Cryolite

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Cryolite
816- Ivigtut - cryolite.jpg
Cryolite from Ivittuut, Greenland
General
Category Halide mineral
Formula
(repeating unit)
Na3AlF6
IMA symbol Crl [1]
Strunz classification 3.CB.15
Dana classification 11.6.1.1
Crystal system Monoclinic
Crystal class Prismatic (2/m)
(same H-M symbol)
Space group P21/n
Unit cell a = 7.7564(3) Å,
b = 5.5959(2) Å,
c = 5.4024(2) Å; β = 90.18°; Z = 2
Identification
Formula mass 209.9 g mol−1
ColorColorless to white, also brownish, reddish and rarely black
Crystal habit Usually massive, coarsely granular. The rare crystals are equant and pseudocubic
Twinning Very common, often repeated or polysynthetic with simultaneous occurrence of several twin laws
Cleavage None observed
Fracture Uneven
Tenacity Brittle
Mohs scale hardness2.5 to 3
Luster Vitreous to greasy, pearly on {001}
Streak White
Diaphaneity Transparent to translucent
Specific gravity 2.95 to 3.0.
Optical propertiesBiaxial (+)
Refractive index nα = 1.3385–1.339, nβ = 1.3389–1.339, nγ = 1.3396–1.34
Birefringence δ = 0.001
2V angle 43°
Dispersion r < v
Melting point 1012 °C
Solubility Soluble in AlCl3 solution, soluble in H2SO4 with the evolution of HF, which is poisonous. Insoluble in water. [2]
Other characteristicsWeakly thermoluminescent. Small clear fragments become nearly invisible when placed in water, since its refractive index is close to that of water. May fluoresce intense yellow under SWUV, with yellow phosphorescence, and pale yellow phosphorescence under LWUV. Not radioactive.
References [3] [4] [5] [6] [7]

Cryolite (Na 3 Al F 6, sodium hexafluoroaluminate) is an uncommon mineral identified with the once-large deposit at Ivittuut on the west coast of Greenland, mined commercially until 1987. [8]

Contents

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 Peder Christian Abildgaard (1740–1801); [9] [10] it was obtained from a deposit of it in Ivigtut (old spelling) and nearby Arsuk Fjord, Southwest Greenland. [11] The name is derived from the Greek language words κρύος (cryos) = frost, and λίθος (lithos) = stone. [12] 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 ]

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.[ citation needed ]

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. [13]

Source locations

The cryolite mine Ivigtut, Greenland, summer 1940 Cryolite mine ivgtut greenland.jpg
The cryolite mine Ivigtut, Greenland, summer 1940

Besides Ivittuut, on the west 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. [14] [15]

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 [16] thus making the extraction of aluminium more economical. [17]

Cryolite is used as an insecticide and a pesticide. [18] It is also used to give fireworks a yellow color. [19]

Physical properties

Cryolite's unit cell. Fluorine atoms (yellow) are arranged in octahedra around aluminium atoms (red). Sodium ions (purple) occupy the interstices between the octahedra. Cryolite-unit-cell-3D-polyhedra.png
Cryolite's unit cell. Fluorine atoms (yellow) are arranged in octahedra around aluminium atoms (red). Sodium ions (purple) occupy the interstices between the octahedra.

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. [7]

Related Research Articles

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Bauxite is a sedimentary rock with a relatively high aluminium content. It is the world's main source of aluminium and gallium. Bauxite consists mostly of the aluminium minerals gibbsite (Al(OH)3), boehmite (γ-AlO(OH)) and diaspore (α-AlO(OH)), mixed with the two iron oxides goethite (FeO(OH)) and haematite (Fe2O3), the aluminium clay mineral kaolinite (Al2Si2O5(OH)4) and small amounts of anatase (TiO2) and ilmenite (FeTiO3 or FeO.TiO2). Bauxite appears dull in luster and is reddish-brown, white, or tan.

