Cryolite: Difference between revisions
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| references = <ref>{{cite book |last1=Gaines |first1=Richard V. |last2=Skinner |first2=H. Catherine W. |last3=Foord |first3=Eugene E. |last4=Mason |first4=Brian |last5=Rosensweig |first5=Abraham |title=Dana's new mineralogy : the system of mineralogy of James Dwight Dana and Edward Salisbury Dana. |date=1997 |publisher=Wiley |location=New York |isbn=978-0-471-19310-4 |edition=8th, entirely rewritten and greatly enl.}}</ref><ref name = mindat>{{cite web |url=http://www.mindat.org/min-1161.html |title=Cryolite: Cryolite mineral information and data |website=Mindat.org |date=3 October 2010 |access-date=25 October 2020}}</ref><ref name = webmineral>{{cite web |url=http://www.webmineral.com/data/Cryolite.shtml |title=Cryolite Mineral Data |website=Webmineral.com. |access-date=25 October 2010}}</ref><ref name = HOM>{{cite web |url=http://rruff.geo.arizona.edu/doclib/hom/cryolite.pdf |title=Cryolite |website=Handbook of Mineralogy |access-date=25 October 2010}}</ref><ref name=Hurlbut>{{cite book |last1=Klein |first1=Cornelis |last2=Hurlbut |first2=Cornelius S. |title=Manual of mineralogy : (after James D. Dana) |date=1985 |publisher=Wiley |location=New York |isbn=0-471-80580-7 |edition=20th}}</ref> | | references = <ref>{{cite book |last1=Gaines |first1=Richard V. |last2=Skinner |first2=H. Catherine W. |last3=Foord |first3=Eugene E. |last4=Mason |first4=Brian |last5=Rosensweig |first5=Abraham |title=Dana's new mineralogy : the system of mineralogy of James Dwight Dana and Edward Salisbury Dana. |date=1997 |publisher=Wiley |location=New York |isbn=978-0-471-19310-4 |edition=8th, entirely rewritten and greatly enl.}}</ref><ref name = mindat>{{cite web |url=http://www.mindat.org/min-1161.html |title=Cryolite: Cryolite mineral information and data |website=Mindat.org |date=3 October 2010 |access-date=25 October 2020}}</ref><ref name = webmineral>{{cite web |url=http://www.webmineral.com/data/Cryolite.shtml |title=Cryolite Mineral Data |website=Webmineral.com. |access-date=25 October 2010}}</ref><ref name = HOM>{{cite web |url=http://rruff.geo.arizona.edu/doclib/hom/cryolite.pdf |title=Cryolite |website=Handbook of Mineralogy |access-date=25 October 2010}}</ref><ref name=Hurlbut>{{cite book |last1=Klein |first1=Cornelis |last2=Hurlbut |first2=Cornelius S. |title=Manual of mineralogy : (after James D. Dana) |date=1985 |publisher=Wiley |location=New York |isbn=0-471-80580-7 |edition=20th}}</ref> | ||
}} | }} | ||
'''Cryolite''' ([[sodium|Na]]<sub>3</sub>[[aluminium|Al]][[fluorine|F]]<sub>6</sub>, [[sodium hexafluoroaluminate]]) is a rare [[mineral]] identified with the once-large deposit at [[Ivittuut]] on the | '''Cryolite''' ([[sodium|Na]]<sub>3</sub>[[aluminium|Al]][[fluorine|F]]<sub>6</sub>, [[sodium hexafluoroaluminate]]) is a rare [[mineral]] identified with the once-large deposit at [[Ivittuut]] on the southwest coast of [[Greenland]], mined commercially until 1987.<ref name="Eclipse Metals buys cryolite mine in Greenland">{{cite web |title=Eclipse Metals buys unique historical cryolite mine in Greenland |url=https://im-mining.com/2021/01/15/eclipse-metals-buys-unique-historical-cryolite-mine-greenland/ |website=im-mining.com |date=15 January 2021 |access-date=11 July 2022}}</ref> | ||
It is used in the reduction ("[[smelting]]") of aluminium, in pest control, and as a dye. | It is used in the reduction ("[[smelting]]") of [[aluminium]], in pest control, and as a dye. | ||
==History== | ==History== | ||
| Line 52: | Line 52: | ||
The [[Pennsylvania Salt Manufacturing Company]] used large amounts of cryolite to make [[caustic soda]] and [[fluorine]] compounds, including [[hydrofluoric acid]] at its [[Natrona, Pennsylvania]], works, and at its integrated chemical plant in [[Cornwells Heights, Pennsylvania]], during the 19th and 20th centuries.{{Citation needed|date=January 2021}} | The [[Pennsylvania Salt Manufacturing Company]] used large amounts of cryolite to make [[caustic soda]] and [[fluorine]] compounds, including [[hydrofluoric acid]] at its [[Natrona, Pennsylvania]], works, and at its integrated chemical plant in [[Cornwells Heights, Pennsylvania]], during the 19th and 20th centuries.{{Citation needed|date=January 2021}} | ||
