The lateritic bauxites are found mostly in the countries of thetropics. They were formed bylateritization of varioussilicate rocks such asgranite,gneiss,basalt,syenite, andshale. In comparison with the iron-rich laterites, the formation of bauxites depends even more on intense weathering conditions in a location with very good drainage. This enables the dissolution of thekaolinite and the precipitation of thegibbsite. Zones with highest aluminium content are frequently located below aferruginous surface layer. Thealuminium hydroxide in the lateritic bauxite deposits is almost exclusively gibbsite.
In the case ofJamaica, recent analysis of the soils showed elevated levels ofcadmium, suggesting that the bauxite originates fromMiocenevolcanic ash deposits from episodes of significant volcanism in Central America.[7]
World bauxite production in 2005One of the world's largest bauxite mines inWeipa, in northernQueensland, Australia
Guinea is the largest producer of bauxite, followed byAustralia andChina.[8] Bauxite is usuallystrip mined because it is almost always found near the surface of theterrain, with little or nooverburden. Increasedaluminium recycling, which requires lesselectric power than producing aluminium from ores, may considerably extend the world's bauxite reserves.
Bauxite being loaded at Cabo Rojo,Dominican Republic, to be shipped elsewhere for processing; 2007Bauxite being digested by washing with a hot solution of sodium hydroxide at 175 °C (347 °F) under pressure at National Aluminium Company, Nalconagar, India.
As of 2010[update], approximately 70% to 80% of the world's dry bauxite production is processed first intoalumina and then into aluminium byelectrolysis.[9] Bauxite rocks are typically classified according to their intended commercial application: metallurgical, abrasive, cement, chemical, and refractory.[10][11]
Bauxite ore is usually heated in a pressure vessel along with asodium hydroxide solution at a temperature of 150 to 200 °C (300 to 390 °F). At these temperatures, thealuminium is dissolved assodium aluminate (theBayer process). The aluminium compounds in the bauxite may be present asgibbsite (Al(OH)3),boehmite (AlOOH) ordiaspore (AlOOH); the different forms of the aluminium component will dictate the extraction conditions. The undissolved waste,bauxite tailings, after the aluminium compounds are extracted containsiron oxides,silica,calcia,titania and some un-reactedalumina. After separation of the residue by filtering, pure gibbsite is precipitated when the liquid is cooled, and then seeded with fine-grainedaluminium hydroxide. The gibbsite is usually converted intoaluminium oxide, Al2O3, by heating in rotary kilns or fluid flash calciners to a temperature in excess of 1,000 °C (1,830 °F). This aluminium oxide is dissolved at a temperature of about 960 °C (1,760 °F) in moltencryolite. Next, this molten substance can yield metallic aluminium by passing anelectric current through it in the process of electrolysis, which is called theHall–Héroult process, named after its American and French discoverers.
Prior to the invention of this process, and prior to theDeville process, aluminium ore was refined by heating ore along with elementalsodium orpotassium in avacuum. The method was complicated and consumed materials that were themselves expensive at that time. This made early elemental aluminium more expensive thangold.[12]
As abulk cargo, bauxite is a Group A cargo that may liquefy if excessively moist.[13]Liquefaction and thefree surface effect can cause the cargo to shift rapidly inside the hold and make the ship unstable, potentially sinking the ship. One vessel suspected to have been sunk in this way was theMSBulk Jupiter in 2015.[14] One method which can demonstrate this effect is the "can test", in which a sample of the material is placed in a cylindrical can and struck against a surface many times.[15] If a moistslurry forms in the can, then there is a likelihood for the cargo to liquefy; although conversely, even if the sample remains dry it does not conclusively prove that it will remain that way, or that it is safe for loading.
