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Bismutite

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(Redirected from Bismuthite) Bismuth carbonate mineral
Bismutite
Bismutite from Schneeberg, Germany
General
CategoryCarbonate mineral
Formula
(repeating unit)
Bi2(CO3)O2
IMA symbolBit
Strunz classification5.BE.25
Dana classification16a.03.05.01
Crystal systemOrthorhombic
Crystal classPyramidal (mm2)
(same H-M symbol)
Space groupImmm
Unit cella = 3.865 Å, b = 3.862 Å,
c = 13.675 Å; Z = 2
Identification
ColorYellow to brown, greenish, green-grey, grey or black
Crystal habitVery rare as platy crystals; typically radially fibrous to spheroidal, in crusts and earthy to dense massive aggregates
Twinningpseudo-merohedral twinning simulates tetragonal symmetry
CleavageDistinct/Good on {001} (microscopically observable)
Mohs scale hardness2.5 – 3.5
LusterVitreous, waxy, may be dull to earthy
StreakGrey
DiaphaneityOpaque to transparent in small grains
Specific gravity6.7 – 7.4 measured, 8.15 calculated
Optical propertiesBiaxial (−) (appears uniaxial due to twinning)
Refractive indexa=2.12–2.15, b=2.12–2.15, g=2.28
Birefringence0.1300–0.1600
2V angle45
References

Bismutite or bismuthite is a bismuth carbonate mineral with formula Bi2(CO3)O2 (bismuth subcarbonate). Bismutite occurs as an oxidation product of other bismuth minerals such as bismuthinite and native bismuth in hydrothermal veins and pegmatites. It crystallizes in the orthorhombic system and typically occurs as earthy to fibrous masses.

It was first described in 1841 for an occurrence in Saxony.

The term bismuthite has been used in the past for bismuthinite.

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. ^ Webmineral
  3. ^ Mindat
  4. Handbook of mineralogy
  5. Grice, Joel D., A Solution to the Crystal Structures of Bismutite and Beyerite, The Canadian Mineralogist, Vol. 40, pp. 693–698 (2002)
  6. Chisholm, Hugh, ed. (1911). "Bismuthite" . Encyclopædia Britannica. Vol. 4 (11th ed.). Cambridge University Press. p. 11.

See also

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