Pararealgar
| Pararealgar | |
|---|---|
 | |
| General | |
| Category | Sulfide mineral |
| Formula (repeating unit) | As4S4 |
| IMA symbol | Prlg[1] |
| Strunz classification | 2.FA.15b |
| Crystal system | Monoclinic |
| Crystal class | Prismatic (2/m) (same H-M symbol) |
| Space group | P21/c |
| Unit cell | a = 9.909 Å, b = 9.655 Å, c = 8.502 Å; β = 97.20°; Z = 16 |
| Identification | |
| Colour | Bright yellow when powdery, to yellow-orange and orange-brown when granular |
| Crystal habit | Fine powder to granular |
| Fracture | Uneven |
| Tenacity | Brittle |
| Mohs scale hardness | 1 – 1.5 |
| Lustre | Vitreous to resinous |
| Streak | Bright yellow |
| Diaphaneity | Translucent |
| Specific gravity | 3.52 |
| Optical properties | Biaxial (?) |
| Birefringence | 2.02 |
| Pleochroism | High: x = orange yellow, y = bright yellow, z = orange red |
| References | [2][3][4][5] |
Pararealgar is an arsenic sulfide mineral with the chemical formula As4S4,[3] also represented as AsS.[5] It forms gradually from realgar under exposure to light. Its name derives from the fact that its elemental composition is identical to realgar, As4S4. It is soft with a Mohs hardness of 1 - 1.5, is yellow orange in colour, and its monoclinic prismatic crystals are very brittle, easily crumbling to powder.
It is one of the sulfides of arsenic and is one of two isomers of As4S4. It forms upon exposure of the symmetrical isomer to light. Its name derives from the fact that its elemental composition is identical to realgar, As4S4.
Structure
[edit]
realgar (left) and pararealgar.
Both isomers of As4S4 are molecular, in contrast to the other main sulfide of arsenic, orpiment (As2S3), which is polymeric. In pararealgar, there are three kinds of As centres (and three kinds of S centres). The molecule has Cs symmetry. In realgar, the four As (and four S) centres are equivalent and the molecule has D2d symmetry.[6] An analogous pair of isomers is also recognized for the corresponding phosphorus sulfides P4S4.[7]
Occurrence
[edit]Pararealgar occurs as an alteration product of realgar in stibnite-bearing quartz veins typically as a result of exposure to light. It occurs associated with realgar, stibnite, tetrahedrite, arsenopyrite, duranusite, native arsenic, arsenolite, native sulfur, lepidocrocite and pyrite.[5]
It was first described in 1980 for an occurrence in the Grey Rock Mine, Truax Creek, Bridge River area, Lillooet Mining Division, British Columbia, Canada.[3] It has since been reported from a variety of locations worldwide.
Formation
[edit]Pararealgar is an alteration product of realgar resulting from exposure to light. The process of alteration is dependent on the wavelength of light, with alteration only occurring at wavelengths longer than approximately 500 nm, in the visible light spectrum.
In realgar's crystal structure, each arsenic atom is bonded to two sulphur atoms and one other arsenic atom. The As-As bonds are 30% weaker than the As-S bonds and certain wavelengths of lights interact with the crystal structure of realgar, breaking the weaker bonds between arsenic atoms. The free As formed as a result of this process destabilises the realgar structure, causing the realgar to become powdery pararealgar without changing overall chemical composition.[8]
References
[edit]- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ mineralienatlas
- ^ a b c Mindat.org
- ^ Webmineral.com Mineralogy Database: Pararealgar
- ^ a b c Handbook of Mineralogy
- ^ Paola Bonazzi, Silvio Menchetti, Giovanni Pratesi "The crystal structure of pararealgar, As4S4" American Mineralogist, 1995, vol.80 400.
- ^ Jason, M. E.; Ngo, T.; Rahman, S. (1997). "Products and Mechanisms in the Oxidation of Phosphorus by Sulfur at Low Temperature". Inorg. Chem. 36 (12): 2633–2640. doi:10.1021/ic9614879.
- ^ Douglass, D. L.; Shing, Chichang; Wang, Ge (1992). "The light-induced alteration of realgar to pararealgar" (PDF). American Mineralogist. 77: 1266–1274. Retrieved 11 August 2014.