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Schoepite, empirical formula (UO2)8O2(OH)12·12(H2O)[2] is a rare alteration product of uraninite in hydrothermal uranium deposits. It may also form directly from ianthinite. The mineral presents as a transparent to translucent yellow, lemon yellow, brownish yellow, or amber orthorhombic tabular crystals. Although over 20 other crystal forms have been noted; rarely in microcrystalline aggregates. When exposed to air schoepite converts over a short time to the metaschoepite form (UO3·nH2O, n < 2) within a few months of being exposed to ambient air.[2]
Schoepite | |
---|---|
General | |
Category | Uranium minerals |
Formula (repeating unit) | (UO2)8O2(OH)12 • 12(H2O) |
IMA symbol | Sho[1] |
Strunz classification | 4.GA.05 |
Crystal system | Orthorhombic |
Crystal class | Pyramidal (mm2) H-M symbol: (mm2) |
Space group | P21ca |
Unit cell | a = 14.33 Å, b = 16.79 Å c = 14.73 Å; Z = 4 |
Identification | |
Color | Amber, lemon- or sulfur yellow |
Crystal habit | Commonly as tabular equant, to short prismatic crystals; rarely in microcrystalline aggregates |
Cleavage | [001] Perfect, [010] indistinct |
Tenacity | Brittle |
Mohs scale hardness | 2.5 |
Luster | Adamantine |
Streak | Yellow |
Diaphaneity | Transparent to translucent |
Specific gravity | 4.8 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.690 nβ = 1.714 nγ = 1.735 |
Birefringence | δ = 0.045 |
Pleochroism | X = almost colorless; Y = Z = lemon-yellow to golden yellow |
2V angle | Measured: 89° |
Ultraviolet fluorescence | Short and long UV = pale green |
Other characteristics | Radioactive |
References | [2][3][4] |
The hardness is 2.5, density is 4.8 g/cm3, and it streaks yellow.
It was first described from specimens from Shinkolobwe mine in Belgian Congo in 1923,[2] several additional localities are known.
Schoepite was named to honor Alfred Schoep (1881–1966), Professor of Mineralogy at the University of Ghent, Belgium.[3]
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