Bauxite Information
Bauxite is an aluminium ore and is the main source of aluminium. This form of rock consists mostly of the minerals gibbsite Al(OH)3, boehmite γ-AlO(OH), and diaspore α-AlO(OH), in a mixture with the two iron oxides goethite and hematite, the clay mineral kaolinite, and small amounts of anatase TiO2. Bauxite was named after the village Les Baux in southern France, where it was first recognised as containing aluminium and named by the French geologist Pierre Berthier in 1821.
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Bauxite formation
Lateritic bauxites (silicate bauxites) are distinguished from karst bauxite ores (carbonate bauxites). The early discovered carbonate bauxites occur predominantly in Europe and Jamaica above carbonate rocks (limestone and dolomite), where they were formed by lateritic weathering and residual accumulation of intercalated clays or by clay dissolution residues of the limestone.
The lateritic bauxites are found mostly in the countries of the tropics.They were formed by lateritization (see laterite) of various silicate rocks such as granite, gneiss, basalt, syenite, and shale. In comparison with the iron-rich laterites, the formation of bauxites demands even more on intense weathering conditions in a location with very good drainage. This enables the dissolution of the kaolinite and the precipitation of the gibbsite. Zones with highest aluminium content are frequently located below a ferruginous surface layer. The aluminium hydroxide in the lateritic bauxite deposits is almost exclusively gibbsite.
Production trends
Bauxite output in 2005In 2007, Australia was one of the top producers of bauxite with almost one-third of the world's production, followed by China, Brazil, Guinea, and India. Although aluminium demand is rapidly increasing, known reserves of its bauxite ore are sufficient to meet the worldwide demands for aluminium for many centuries. Increased aluminium recycling, which has the advantage of lowering the cost in electric power in producing aluminium, will considerably extend the world's bauxite reserves.
| Country | Mine production | Reserves | Reserve base | |
|---|---|---|---|---|
| 2007 | 2008 | |||
| Guinea | 18,000 | 18,000 | 7,400,000 | 8,600,000 |
| Australia | 62,400 | 63,000 | 5,800,000 | 7,900,000 |
| Vietnam | 30 | 30 | 2,100,000 | 5,400,000 |
| Jamaica | 14,600 | 15,000 | 2,000,000 | 2,500,000 |
| Brazil | 24,800 | 25,000 | 1,900,000 | 2,500,000 |
| Guyana | 1,600 | 1,600 | 700,000 | 900,000 |
| India | 19,200 | 20,000 | 770,000 | 1,400,000 |
| China | 30,000 | 32,000 | 700,000 | 2,300,000 |
| Greece | 2,220 | 2,200 | 600,000 | 650,000 |
| Iran | — | 500[2] | — | — |
| Suriname | 4,900 | 4,500 | 580,000 | 600,000 |
| Kazakhstan | 4,800 | 4,800 | 360,000 | 450,000 |
| Venezuela | 5,900 | 5,900 | 320,000 | 350,000 |
| Russia | 6,400 | 6,400 | 200,000 | 250,000 |
| United States | NA | NA | 20,000 | 40,000 |
| Other countries | 7,150 | 6,800 | 3,200,000 | 3,800,000 |
| World total (rounded) | 202,000 | 205,000 | 27,000,000 | 38,000,000 |
In November 2010, Nguyen Tan Dung, the prime minister of Vietnam, announced that Vietnam's bauxite reserves might total 11000Mt; this would be the largest in the world.[3]
Processing
Bauxite being loaded at Cabo Rojo, Dominican Republic, to be shipped elsewhere for processing; 2007Bauxite is usually strip mined because it is almost always found near the surface of the terrain, with little or no overburden. Approximately 75% to 85% of the world's bauxite production is processed first into alumina, and then into aluminium by electrolysis. Bauxite rocks are typically classified according to their intended commercial application: metallurgical, abrasive, cement, chemical, and refractory.
Usually, bauxite ore is heated in a pressure vessel along with a sodium hydroxide solution at a temperature of 150 to 200 °C. At these temperatures, the aluminium is dissolved as an aluminate (the Bayer process). After separation of ferruginous residue (red mud) by filtering, pure gibbsite is precipitated when the liquid is cooled, and then seeded with fine-grained aluminium hydroxide. The gibbsite is usually converted into aluminium oxide, Al2O3, by heating. This mineral becomes molten at a temperature of about 1000 °C, when the mineral cryolite is added as a flux. Next, this molten substance can yield metallic aluminium by passing an electric current through it in the process of electrolysis, which is called the Hall–Héroult process after its American and French discoverers in 1886.
Prior to the Hall–Héroult process, elemental aluminium was made by heating ore along with elemental sodium or potassium in a vacuum. The method was complicated and consumed materials that were themselves expensive at that time. This made early elemental aluminium more expensive than gold.[4]
See also
| Book: Aluminium | |
| Wikipedia books are collections of articles that can be downloaded or ordered in print. | |
Notes
- ^ U.S. Geological Survey, Mineral Commodity Summaries, January 2009
- ^ http://www.bgs.ac.uk/mineralsuk/commodity/world/home.html
- ^ "Mining Journal - Vietnam’s bauxite reserves may total 11 billion tonnes". http://www.mining-journal.com/exploration--and--development/vietnams-bauxite-reserves-may-total-11-billion-tonnes. Retrieved 2010-11-28.
- ^ http://www.worldwidewords.org/articles/aluminium.htm Aluminium versus aluminum Author: Michael Quinion, 1996–2011
References
- Bardossy, G. (1982): Karst Bauxites. Bauxite deposits on carbonate rocks. Elsevier Sci. Publ. 441 p.
- Bardossy, G. and Aleva, G.J.J. (1990): Lateritic Bauxites. Developments in Economic Geology 27, Elsevier Sci. Publ. 624 p. ISBN 0-444-988
External links
| Wikimedia Commons has media related to: Bauxite |
- USGS Minerals Information: Bauxite
- Mineral Information Institute
- "Bauxite". New International Encyclopedia. 1905.
- "Bauxite". Encyclopedia Americana. 1920.
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