Kröhnkite
(repeating unit)Na2Cu(SO4)2•2H2O IMA symbol Khk[1] Strunz classification 7.CC.30 Crystal system Monoclinic Crystal class Prismatic (2/m)
(same H-M symbol) Space group P21/c Unit cell a = 5.78 Å, b = 12.58 Å
c = 5.48 Å; β = 108.3°; Z = 2 Identification Color Blue, dark sky blue, greenish blue, yellowish green Crystal habit Encrustations (on matrix), fibrous, massive Twinning Common, sometimes heart-shaped Cleavage Perfect {010}, good (011), very imperfect {101} Fracture Conchoidal Mohs scale hardness 2.5 – 3.0 Luster Vitreous Streak White Diaphaneity Transparent Specific gravity 2.92 Optical properties Biaxial (-) Refractive index nα = 1.544 nβ = 1.578 nγ = 1.601 Birefringence 0.057 2V angle 78° measured Solubility Readily soluble in water References [2][3][4][5]
(same H-M symbol)
c = 5.48 Å; β = 108.3°; Z = 2
Kröhnkite ( Na2Cu(SO4)2•2H2O ) is a rare copper sulfate mineral named after B. Kröhnke who first researched it.[3] Kröhnkite may be replaced by Saranchinaite, the anhydrous form of the mineral, if heated to temperatures above 200 °C (392 °F).[3]
Crystallography
Kröhnkite has monoclinic symmetry (2/m).[5] Monoclinic symmetry implies that the mineral contains three axes of differing length (typically labeled a, b, and c), two of which intersect each other at 90° and one that intersects at an acute angle.[6] Specifically, it belongs to the 2/m symmetry class meaning, the mineral has a 2-fold rotation axis about the b axis.[6] It also has a unique motif of sulfate tetrahedra chains and copper octahedra aligned along the c axis and linked together by sodium atoms.[5] Kröhnkite exhibits the optical property birefringence; the difference in the two refractive indices of a mineral.[3] Because this mineral is birefringent, it must be anisotropic. Anisotropic minerals cause the velocity of light to vary depending on the direction of travel through the mineral. Kröhnkite is biaxial negative, which reveals that the mineral has two optic axes.[3]
Importance
Kröhnkite has the same general formula ( (X2M(TO4)2(H2O)2) ) as minerals which are found in environments affected by hydrothermal alteration, making it important in identifying where such alterations have occurred. Furthermore, the minerals sharing this composition are organized according to three crystal structure types, one being the unique kröhnkite structure which is often used to describe minerals exhibiting the same chain-like structure.[7]
Discovery and occurrence
Kröhnkite was first researched after an occurrence in the Chuquicamata Mine, Chile, and has been reported from a number of locations in the Atacama region. Associated minerals in the discovery location include atacamite, blodite, chalcanthite, antlerite and natrochalcite. It occurs in the oxidized zone of copper deposits in arid environments.[4]
References
- ^ 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.
- ^ "Kröhnkite Mineral Data." http://webmineral.com/data/Krohnkite.shtml. Accessed 28 November 2010.
- ^ a b c d e Kröhnkite Mineral Data, Mindat.org, retrieved 8 October 2010
- ^ a b Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C. (2005). "Kröhnkite" (PDF). Handbook of Mineralogy. Mineral Data Publishing. Retrieved 22 May 2022.
- ^ a b c Hawthorne, F. C.; Ferguson, R. B. (15 June 1975). "Refinement of the crystal structure of kröhnkite". Acta Crystallographica Section B: Structural Crystallography and Crystal Chemistry. 31 (6): 1753–1755. doi:10.1107/S0567740875006048.
- ^ a b Schwarzenbach, Dieter (1996). Crystallography. New York: John Wiley. ISBN 978-0-471-95598-6.
- ^ Herwig, S.; Hawthorne, F. C. (1 October 2006). "The topology of hydrogen bonding in brandtite, collinsite and fairfieldite". The Canadian Mineralogist. 44 (5): 1181–1196. doi:10.2113/gscanmin.44.5.1181.