It was historically used as an ore of aluminium and later in the electrolytic processing of the [[aluminium]]-rich oxide [[ore]] [[bauxite]] (itself a combination of [[aluminium oxide]] minerals such as [[gibbsite]], [[boehmite]] and [[diaspore]]). The difficulty of separating aluminium from oxygen in the oxide ores was overcome by the use of cryolite as a [[flux (metallurgy)#Smelting|flux]] to dissolve the oxide mineral(s). | It was historically used as an ore of aluminium and later in the electrolytic processing of the [[aluminium]]-rich oxide [[ore]] [[bauxite]] (itself a combination of [[aluminium oxide]] minerals such as [[gibbsite]], [[boehmite]] and [[diaspore]]). The difficulty of separating aluminium from oxygen in the oxide ores was overcome by the use of cryolite as a [[flux (metallurgy)#Smelting|flux]] to dissolve the oxide mineral(s). | ||
Pure cryolite itself melts at 1012 °C (1285 [[Kelvin temperature scale|K]]), and it can dissolve the aluminium oxides sufficiently well to allow easy extraction of the aluminium by [[electrolysis]]. Substantial energy is still needed for both heating the materials and the electrolysis, but it is much more energy-efficient than melting the oxides themselves. As natural cryolite is now too rare to be used for this purpose, synthetic sodium aluminium fluoride is produced from the common mineral [[fluorite]].{{Citation needed|date=January 2021}} | |||
In 1987 the main mining in Ivittuut was closed. According to economist | In 1940 before entering [[World War II]], the United States became involved with protecting the world's largest cryolite mine in Ivittuut, Greenland from falling into Nazi Germany's control.<ref>{{Cite web |last=Magazine |first=Smithsonian |title=How This Abandoned Mining Town in Greenland Helped Win World War II |url=https://www.smithsonianmag.com/travel/how-abandoned-mining-town-greenland-helped-win-world-war-ii-180973835/ |access-date=2023-03-26 |website=Smithsonian Magazine |language=en}}</ref> | ||
In 1987 the main mining in Ivittuut was closed. According to [[economist]] Arindam Banerjee, exploitation of cryolite in Greenland contributed nearly 54 billion euros to Danish economy,<ref>{{Cite journal |last=Sandré |first=Tanguy |date=3 March 2025 |title=Cryolite: le Danemark censure son histoire coloniale |url=https://blogs.mediapart.fr/tanguy-sandre/blog/030325/cryolite-le-danemark-censure-son-histoire-coloniale |journal=Mediapart}}</ref> though this claim has been strongly disputed.<ref>{{Cite web |last=Kajkus |first=Ines |last2=Lindberg |first2=Kristian |date=2025-02-10 |title=Vrede kilder beskylder DR for at manipulere seerne i sprængfarlig dokumentar: »Grebet ud af den blå luft« |url=https://www.berlingske.dk/kultur/vrede-kilder-beskylder-dr-for-at-manipulere-seerne-i-spraengfarlig |access-date=2025-04-01 |website=Berlingske.dk |language=da}}</ref> | |||
==Source locations== | ==Source locations== | ||
[[Image:Cryolite mine ivgtut greenland.jpg|thumb|left|The cryolite mine at [[Ivigtut]], [[Greenland]], summer 1940]] | [[Image:Cryolite mine ivgtut greenland.jpg|thumb|left|The cryolite mine at [[Ivigtut]], [[Greenland]], summer 1940]] | ||
Besides [[Ivittuut]], on the | Besides [[Ivittuut]], on the southwest coast of [[Greenland]] where cryolite was once found in commercial quantities, small deposits of cryolite have also been reported in some areas of [[Spain]], at the foot of [[Pikes Peak]] in [[Colorado]], Francon Quarry near [[Montreal]] in [[Quebec]], [[Canada]] and also in Miask, [[Russia]].<ref>{{Cite web|title=Cryolite (Sodium Aluminum Fluoride)|url=http://www.galleries.com/Cryolite|access-date=2020-10-07|website=www.galleries.com}}</ref><ref>{{Cite web|title=Cryolite {{!}} mineral|url=https://www.britannica.com/science/cryolite|access-date=2020-10-07|website=Encyclopedia Britannica|language=en}}</ref> | ||
==Uses== | ==Uses== | ||
Latest revision as of 21:47, 16 July 2025
Template:Short description Template:Infobox mineral Cryolite (Na3AlF6, sodium hexafluoroaluminate) is a rare mineral identified with the once-large deposit at Ivittuut on the southwest coast of Greenland, mined commercially until 1987.[1]
It is used in the reduction ("smelting") of aluminium, in pest control, and as a dye.
