Chemistry:Atacamite

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Short description: Halide evaporite mineral
Atacamite
Atacamite on malachite - Mt Gunson mines, South Australia.jpg
Atacamite from Mt. Gunson mines, South Australia
General
CategoryHalide mineral
Formula
(repeating unit)
Cu2Cl(OH)3
Strunz classification3.DA.10a
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space groupPnma
Unit cella = 6.03, b = 9.12
c = 6.865 [Å]; Z = 4
Identification
ColorBright green, dark emerald-green to blackish green
Crystal habitSlender prismatic crystals, fibrous, granular to compact, massive
TwinningContact and penetration with complex twinned groupings
CleavagePerfect on {010}, fair on {101}
FractureConchoidal
TenacityBrittle
Mohs scale hardness3–3.5
|re|er}}Adamantine to vitreous
StreakApple green
DiaphaneityTransparent to translucent
Specific gravity3.745–3.776
Optical propertiesBiaxial (−)
Refractive indexnα = 1.831 nβ = 1.861 nγ = 1.880
Birefringenceδ = 0.049
PleochroismX = pale green; Y = yellow-green; Z = grass-green
2V angleCalculated: 74°
Dispersionr < v, strong
References[1][2][3][4]

Atacamite is a copper halide mineral: a copper(II) chloride hydroxide with formula Cu2Cl(OH)3. It was first described for deposits in the Atacama Desert of Chile in 1802 by Dmitri de Gallitzin.[1] The Atacama Desert is also the namesake of the mineral.

Occurrence

Atacamite is polymorphous with botallackite, clinoatacamite, and paratacamite.[1] Atacamite is a comparatively rare mineral, formed from primary copper minerals in the oxidation or weathering zone of arid climates. It has also been reported as a volcanic sublimate from fumarole deposits, as sulfide alteration products in black smokers.[2] The mineral has also been found naturally on oxidized copper deposits in Chile, China , Russia , Czech Republic, Arizona, and Australia .[6] It occurs in association with cuprite, brochantite, linarite, caledonite, malachite, chrysocolla and its polymorphs.[2]

Synthetic Occurrence

Atacamite has been discovered in the patina of the Statue of Liberty, and as alteration of ancient bronze and copper artifacts. The mineral has been found as a pigment in sculpture, manuscripts, maps, and frescoes discovered in Eurasia, Russia , and Persia.[6]

Biomineral

Atacamite occurs as a biomineral in the jaws of bloodworms.[7][8]

References

  1. 1.0 1.1 1.2 Atacamite on Mindat.org
  2. 2.0 2.1 2.2 Handbook of Mineralogy
  3. Atacamite on Webmineral
  4. Mineralienatlas
  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. 6.0 6.1 "Atacamite – CAMEO" (in en). http://cameo.mfa.org/wiki/Atacamite. 
  7. "High abrasion resistance with sparse mineralization: copper biomineral in worm jaws". Science 298 (5592): 389–92. October 2002. doi:10.1126/science.1075433. PMID 12376695. Bibcode2002Sci...298..389L. 
  8. "Zinc and mechanical prowess in the jaws of Nereis, a marine worm". Proc. Natl. Acad. Sci. U.S.A. 100 (16): 9144–9. August 2003. doi:10.1073/pnas.1632658100. PMID 12886017. Bibcode2003PNAS..100.9144L. 

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