Bismuth carbonate mineral
Bismutite |
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Bismutite from Schneeberg, Germany |
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Category | Carbonate mineral |
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Formula (repeating unit) | Bi2(CO3)O2 |
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IMA symbol | Bit[1] |
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Strunz classification | 5.BE.25 |
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Dana classification | 16a.03.05.01 |
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Crystal system | Orthorhombic |
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Crystal class | Pyramidal (mm2) (same H-M symbol) |
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Space group | Immm |
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Unit cell | a = 3.865 Å, b = 3.862 Å, c = 13.675 Å; Z = 2 |
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Color | Yellow to brown, greenish, green-grey, grey or black |
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Crystal habit | Very rare as platy crystals; typically radially fibrous to spheroidal, in crusts and earthy to dense massive aggregates |
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Twinning | pseudo-merohedral twinning simulates tetragonal symmetry |
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Cleavage | Distinct/Good on {001} (microscopically observable) |
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Mohs scale hardness | 2.5 – 3.5 |
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Luster | Vitreous, waxy, may be dull to earthy |
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Streak | Grey |
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Diaphaneity | Opaque to transparent in small grains |
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Specific gravity | 6.7 – 7.4 measured, 8.15 calculated |
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Optical properties | Biaxial (−) (appears uniaxial due to twinning) |
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Refractive index | a=2.12–2.15, b=2.12–2.15, g=2.28 |
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Birefringence | 0.1300–0.1600 |
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2V angle | 45 |
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References | [2][3][4][5] |
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Bismutite or bismuthite is a bismuth carbonate mineral with formula Bi2(CO3)O2 (bismuth subcarbonate). Bismutite occurs as an oxidation product of other bismuth minerals such as bismuthinite and native bismuth in hydrothermal veins and pegmatites.[3] It crystallizes in the orthorhombic system and typically occurs as earthy to fibrous masses.[2]
It was first described in 1841 for an occurrence in Saxony.[2]
The term bismuthite has been used in the past for bismuthinite.[6]
References
See also