History
Cryolite was first described in 1798 by Danish veterinarian and physician Template:Ill (1740–1801),[2][3] from rock samples obtained from local Inuit who used the mineral for washing their hides; the actual source of the ore was later discovered in 1806 by the explorer Karl Ludwig Giesecke.[4][5] who found the deposit at Ivigtut (old spelling) and nearby Arsuk Fjord, Southwest Greenland, where it was extracted by Øresund Chemical Industries.[6] The name is derived from the Greek words Script error: No such module "Lang". (Template:Langx), and Script error: No such module "Lang". (Template:Langx).[7]
The Pennsylvania Salt Manufacturing Company used large amounts of cryolite to make caustic soda and fluorine compounds, including hydrofluoric acid at its Natrona, Pennsylvania, works, and at its integrated chemical plant in Cornwells Heights, Pennsylvania, during the 19th and 20th centuries.Script error: No such module "Unsubst".
It was historically used as an ore of aluminium and later in the electrolytic processing of the aluminium-rich oxide ore bauxite (itself a combination of aluminium oxide minerals such as gibbsite, boehmite and diaspore). The difficulty of separating aluminium from oxygen in the oxide ores was overcome by the use of cryolite as a flux to dissolve the oxide mineral(s).
Pure cryolite itself melts at 1012 °C (1285 K), and it can dissolve the aluminium oxides sufficiently well to allow easy extraction of the aluminium by electrolysis. Substantial energy is still needed for both heating the materials and the electrolysis, but it is much more energy-efficient than melting the oxides themselves. As natural cryolite is now too rare to be used for this purpose, synthetic sodium aluminium fluoride is produced from the common mineral fluorite.Script error: No such module "Unsubst".
In 1940 before entering World War II, the United States became involved with protecting the world's largest cryolite mine in Ivittuut, Greenland from falling into Nazi Germany's control.[8]
In 1987 the main mining in Ivittuut was closed. According to economist Arindam Banerjee, exploitation of cryolite in Greenland contributed nearly 54 billion euros to Danish economy,[9] though this claim has been strongly disputed.[10]
Source locations
Besides Ivittuut, on the southwest coast of Greenland where cryolite was once found in commercial quantities, small deposits of cryolite have also been reported in some areas of Spain, at the foot of Pikes Peak in Colorado, Francon Quarry near Montreal in Quebec, Canada and also in Miask, Russia.[11][12]
Uses
Molten cryolite is used as a solvent for aluminium oxide (Al2O3) in the Hall–Héroult process, used in the refining of aluminium. It decreases the melting point of aluminium oxide from 2000–2500 °C to 900–1000 °C, and increases its conductivity[13] thus making the extraction of aluminium more economical.[14]
Cryolite is used as an insecticide and a pesticide.[15] It is also used to give fireworks a yellow color.[16] It is used in glass manufacturing as a "powerful opaliser."[17]
Physical properties
Cryolite occurs as glassy, colorless, white-reddish to gray-black prismatic monoclinic crystals. It has a Mohs hardness of 2.5 to 3 and a specific gravity of about 2.95 to 3.0. It is translucent to transparent with a very low refractive index of about 1.34, which is very close to that of water; thus if immersed in water, cryolite becomes essentially invisible.[18]
References
- Phase transitions and volumetric properties of cryolite, Na3AlF6: Differential thermal analysis to 100 MPa; American Mineralogist; January 2006; v. 91; no. 1; p. 97-103; Script error: No such module "doi".
- ↑ Script error: No such module "citation/CS1".
- ↑ Script error: No such module "Citation/CS1". (At the ordinary session of the [Danish] Royal Society of Science on February 1st of this year, Prof. Abildgaard presented a report about Norwegian titanium ores and about the analysis of them undertaken by him. He also communicated a notice of an especially white, spar-like mineral that was brought several years ago from Greenland to Denmark. According to an investigation performed on it, it consists of alumina and hydrofluoric acid. A compound of which no similar example in the mineral realm has yet been found. It received the name "cryolite" because under a blowpipe, it melts like frozen brine.)
- ↑ Script error: No such module "Citation/CS1". (He has named this Greenlandic stone cryolite or ice stone on account of its appearance, and because it melts so easily under a blowpipe.)
- ↑ Script error: No such module "citation/CS1".
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- ↑ The Brazilian statesman and scientist José Bonifácio de Andrada e Silva also analyzed cryolite:
- Script error: No such module "Citation/CS1". Cryolite (Chryolit) is discussed on pp. 37–38. From p. 38: "Dieses sonderbare Fossil besteht aus Thonerde, Fluẞspathsäure und ein klein wenig Kali. Er kommt vor in Grönland, … " (This strange mineral consists of alumina, hydrofluoric acid and a very little potassium carbonate. It occurs in Greenland, … )
- Reprinted in French: Script error: No such module "Citation/CS1".
- Reprinted in English: Script error: No such module "Citation/CS1". See "Chryolite" on pp. 212–213.
- ↑ Albert Huntington Chester, A Dictionary of the Names of Minerals Including Their History and Etymology (New York, New York: John Wiley & Sons, 1896), p. 68.
- ↑ Script error: No such module "citation/CS1".
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