Cuprosklodowskite
Cuprosklodowskite is a secondary uranium mineral formed by alteration of earlier uranium minerals. Its empirical formula is Cu(UO2)2(HSiO4)2·6(H2O).[2] Cuprosklodowskite is a nesosilicate mineral, It is grass green to dark green in color, and its crystal habit is typically acicular, flat bladed crystals. It is a strongly radioactive mineral.
| Cuprosklodowskite | |
|---|---|
 Cuprosklodowskite, Musonoi mine, Kolwezi, Lualaba District, Democratic Republic of the Congo {3.6 x 2.7 x 2.2 cm} | |
| General | |
| Category | Uranium mineral |
| Formula (repeating unit) | Cu(UO2)2(HSiO4)2·6(H2O) |
| Strunz classification | 9.AK.10 |
| Crystal system | Triclinic |
| Crystal class | Pinacoidal (1) (same H-M symbol) |
| Space group | P1 |
| Unit cell | a = 7.052(5) Å, b = 9.267(8) Å, c = 6.655(5) Å; α = 109.23°, β = 89.84°, γ = 110.01°; Z = 1 |
| Identification | |
| Color | Yellowish to grass-green |
| Crystal habit | In radiating groups of acicular flattened or bladed needles or fibrous crusts |
| Cleavage | On {100} |
| Fracture | Uneven |
| Mohs scale hardness | 4 |
| Luster | Dull to silky in aggregates |
| Streak | Greenish yellow |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 3.85 |
| Optical properties | Biaxial (-) |
| Refractive index | nα = 1.654 - 1.655 nβ = 1.664 - 1.667 nγ = 1.664 - 1.667 |
| Birefringence | δ = 0.010 - 0.012 |
| Pleochroism | X = nearly colorless; Y = Z = yellowish green |
| Other characteristics |  Radioactive |
| References | [1][2][3] |
Cuprosklodowskite was discovered in 1933 at the Kalongwe deposit in (then) Katanga province, Belgian Congo, the type locality. It was named in the mistaken belief that the mineral was the copper analogue of sklodowskite, which in turn was named for Marie Skłodowska Curie (1867–1934).
It occurs in association with becquerelite, brochantite, uranophane, kasolite, vandenbrandeite, liebigite and compreignacite.[1]
References
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