<span class="mw-page-title-main">Mineral</span> Crystalline chemical element or compound formed by geologic processes

In geology and mineralogy, a mineral or mineral species is, broadly speaking, a solid substance with a fairly well-defined chemical composition and a specific crystal structure that occurs naturally in pure form.

<span class="mw-page-title-main">Titanium</span> Chemical element, symbol Ti and atomic number 22

Titanium is a chemical element; it has symbol Ti and atomic number 22. Found in nature only as an oxide, it can be reduced to produce a lustrous transition metal with a silver color, low density, and high strength, resistant to corrosion in sea water, aqua regia, and chlorine.

<span class="mw-page-title-main">Fluorite</span> Mineral form of calcium fluoride

Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2. It belongs to the halide minerals. It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon.

<span class="mw-page-title-main">Aluminium oxide</span> Chemical compound with formula Al2O3

Aluminium oxide (or aluminium(III) oxide) is a chemical compound of aluminium and oxygen with the chemical formula Al2O3. It is the most commonly occurring of several aluminium oxides, and specifically identified as aluminium oxide. It is commonly called alumina and may also be called aloxide, aloxite, or alundum in various forms and applications. It occurs naturally in its crystalline polymorphic phase α-Al2O3 as the mineral corundum, varieties of which form the precious gemstones ruby and sapphire. Al2O3 is significant in its use to produce aluminium metal, as an abrasive owing to its hardness, and as a refractory material owing to its high melting point.

<span class="mw-page-title-main">Ilmenite</span> Titanium-iron oxide mineral

Ilmenite is a titanium-iron oxide mineral with the idealized formula FeTiO
3
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<span class="mw-page-title-main">Gadolinite</span> Nesosilicate mineral

Gadolinite, sometimes known as ytterbite, is a silicate mineral consisting principally of the silicates of cerium, lanthanum, neodymium, yttrium, beryllium, and iron with the formula (Ce,La,Nd,Y)2FeBe2Si2O10. It is called gadolinite-(Ce) or gadolinite-(Y), depending on the prominent composing element. It may contain 35.5% yttria sub-group rare earths, 2.2% ceria earths, as much as to 11.6% BeO, and traces of thorium. It is found in Sweden, Norway, and the US.

The Hall–Héroult process is the major industrial process for smelting aluminium. It involves dissolving aluminium oxide (alumina) in molten cryolite and electrolyzing the molten salt bath, typically in a purpose-built cell. The Hall–Héroult process applied at industrial scale happens at 940–980 °C and produces 99.5–99.8% pure aluminium. Recycling aluminum requires no electrolysis, thus it is not treated in this way.

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2
SiF
6
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<span class="mw-page-title-main">Sodium hexafluoroaluminate</span> Chemical compound

Sodium hexafluoroaluminate is an inorganic compound with formula Na3AlF6. This white solid, discovered in 1799 by Peder Christian Abildgaard (1740–1801), occurs naturally as the mineral cryolite and is used extensively in the industrial production of aluminium metal. The compound is the sodium (Na+) salt of the hexafluoroaluminate (AlF63−) ion.

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<span class="mw-page-title-main">Ivittuut</span> Place in Greenland, Kingdom of Denmark

