Chemistry:Andradite

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Short description: Nesosilicate mineral species of garnet
Andradite [Adr]
Andradite-Mali.jpg
Single crystal (4.2 cm) – Diakon, Nioro du Sahel Circle, Kayes Region, Mali
General
CategoryGarnet group
Formula
(repeating unit)
Ca3Fe2(SiO4)3
Strunz classification9.AD.25
Crystal systemCubic
Crystal classHexoctahedral (m3m)
H-M symbol: (4/m 3 2/m)
Space groupIa3d
Unit cella = 12.056 Å; Z = 8
Identification
ColorYellow, greenish yellow to emerald-green, dark green; brown, brownish red, brownish yellow; grayish black, black; may be sectored
Crystal habitCommonly well-crystallized dodecahedra, trapezohedra, or combinations, also granular to massive
Cleavagenone
Fractureconchoidal to uneven
TenacityBrittle
Mohs scale hardness6.5 to 7
|re|er}}Adamantine to resinous, dull
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity3.859 calculated; 3.8–3.9 measured
Optical propertiesIsotropic, typically weakly anisotropic
Refractive indexn = 1.887
Absorption spectrademantoid – 440 nm band or complete absorption at 440 nm and below, may also have lines at 618, 634, 685, 690 nm[1]
References[1][2][3][4]
Major varieties
Demantoidtransparent light to dark green to yellow-green
Melaniteopaque black
Topazolitetransparent to translucent yellow, may show chatoyancy

Andradite is a mineral species of the garnet group. It is a nesosilicate, with formula Ca3Fe2Si3O12.

Andradite includes three varieties:

  • Melanite: Black in color due to limited substitution of titanium for iron. Also known as "titanian andradite". Forms a solid solution with morimotoite and schorlomite depending on titanium and iron content.[6]
  • Demantoid: Vivid green in color, one of the most valuable and rare stones in the gemological world.[7]
  • Topazolite: Yellow-green in color and sometimes of high enough quality to be cut into a faceted gemstone, it is rarer than demantoid.[7]

It was first described in 1868 for an occurrence in Drammen, Buskerud, Norway .[2][3][7] Andradite was named after the Brazil ian statesman, naturalist, professor and poet José Bonifácio de Andrada e Silva (1763–1838).[2][7]

Occurrence

It occurs in skarns developed in contact metamorphosed impure limestones or calcic igneous rocks; in chlorite schists and serpentinites and in alkalic igneous rocks (typically titaniferous). Associated minerals include vesuvianite, chlorite, epidote, spinel, calcite, dolomite and magnetite.[2] It is found in Iran, Italy, the Ural Mountains of Russia , Arizona and California and in Dnipropetrovsk Oblast in Ukraine .

Like the other garnets, andradite crystallizes in the cubic space group 3}}d, with unit-cell parameter of 12.051 Å at 100 K.[8]

The spin structure of andradite contains two mutually canted equivalent antiferromagnetic sublattices[9] below the Néel temperature (TN=11 K[10]).

See also


References

  1. 1.0 1.1 Gemological Institute of America, GIA Gem Reference Guide 1995, ISBN:0-87311-019-6
  2. 2.0 2.1 2.2 2.3 Handbook of Mineralogy
  3. 3.0 3.1 Andradite, Mindat.org
  4. Webmineral data
  5. Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine 85 (3): 291–320. doi:10.1180/mgm.2021.43. Bibcode2021MinM...85..291W. 
  6. Melanite, Mindat.org
  7. 7.0 7.1 7.2 7.3 Grande, Lance; Augustyn, Allison (2009). Gems and Gemstones: Timeless Natural Beauty of the Mineral World. University of Chicago Press. pp. 188–91. ISBN 978-0-226-30511-0. https://books.google.com/books?id=RnE9Fa4pbn0C. 
  8. Thomas Armbruster and Charles A. Geiger (1993): "Andradite crystal chemistry, dynamic X-site disorder and structural strain in silicate garnets." European Journal of Mineralogy v. 5, no. 1, p. 59-71.
  9. Danylo Zherebetskyy (2010). Quantum mechanical first principles calculations of the electronic and magnetic structure of Fe-bearing rock-forming silicates, PhD Thesis, Universal Publishers/Dissertation.com, Boca Raton, Florida, USA, p. 136. ISBN:1-59942-316-2.
  10. Enver Murad (1984): "Magnetic ordering in andradite." American Mineralogist 69, no. 7-8; pp. 722–24.

External links