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Schoepite

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Mineral
Schoepite
General
CategoryUranium minerals
Formula
(repeating unit)
(UO2)8O2(OH)12 • 12(H2O)
IMA symbolSho
Strunz classification4.GA.05
Crystal systemOrthorhombic
Crystal classPyramidal (mm2)
H-M symbol: (mm2)
Space groupP21ca
Unit cella = 14.33 Å, b = 16.79 Å
c = 14.73 Å; Z = 4
Identification
ColorAmber, lemon- or sulfur yellow
Crystal habitCommonly as tabular equant, to short prismatic crystals; rarely in microcrystalline aggregates
Cleavage Perfect, indistinct
TenacityBrittle
Mohs scale hardness2.5
LusterAdamantine
StreakYellow
DiaphaneityTransparent to translucent
Specific gravity4.8
Optical propertiesBiaxial (−)
Refractive indexnα = 1.690 nβ = 1.714 nγ = 1.735
Birefringenceδ = 0.045
PleochroismX = almost colorless; Y = Z = lemon-yellow to golden yellow
2V angleMeasured: 89°
Ultraviolet fluorescenceShort and long UV = pale green
Other characteristics Radioactive
References

Schoepite, empirical formula (UO2)8O2(OH)12·12(H2O) 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.

The hardness is 2.5, density is 4.8 g/cm, and it streaks yellow.

It was first described from specimens from Shinkolobwe mine in Belgian Congo in 1923, several additional localities are known.

Schoepite was named to honor Alfred Schoep (1881–1966), Professor of Mineralogy at the University of Ghent, Belgium.

References

  1. 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.
  2. ^ Mindat.org
  3. ^ Webmineral data
  4. Handbook of Mineralogy


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