Bauxite is the main source of the rare metalgallium.[16]
During the processing of bauxite toalumina in theBayer process, gallium accumulates in thesodium hydroxide liquor. From this it can be extracted by a variety of methods. The most recent is the use ofion-exchange resin.[17] Achievable extraction efficiencies critically depend on the original concentration in the feed bauxite. At a typical feed concentration of 50 ppm, about 15 percent of the contained gallium is extractable.[17] The remainder reports to thered mud andaluminium hydroxide streams.[18]
Bauxite is also a potential source forvanadium.[19]
The social and environmental impacts of bauxite extraction are well documented. Most of the world's bauxite deposits can be found within 1 to 20 metres (3 ft 3 in to 65 ft 7 in) of the earths surface.[20][21]Strip mining is the most common technique used for extracting shallow bauxite.[21] This process involves removing the vegetation, top soil, andoverburden to expose the bauxite ore.[21] The overlying soil is typically stockpiled in order torehabilitate the mine once operations have finished.[21] During the strip mining process, the biodiversity and habitat once present in the area is completely lost and the hydrological and soil characteristics in the region are permanently altered.[21] Other environmental impacts of bauxite mining includesoil degradation,air pollution, andwater pollution.[20]
Red mud is a highlyalkaline sludge, with a high pH around 13, that is a byproduct of theBayer process.[22] It contains several compounds such assodium aluminoscilicate,calcium titanate, monohydrate aluminium, and trihydrate aluminium that do not break down in nature. When improperly stored, red mud can contaminate soil and water, which can result inlocal extinction of all life. Red mud was responsible for killing all life in theMarcal River in Hungary after a spill occurred in 2010. When red mud dries, it turns into dust that can cause lung disease, cancer and birth defects.[22]
In the tropical regions of Asia, central Africa, South America and northern Australia, there has been an increase of bauxite mines on traditional and indigenous lands.[21] This has resulted in a number of negative social impacts on local and indigenous peoples.[23] In theBoké Region of Guinea, there has been a significant increase in bauxite mining pressure on the local population. This has resulted in potable water issues, air pollution, food contamination, and landexpropriation disputes due to improper compensation.[23]
Bauxite mining has led to protests, civil unrest, and violent conflicts in Guinea, Ghana, Vietnam, and India.[22]
Guinea has a long history of mining related conflicts between communities and mining companies.[citation needed] Between 2015 and 2018, new bauxite mining operations in theBoké Region of Guinea have caused in 35 conflicts which include movements of revolts and road blockades. These conflicts have resulted in the loss of human life, the destruction of heavy machinery, and damage to government buildings.[citation needed]
TheAtewa range in Ghana, classified as an ecologically important forest reserve with an area of 17,400 hectares (43,000 acres), has been is a recent site of conflict and controversy surrounding bauxite mining.[24] The forest reserve is one of the only two upland evergreen forests in Ghana, and makes up a significant portion of the remaining 20% of forested habitat left in Ghana. The Atewa range falls under the jurisdiction ofAkyem Abuakwa Traditional Area and is overseen by the king known as Okyenhene.[24] In 2013, an NGO called A Rocha Ghana held a summit with the forestry and water resource commission, the minister of lands, the minister of the environment, and other important stakeholders. They came to the conclusion that no future government should mine bauxite in the region because the reserve is environmentally and culturally significant.[24] In 2016, the government along with NGO's began the process of upgrading the reserved to a national park. However, that year an election took place, and before it became official, the newly elected National Patriotic Party (NPP) rejected the plan.[24] In 2017, the government of Ghana signed aMemorandum of Understanding with China to develop new bauxite mining infrastructure in Ghana. Although there was no official plan to mine the Atewa Forest Reserve, tensions between local communities, NGO and the government began to rise. In 2019, tensions began to reach a peak when the government presented theGhana Integrated Bauxite and Aluminium Development Authority Act that would create the legal framework required to develop and establish an integrated bauxite industry.[24] In may of that year, the government began drilling deep holes in the reserve. These actions sparked several protests, including a 95-kilometre (59 mi) march from the reserve to the presidential palace, an informational billboard campaign led by A Rocha Ghana, and a youth march.[24] In 2020, A Rocha Ghana also sued the government over the drilling in the reserve after they failed to provide a statement explaining their actions.[24]
