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Contents

   



(Top)
 


1 Synthetic material  





2 Occurrence and discovery  





3 See also  





4 References  





5 Further reading  














Chaoite






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Chaoite
General
CategoryNative element mineral
Formula
(repeating unit)
C
IMA symbolCh[1]
Strunz classification1.CB.05b
Crystal systemHexagonal
Crystal classDihexagonal dipyramidal (6/mmm)
H-M symbol: (6/m 2/m 2/m)
Space groupP6/mmm
Unit cella = 8.948 Å, c = 14.078 Å; Z = 168
Identification
ColourBlack
Crystal habitThin 3-15 μm intergrowth lamallae with graphite
Mohs scale hardness1 - 2
LustreSubmetallic
DiaphaneityOpaque
Specific gravity3.43 (calculated)
References[2][3][4]

Chaoite, or white carbon, is a mineral described as an allotropeofcarbon whose existence is disputed. It was discovered in shock-fused graphite gneiss from the Ries crater in Bavaria. It has been described as slightly harder than graphite, with a reflection colour of grey to white.[5] From its electron diffraction pattern, the mineral has been considered to have a carbyne structure,[6] the linear acetylenic carbon allotrope of carbon. A later report has called this identification, and the very existence of carbyne phases, into question, arguing that the new reflections in the diffraction pattern are due to clay impurities.[7]

Synthetic material

[edit]

It has been claimed that an identical form can be prepared from graphite by sublimation at 2700-3000 K or by irradiating it with a laser in high vacuum. This substance has been termed ceraphite.[8]

A review cautions that "in spite of these seemingly definitive reports … several other groups have tried unsuccessfully to reproduce these experiments. Independent confirmatory work is obviously needed … and at the present time white graphite appears to be the carbon analog of polywater".[9]

Occurrence and discovery

[edit]

Chaoite was first described from Möttingen, Ries Crater, Nördlingen, Bavaria, Germany and approved by the IMA in 1969.[3] The mineral was named for USGS petrologist Edward C. T. Chao (1919-2008).[3] At the type locality in Bavaria chaoite occurs in graphite bearing gneiss that has undergone shock metamorphism.[2] It has also been reported from meteorites including the Goalpara meteorite in Assam, the Dyalpur meteorite in Uttar PradeshinIndia and the Popigai impact structure in the Anabarskii massif of Eastern Siberia.[2][3] Minerals associated with chaoite include: graphite, zircon, rutile, pseudobrookite, magnetite, nickeliferous pyrrhotite and baddeleyite.[2]

See also

[edit]

References

[edit]
  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.
  • ^ a b c d Handbook of Mineralogy
  • ^ a b c d Chaoite on Mindat.org
  • ^ Chaoite on Webmineral
  • ^ A. El Goresy, G. Donnay, A new allotriomorphic form of carbon from the Ries Crater, Science, 1969, 161, 363–364
  • ^ A.G. Whittaker, P.L. Kintner, Carbon: observation on the new allotropic form, Science 1969, 165, 589
  • ^ P.P.K. Smith, P.R. Buseck, Carbyne forms of carbon: do they exist? Science, 1982, 216, 984–986
  • ^ C. Nakayama, M. Okawa, H. Nagashima, Carbon 1977, 15, 434; D.J. Johnson, D. Crawford, C. Oates, 1971, 10th Carbon Conf, Bethlehem, PA, FC-18
  • ^ D.W. McKee, Annu. Rev. Mater. Sci. 1973, 3, 195
  • Further reading

    [edit]

    Frans J. M. Rietmeijer and Alessandra Rotundi, Chapter 16. Natural Carbynes, Including Chaoite, on Earth, in Meteorites, Comets, Circumstellar and Interstellar Dust, in Polyynes: Synthesis, Properties, and Applications, Edited by Franco Cataldo, CRC Press 2005, Pages 339–370, Print ISBN 978-1-57444-512-1 eBook ISBN 978-1-4200-2758-7 Contents link


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Chaoite&oldid=1139630235"

    Categories: 
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    Native element minerals
    Meteorite minerals
    Hexagonal minerals
    Minerals in space group 191
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    This page was last edited on 16 February 2023, at 02:43 (UTC).

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