Mohrite

{{Short description|Rare ammonium iron(II) sulfate mineral}}

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| caption = A close up of the yellowish microcrystals of the mohrite mineral

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| formula = NH4)2Fe(SO4)2·6 H2O

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Mohrite, (NH4)2Fe(SO4)2·6 H2O, is a rare ammonium iron(II) sulfate mineral originally found in the geothermal fields of Tuscany, Italy.Fleischer M. 1965: New mineral names. American Mineralogist, 50, 805 This Fe-dominant analogue of boussingaultite is sometimes reported from burning coal dumps where it is a product of pyrite oxidation.Chesnokov B. V. and Shcherbakova E. P. 1991: Mineralogiya gorelykh otvalov Chelyabinskogo ugolnogo basseina - opyt mineralogii tekhnogenesa. Nauka, Moscow[http://www.mindat.org/min-2742.html Mindat - Mohrite]{{Cite web |url=http://www.handbookofmineralogy.com/pdfs/mohrite.pdf |title=Handbook of Mineralogy - Mohrite |access-date=2013-01-25 |archive-date=2012-07-16 |archive-url=https://web.archive.org/web/20120716025543/http://www.handbookofmineralogy.com/pdfs/mohrite.pdf |url-status=dead }}

The mineral crystallizes in the monoclinic crystal system with space group P21/a.{{cite journal |last1=Figgis |first1=B. N. |last2=Kucharski |first2=E. S. |last3=Reynolds |first3=P. A. |last4=Tasset |first4=F. |title=The structure of (ND4)2Fe(SO4)2 · 6 D2O at 4.3 K by neutron diffraction |journal=Acta Crystallographica Section C Crystal Structure Communications |date=15 June 1989 |volume=45 |issue=6 |pages=942–944 |doi=10.1107/S0108270188013903|bibcode=1989AcCrC..45..942F }}

See also

References