| Plášilite | |
| Category: | Sulfate mineral |
| Formula: | Na(UO2)(SO4)(OH)•2H2O |
| Imasymbol: | Pšl[1] |
| System: | Monoclinic |
| Class: | Prismatic (2/m) (same H-M symbol) |
| Symmetry: | P21/c |
| Unit Cell: | a = 8.71, b = 13.84, c = 7.05 [Å], β = 112.13° (approximated) |
| Color: | Greenish yellow |
| Habit: | prismatic |
| Cleavage: | and, perfect |
| Tenacity: | Brittle |
| Mohs: | 2-3 |
| Luster: | Vitreous |
| Streak: | White |
| Diaphaneity: | Transparent |
| Density: | 3.73 (calculated) (approximated) |
| Opticalprop: | Biaxal (+) |
| Refractive: | nα=1.56, nβ=1.58, nγ=1.61 (approximated) |
| Pleochroism: | ~Colourless (X), very pale yellow (Y), pale yellow (Z) |
| 2V: | 88o (measured) |
| Fluorescence: | Bluish-white |
| Other: | Radioactive |
| References: | [2] |
Plášilite is a very rare uranium mineral with the formula Na2(UO2)(SO4)2•3H2O.[3] Chemically related minerals include natrozippeite, belakovskiite, meisserite, fermiite and oppenheimerite.[4] [5] [6] [7] [8] Most of these uranyl sulfate minerals were originally found in the Blue Lizard mine, San Juan County, Utah, US.[9] The mineral is named after Czech crystallographer Jakub Plášil.
Plášilite is associated with other sulfate minerals: natrozippeite, johannite, blödite, brochantite, chalcanthite, gypsum, hexahydrite, manganoblödite, and tamarugite. Non-sulfate coexisting minerals include atacamite, calcite, dickite and gerhardtite. Plášilite is secondary in origin, being the product of weathering of the primary uranium mineral, uraninite.
The crystal structure of plášilite is of a new type. Its building blocks are:
The sodium-bearing polyhedra link the uranyl-sulfate sheets. It terms of sheet geometry, crystal structure of plášilite is similar to that of deliensite.