| Oppenheimerite | |
|---|---|
| General | |
| Category | Sulfate mineral |
| Formula | Na2(UO2)(SO4)2•3H2O |
| IMA symbol | Ohm |
| Crystal system | Triclinic |
| Crystal class | Pinacoidal (1) (same H-M symbol) |
| Space group | P1 |
| Unit cell | a = 7.96, b = 8.20, c = 9.81 [Å]; α = 65.97° β = 70.28°, γ = 91.46° (approximated), Z = 2 |
| Identification | |
| Color | Pale greenish-yellow |
| Crystal habit | prismatic |
| Cleavage | {110}, {011} and {101}, good |
| Fracture | Irregular |
| Mohs scale hardness | 2.5 |
| Luster | Vitreous |
| Streak | White |
| Diaphaneity | Transparent |
| Density | 3.36 (calculated) (approximated) |
| Optical properties | Biaxal (+) |
| Refractive index | nα=1.54, nβ=1.63, nγ=1.59 (approximated) |
| Pleochroism | Very pale greenish-yellow (X), pale greenish-yellow (Y), greenish-yellow (Z) |
| 2V angle | 72o (measured) |
| Ultraviolet fluorescence | Greenish-white |
| Other characteristics | |
| References | |
Oppenheimerite is a very rare uranium mineral with the formula Na2(UO2)(SO4)2•3H2O. Chemically related minerals include fermiite, natrozippeite, plášilite, belakovskiite and meisserite. Most of these uranyl sulfate minerals were originally found in the Blue Lizard mine, San Juan County, Utah, US. The mineral is named after American Theoretical physicist J. Robert Oppenheimer.
Oppenheimerite is associated with other sulfate minerals: fermiite, bluelizardite, wetherillite, blödite, chalcanthite, epsomite, gypsum, hexahydrite, kröhnkite, manganoblödite, sideronatrite, and tamarugite.
The crystal structure of oppenheimerite is of a new type. It contains chains of the (UO2)(SO4)2(H2O) composition, connected with two types of sodium polyhedra.