SODDYITE
Class : Silicates
Subclass : Nesosilicates
Crystal system : Orthorhombic
Chemistry : (UO2)2SiO4 2H2O
Rarity : Rare
Soddyite is a hydrated uranium silicate, one of the many secondary minerals present in the oxidation zone of uranium deposits. It is a rare mineral, exceptionally common in the Shinkolobwe deposit (Kantanga), where it is associated with kasolite, curite and metatorbernite. It was named in honor of the British physicist and radiochemist Frederick Soddy, to whom we owe the explanation of the mechanism of disintegration of atoms. Soddyite is lemon yellow to amber yellow, sometimes light green, it composes millimeter-sized crystals in the shape of acute bipyramids or elongated and striated prisms.
Main photo : Soddyite of Musonoï, Kolwezi, Democratic Republic of Congo © Gianfranco Ciccolini
Soddyite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 3 to 4
Density : 4.63 to 4.70
Fracture : Undetermined
Streak : Yellow
TP : Opaque to transparent
RI : 1.650 to 1.715
Birefringence : 0.049 to 0.061
Optical character : Biaxial -
Pleochroism : Weak
Fluorescence : None
Solubility : Hydrochloric acid
Magnetism : NoneRadioactivity : Very strong