Uranophane | |
---|---|
General | |
Category | Uranyl neso- and polysilicates |
Formula (repeating unit) | Ca(UO2)2[HSiO42·5H2O |
IMA symbol | Urp-α [1] |
Strunz classification | 9.AK.15 |
Crystal system | Monoclinic |
Crystal class | Sphenoidal (2) (same H-M symbol) |
Space group | P21 |
Unit cell | a = 15.85
Å, b = 6.98 Å c = 6.64 Å; β = 97.45°; Z = 2 |
Identification | |
Formula mass | 586.36 g/mol |
Color | Light yellow, lemon-yellow, honey-yellow, straw-yellow, green-yellow |
Crystal habit | Crystals occur as stellate needle aggregates; as fibrous crusts, and massive |
Cleavage | {100} Perfect |
Fracture | Uneven |
Tenacity | Brittle |
Mohs scale hardness | 2.5 |
Luster | Vitreous to pearly; waxy or dull when massive |
Streak | Yellowish white |
Diaphaneity | Translucent to subtranslucent |
Specific gravity | 3.81–3.90 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.643 nβ = 1.666 nγ = 1.669 |
Birefringence | δ = 0.026 |
Pleochroism | Weak; X = colorless; Y = pale canary-yellow; Z = canary-yellow |
2V angle | 32° to 45°, measured |
Ultraviolet fluorescence | Weak yellow-green under both short and long UV |
Other characteristics | Radioactive |
References | [2] [3] [4] |
Uranophane ( Ca( U O2)2( SiO3O H)2·5 H2O), also known as uranotile, is a rare calcium uranium silicate hydrate mineral that forms from the oxidation of other uranium-bearing minerals. It has a yellow color and is radioactive.
Alice Mary Weeks, and Mary E. Thompson of the United States Geological Survey, identified uranophane in 1953. [5]
Classic samples have been produced at Madawaska Mine near Bancroft, Ontario. [6]
Uranophane | |
---|---|
General | |
Category | Uranyl neso- and polysilicates |
Formula (repeating unit) | Ca(UO2)2[HSiO42·5H2O |
IMA symbol | Urp-α [1] |
Strunz classification | 9.AK.15 |
Crystal system | Monoclinic |
Crystal class | Sphenoidal (2) (same H-M symbol) |
Space group | P21 |
Unit cell | a = 15.85
Å, b = 6.98 Å c = 6.64 Å; β = 97.45°; Z = 2 |
Identification | |
Formula mass | 586.36 g/mol |
Color | Light yellow, lemon-yellow, honey-yellow, straw-yellow, green-yellow |
Crystal habit | Crystals occur as stellate needle aggregates; as fibrous crusts, and massive |
Cleavage | {100} Perfect |
Fracture | Uneven |
Tenacity | Brittle |
Mohs scale hardness | 2.5 |
Luster | Vitreous to pearly; waxy or dull when massive |
Streak | Yellowish white |
Diaphaneity | Translucent to subtranslucent |
Specific gravity | 3.81–3.90 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.643 nβ = 1.666 nγ = 1.669 |
Birefringence | δ = 0.026 |
Pleochroism | Weak; X = colorless; Y = pale canary-yellow; Z = canary-yellow |
2V angle | 32° to 45°, measured |
Ultraviolet fluorescence | Weak yellow-green under both short and long UV |
Other characteristics | Radioactive |
References | [2] [3] [4] |
Uranophane ( Ca( U O2)2( SiO3O H)2·5 H2O), also known as uranotile, is a rare calcium uranium silicate hydrate mineral that forms from the oxidation of other uranium-bearing minerals. It has a yellow color and is radioactive.
Alice Mary Weeks, and Mary E. Thompson of the United States Geological Survey, identified uranophane in 1953. [5]
Classic samples have been produced at Madawaska Mine near Bancroft, Ontario. [6]