In early 2009, the Vietnamese Government proposed a plan to mine remote regions of the central highlands.[22] This proposal was highly controversial and sparked a nationwide debate and the most significant domestic conflict since theVietnam War. Government scientists, journalists, religious leaders, retired high level state officials, andGeneral Võ Nguyên Giáp, the military leader of anti-colonial revolution, were among the many people across Vietnamese society who opposed the governments plans.[22] In an attempt to stop the spread of information across the globe, the government banned domestic reporters from reporting on bauxite mining. However, reporters turned to Vietnamese language websites and blogs where the reporting and discussion continued. On April 12, 2009, several well-respected Vietnamese scholars started a petition against the mining of bauxite that was signed by 135 accomplished and well known "Intellectuals".[22] This petition helped unite the scattered anti-bauxite movement into a unified opposition against the state. These acts of governmental defiance were met with repressive state actions. Many domestic online reporters were arrested, and legislative action was taken to repress scientific research.[22]
Most of India's bauxite ore reserves, which are among the top ten largest in the world, are located on tribal land.[25] These tribal lands are densely populated and home to over 100 million Indigenous Indian peoples. The mountain summits located on these lands act as a source of water and greatly contribute to the regions fertility.[25] The Indian bauxite industry is interested in developing this land for aluminium production, which poses great risk to the terrestrial and aquatic ecosystems. Historically, the Indigenous peoples living on these lands have shown resistance to development, and oppose any new bauxite mining projects in the area. This has led to violent conflicts between Indigenous communities and police.[25] On December 16, 2000, police killed three Indigenous protestors and wounded over a dozen more during a protest over a bauxite project in theRayagada district ofOdisha.[25]
In 1847, in the cumulative index of volume 3 of his series,Traité de minéralogie, French mineralogistArmand Dufrénoy listed the hydrated alumina from Les Beaux as "beauxite". (See: A. Dufrénoy,Traité de minéralogie, volume 3 (Paris, France: Carilian-Goeury et Vor Dalmont, 1847),p. 799.)
^Muhs, Daniel R.; Budahn, James R. (2009). "Geochemical evidence for African dust and volcanic ash inputs to terra rossa soils on carbonate reef terraces, northern Jamaica, West Indies".Quaternary International.196 (1–2): 15.Bibcode:2009QuInt.196...13M.doi:10.1016/j.quaint.2007.10.026.
^Michael Quinion (January 23, 2006)."Aluminium versus aluminum". Worldwidewords.org.Archived from the original on October 23, 2019. RetrievedDecember 19, 2011.
^Cusack, Patricia B.; Courtney, Ronan; Healy, Mark G.; O'Donoghue, Lisa; Ujaczki, Eva (2019). "An evaluation of the general composition and critical raw material content of bauxite residue in a storage area over a twelve-year period".Journal of Cleaner Production.208 (20): 393.Bibcode:2019JCPro.208..393C.doi:10.1016/j.jclepro.2018.10.083.hdl:10379/14624 – via Elsevier Science Direct.
Bárdossy, G. (1982):Karst Bauxites: Bauxite deposits on carbonate rocks. Elsevier Sci. Publ. 441 p.
Bárdossy, G. and Aleva, G.J.J. (1990):Lateritic Bauxites. Developments in Economic Geology 27, Elsevier Sci. Publ. 624 p.ISBN0-444-98811-4
Grant, C.; Lalor, G. and Vutchkov, M. (2005)Comparison of bauxites from Jamaica, the Dominican Republic and Suriname. Journal of Radioanalytical and Nuclear Chemistry p. 385–388 Vol.266, No.3
Hanilçi, N. (2013).Geological and geochemical evolution of the Bolkardaği bauxite deposits, Karaman, Turkey: Transformation from shale to bauxite. Journal of Geochemical Exploration