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Radioactive yellow uranium-containing carbonate mineral From Wikipedia, the free encyclopedia
Schröckingerite is a radioactive yellow uranium-containing carbonate mineral, hydrated sodium calcium uranyl sulfate carbonate fluoride.[3][4][5] Schröckingerite crystallizes in the orthorhombic system, occurring as globular clusters, and fluoresces yellow-green under ultraviolet light.
Schröckingerite | |
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General | |
Category | Carbonate minerals |
Formula (repeating unit) | NaCa3(UO2)[F|(CO3)3(SO4)]·10(H2O)[1] |
IMA symbol | Srö[2] |
Strunz classification | 5.EG.05 |
Crystal system | Triclinic |
Crystal class | Pinacoidal (1) (same H-M symbol) |
Space group | P1 |
Identification | |
Other characteristics | Radioactive |
Schröckingerite was first described in 1783 from an occurrence in Jáchymov, Bohemia, Czech Republic, and named for its discoverer, Julius Freiherr Schröckinger von Neudenberg (1814–1882).[3][5]
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