. Igneous rocks which most commonly contain corundum include syenites, nepheline syenites, and syenite pegmatites. Both contact and regionally metamorphosed silica-poor rocks may contain corundum. See also
For more information on corundum, visit Britannica.com.
A hard, abrasive mineral, principally aluminum oxide, applied to a surface to make it non-slippery; for example, on the walking surface of a ramp.
| Corundum | |
|---|---|
| General | |
| Category | Mineral |
| Chemical formula | aluminium oxide, Al2O3 |
| Identification | |
| Color | Brown to grey, less often red, blue, white, yellow. |
| Crystal habit | Steep bipyramidal, tabular, prismatic, rhombohedral crystals, massive or granular |
| Crystal system | Trigonal Hexagonal Scalenohedral bar32/m |
| Twinning | Polysynthetic twinning common |
| Cleavage | None - parting in 3 directions |
| Fracture | Conchoidal to uneven |
| Mohs Scale hardness | 9 |
| Luster | Adamantine to vitreous |
| Refractive index | nω=1.768 - 1.772 nε=1.760 - 1.763, Biref 0.009 |
| Pleochroism | None |
| Streak | White |
| Specific gravity | 3.95-4.1 |
| Fusibility | Infusible |
| Solubility | Insoluble |
| Major varieties | |
| Sapphire | Any color except red |
| Ruby | Red |
| Emery | Granular |
Corundum (from Tamil kurundam) is a crystalline form of aluminium oxide and one of the rock-forming minerals. It is naturally clear, but can have different colors when impurities are present. Transparent specimens are used as gems, called ruby if red, while all other colors are called sapphire. In addition to its hardness, corundum is unusual for its high density of 4.02 g/cm³ which is very high for a transparent mineral composed of the low atomic mass elements aluminium and oxygen.
Due to corundum's hardness (pure corundum is defined to have 9.0 Mohs), it is commonly used as an abrasive in machining, from huge machines to sandpaper. Some emery is a mix of corundum and other substances, and the mix is less abrasive, with a lower average Mohs hardness near 8.0.
Corundum occurs as a mineral in mica schist, gneiss, and some marbles in metamorphic terranes. It also occurs in low silica igneous syenite and nepheline syenite intrusives. Other occurrences are as masses adjacent to ultramafic intrusives, associated with lamprophyre dikes and as large crystals in pegmatites. Because of its hardness and resistance to weathering, it commonly occurs as a detrital mineral in stream and beach sands.
Corundum for abrasives is mined in Zimbabwe, Russia, and India. Historically it was mined from deposits associated with dunites in North Carolina and from a nepheline syenite in Craigmont, Ontario. Emery grade corundum is found on the Greek island of Naxos and near Peekskill, New York. Abrasive corundum is synthetically manufactured from bauxite.
In 1837 Gaudin made the first synthetic rubies by fusing alumina at a high temperature with a little chromium as a pigment. In 1847 Edelman made white sapphire by fusing alumina in boric acid. In 1877 Frenic and Freil made crystal corundum from which small stones could be cut. Frimy and Auguste Verneuil manufactured artificial ruby by fusing BaF2 and Al2O3 with a little Chromium at red heat. In 1903 Verneuil announced he could produce synthetic rubies on a commercial scale using this flame fusion process. [1]
The Verneuil process actually allows the production of large quantities of
sapphire, rubies, and other corundum gems. It is also possible to
grow gem-quality synthetic corundum by flux-growth and hydrothermal synthesis.
Because of the simplicity of the methods involved in corundum synthesis, large quantities of these crystals became available on
the market causing a significant reduction of price in recent years. Apart from ornamental use, synthetic corundum is also used
to produce mechanical parts (tubes, rods, bearings, and other machined parts), watch crystals, and
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