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Jarosite

Jarosite
Jarosite on quartz Potassium iron sulfate Arabia District, Pershing County, Nevada 2779.jpg
Jarosite on quartz from the Arabia District, Pershing County, Nevada
General
Category Sulfate minerals
Formula
(repeating unit)
KFe3+3(OH)6(SO4)2
Strunz classification 7.BC.10
Dana classification 30.2.5.1
Crystal system Trigonal
Crystal class Rhombohedral (3m)
H-M symbol: (3m)
Space group R3m
Unit cell a = 7.304 Å, c = 17.268 Å; Z = 3
Identification
Formula mass 500.8 g/mol
Color Amber yellow or dark brown
Crystal habit Crystals are usually pseudocubic or tabular, also as granular crusts, nodules, fibrous masses or concretionary.
Cleavage Distinct on {0001}
Fracture Uneven to conchoidal
Tenacity Brittle
Mohs scale hardness 2.5 - 3.5
Luster Subadamantine to vitreous, resinous on fractures
Streak light yellow
Diaphaneity Transparent to translucent
Specific gravity 2.9 to 3.3
Optical properties Uniaxial (-), usually anomalously biaxial with very small 2V
Refractive index nω = 1.815 to 1.820; nε = 1.713 to 1.715
Birefringence 0.102 to 0.105
Pleochroism E colorless, very pale yellow, or pale greenish yellow, O deep golden yellow or reddish brown
Solubility Insoluble in water. Soluble in HCl.
Other characteristics Strongly pyroelectric. Non-fluorescent. Barely detectable radioactivity
References

Jarosite is a basic hydrous sulfate of potassium and iron with a chemical formula of KFe3+3(OH)6(SO4)2. This sulfate mineral is formed in ore deposits by the oxidation of iron sulfides. Jarosite is often produced as a byproduct during the purification and refining of zinc and is also commonly associated with acid mine drainage and acid sulfate soil environments.

Jarosite has a trigonal crystal structure and is brittle, with basal cleavage, a hardness of 2.5-3.5, and a specific gravity of 3.15-3.26. It is translucent to opaque with a vitreous to dull luster, and is colored dark yellow to yellowish-brown. It can sometimes be confused with limonite or goethite with which it commonly occurs in the gossan (oxidized cap over an ore body). Jarosite is an iron analogue of the potassium aluminium sulfate, alunite.

The alunite supergroup includes the alunite, jarosite, beudantite, crandallite and florencite subgroups. The alunite supergroup minerals are isostructural with each other and substitution between them occurs, resulting in several solid solution series. The alunite supergroup has the general formula AB3(TO4)2(OH)6. In the alunite subgroup B is Al, and in the jarosite subgroup B is Fe3+. The beudantite subgroup has the general formula AB3(XO4)(SO4)(OH)6, the crandallite subgroup AB3(TO4)2(OH)5.H2O and the florencite subgroup AB3(TO4)2(OH)5or6.


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