szomolnokite
{{Infobox mineral
| name = Szomolnokite
| category = Sulfate mineral
| image = Halotriquita i szomolnokita.png
| imagesize =
| alt =
| caption = Halotrichite (Hal); szomolnokite (Szo) and voltaite (Vol)
| formula = Fe2+SO4 · H2O
| molweight =
| strunz = 7.CB.05
| dana = 29.6.2.2
| system = Monoclinic
| class = Prismatic (2/m)
| symmetry = C2/c (no. 15)
| unit cell =
| color = Sulfur-yellow, yellow-brown, red-brown, blue, colorless
| habit = Bipyramidal, distorted, tabular, parallel growths, globular, stalactites
| twinning =
| cleavage =
| fracture = Conchoidal to sub-conchoidal, uneven
| tenacity = Brittle
| mohs = 2.5
| luster = Vitreous
| refractive =
| opticalprop = Biaxial (+), colorless (transmitted light)
| birefringence =
| 2V = 80° (measured), 86° (calculated)
| pleochroism =
| streak =
| gravity = 3.03–3.07 (measured), 3.10 (calculated)
| melt =
| fusibility =
| diagnostic =
| solubility =
| diaphaneity = Translucent
| other =
| references = {{cite journal |last1=Wildner |first1=M. |last2=Giester |first2=G. |journal=Neues Jahrbuch für Mineralogie - Monatshefte |volume=1991 |year=1991 |pages=296–306 |title=The crystal structures of kieserite-type compounds. I. Crystal structures of Me(II)SO4*H2O (Me = Mn,Fe,Co,Ni,Zn)}}
}}
Szomolnokite (Fe2+SO4·H2O) is a monoclinic iron sulfate mineral forming a complete solid solution with magnesium end-member kieserite (MgSO4·H2O).[http://www.mindat.org/min-3859.html Mindat.org - Szomolnokite] In 1877 szomolnokite's name was derived by Joseph Krenner from its type locality of oxidized sulfide ore containing iron in Szomolnok, Slovakia (Hungary at the time).[http://webmineral.com/data/Szomolnokite.shtml Webmineral - Szomolnokite][http://www.handbookofmineralogy.com/pdfs/szomolnokite.pdf Handbook of Mineralogy - Szomolnokite]
As of mid-January 2020 the only continent on which szomolnokite has not been found and reported is Antarctica.
At room temperature szomolnokite is stable up to a pressure of 6.2 GPa, and then transforms into triclinic crystal structure.{{Cite journal |last1=Meusburger |first1=J. M. |last2=Ende |first2=M. |last3=Talla |first3=D. |last4=Wildner |first4=M. |last5=Miletich |first5=R. |date=2019-09-01 |title=Transformation mechanism of the pressure-induced C2/c-to-P1¯ transition in ferrous sulfate monohydrate single crystals |url=https://www.sciencedirect.com/science/article/pii/S0022459619302853 |journal=Journal of Solid State Chemistry |language=en |volume=277 |pages=240–252 |doi=10.1016/j.jssc.2019.06.004 |bibcode=2019JSSCh.277..240M |s2cid=197070809 |issn=0022-4596}}
References
{{reflist}}
Bibliography
- Palache, P.; Berman H.; Frondel, C. (1960). "Dana's System of Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)" John Wiley and Sons, Inc., New York, pp. 479–480.
Category:Minerals in space group 15
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