General | |
---|---|
Category | Mineral |
Formula (repeating unit) | Rh17S15 |
IMA symbol | Mia |
Strunz classification | 2.BC.05 |
Crystal system | cubic |
Crystal class | Pm3n |
Unit cell | a = 10.024 V=1,007.22 Å3 |
Structure | |
SMILES [Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[Rh].[S].[S].[S].[S].[S].[S].[S].[S].[S].[S].[S].[S].[S].[S].[S] (SMILES input only shows in Preview. SMILES is used to create the Jmol 3D image.) | |
Identification | |
Colour | light grey |
Tenacity | brittle |
Mohs scale hardness | 5-6 |
Luster | metallic |
Diaphaneity | Opaque |
Density | 7.42 |
Solubility | insoluble |
Miassite is a mineral made of rhodium and sulfur, with the stoichometric formula Rh
17S
15. It was named after the Miass River in the Urals.[1] It is a superconductor and an unconventional superconductor. Naturally occurring miassite is too brittle, so it is made in a lab for superconductor research. [2]
Its ability to be an unconventional superconductor was discovered at Ames National Laboratory in 2024. [3]
Miassite, covellite, parkerite, and palladseite, occur in nature, and are also made in labs as superconductors. Miassite is the only one found to also have unconventional superconductivity. [4]