Mohrite, (NH4)2Fe(SO4)2·6 H2O, is a rare ammonium iron(II) sulfate mineral originally found in the geothermal fields of Tuscany, Italy.[1] This Fe-dominant analogue of boussingaultite is sometimes reported from burning coal dumps where it is a product of pyrite oxidation.[2][3][4]
| Mohrite | |
|---|---|
 A close up of the yellowish microcrystals of the mohrite mineral | |
| General | |
| Category | Mineral |
| Formula (repeating unit) | NH4)2Fe(SO4)2·6 H2O |
The mineral crystallizes in the monoclinic crystal system with space group P21/a.[5]
See also
editReferences
edit- ^ Fleischer M. 1965: New mineral names. American Mineralogist, 50, 805
- ^ Chesnokov B. V. and Shcherbakova E. P. 1991: Mineralogiya gorelykh otvalov Chelyabinskogo ugolnogo basseina - opyt mineralogii tekhnogenesa. Nauka, Moscow
- ^ Mindat - Mohrite
- ^ "Handbook of Mineralogy - Mohrite" (PDF). Archived from the original (PDF) on 2012-07-16. Retrieved 2013-01-25.
- ^ Figgis, B. N.; Kucharski, E. S.; Reynolds, P. A.; Tasset, F. (15 June 1989). "The structure of (ND4)2Fe(SO4)2 · 6 D2O at 4.3 K by neutron diffraction". Acta Crystallographica Section C Crystal Structure Communications. 45 (6): 942–944. Bibcode:1989AcCrC..45..942F. doi:10.1107/S0108270188013903.