Jarosite | |
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General | |
Category | Sulfate minerals |
Formula (repeating unit) | KFe3(SO4)2(OH)6 |
IMA symbol | Jrs[1] |
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 | [2][3][4] |
Jarosite is a basic hydrous sulfate of potassium and ferric iron (Fe-III) with a chemical formula of KFe3(SO4)2(OH)6. 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.