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References

  1. Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi: 10.1180/mgm.2021.43 . S2CID   235729616.
  2. CRC Handbook of Chemistry and Physics, 83rd Ed., p. 4–84.
  3. Gaines, Richard V.; Skinner, H. Catherine W.; Foord, Eugene E.; Mason, Brian; Rosensweig, Abraham (1997). Dana's new mineralogy : the system of mineralogy of James Dwight Dana and Edward Salisbury Dana (8th, entirely rewritten and greatly enl. ed.). New York: Wiley. ISBN   978-0-471-19310-4.
  4. "Cryolite: Cryolite mineral information and data". Mindat.org. 3 October 2010. Retrieved 25 October 2020.
  5. "Cryolite Mineral Data". Webmineral.com. Retrieved 25 October 2010.
  6. "Cryolite" (PDF). Handbook of Mineralogy. Retrieved 25 October 2010.
  7. 1 2 Klein, Cornelis; Hurlbut, Cornelius S. (1985). Manual of mineralogy : (after James D. Dana) (20th ed.). New York: Wiley. ISBN   0-471-80580-7.
  8. "Eclipse Metals buys unique historical cryolite mine in Greenland". im-mining.com. Retrieved 11 July 2022.
  9. Abildgaard (1799). "Norwegische Titanerze und andre neue Fossilien" [Norwegian titanium ores and other new fossils [i.e., anything dug out of the earth])]. Allgemeines Journal der Chemie (in German). 2: 502. In der ordentlichen Versammlung der königl. Gesellschaft der Wissenschaften am 1. Februar dieses Jahres stattete Hr. Prof. Abildgaard einen Bericht über die Norwegischen Titanerze und über die von ihm mit denselben angestellten Analysen ab. Zugleich theilte er auch eine Nachricht von einer vor wenigen Jahren aus Grönland nach Dänemark gebrachten besonders weißen spathartigen Miner mit. Einer damit angestellten Untersuchung zu folge bestand sie aus Thonerde und Flußspathsäure. Eine Verbindung, von welcher noch kein ähnliches Beyspiel im Mineralreich vorgekommen ist. Sie hat den Namen Chryolit erhalten, weil sie vor dem Löthrohre wie gefrorne Salzlauge schmilzt. (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.)
  10. Abildgaard, P. C. (1800). "Om Norske Titanertser og om en nye Steenart fra Grönland, som bestaaer af Flusspatsyre og Alunjord" [On Norwegian titanium ores and on a new mineral from Greenland, which consists of hydrofluoric acid and alumina]. Det Kongelige Danske Videnskabers-Selskabs (The Royal Danish Scientific Society). 3rd series (in Danish). 1: 305–316. [From p. 312] Han har kaldt denne grönlandske Steen Kryolith eller Iissteen formedelst dens Udseende, og fordi den smelter saa meget let for Blæsröret. (He has named this Greenlandic stone cryolite or ice stone on account of its appearance, and because it melts so easily under a blowpipe.)
  11. The Brazilian statesman and scientist José Bonifácio de Andrada e Silva also analyzed cryolite:
  12. 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.
  13. Magazine, Smithsonian. "How This Abandoned Mining Town in Greenland Helped Win World War II". Smithsonian Magazine. Retrieved 2023-03-26.
  14. "CRYOLITE (Sodium Aluminum Fluoride)". www.galleries.com. Retrieved 2020-10-07.
  15. "Cryolite | mineral". Encyclopedia Britannica. Retrieved 2020-10-07.
  16. Cassayre, Laurent; Palau, Patrice; Chamelot, Pierre; Massot, Laurent (11 November 2010). "Properties of Low-Temperature Melting Electrolytes for the Aluminum Electrolysis Process: A Review" (PDF). Journal of Chemical & Engineering Data. 55 (11): 4549–4560. doi:10.1021/je100214x.
  17. Totten, George E.; MacKenzie, D. Scott (2003). Handbook of Aluminum: Volume 2: Alloy production and materials manufacturing. vol. 2. New York, NY: Marcel Dekker, Inc. ISBN   0-8247-0896-2.
  18. Rao, J.R.; Krishnayya, P.V.; Rao, P.A. (2000). "Efficacy of cryolite against major lepidopteran pests of cauliflower". Plant Protection Bulletin. 52 (3/4): 16–18. ISSN   0378-0449 . Retrieved 17 June 2021.
  19. Helmenstine, Anne Marie. "How Firework Colors Work and the Chemicals That Make Vivid Colors". ThoughtCo. Retrieved 2019-09-01.