Crystal structure of sideronatrite-2M, Na<sub>2</sub>Fe(SO<sub>4</sub>)<sub>2</sub>(OH)(H<sub>2</sub>O)<sub>3</sub>, a new polytype from Xitieshan lead-zinc deposit, Qinghai Province, China
- Autor(en)
- Zhuming Yang, Gerald Giester, Kuishou Ding, He Li
- Abstrakt
A monoclinic (2M) polytype of sideronatrite, Na2Fe(SO4)2(OH)(H2O)3, was found at Xitieshan, Qinghai Province, China. The crystal structure was solved by direct methods and refined by full-matrix least-squares (R1 = 3.88 %) in the space group P121/n1 with a = 7.1559(14), b = 7.2845(15), c = 20.889(4)Å, ß = 99.37(3)°, V = 1074.4(4)Å3, and Z = 4, using 2207 observed reflections with I > 2s(I). The atomic arrangement of sideronatrite-2M confirms a theoretical model in space group P21/a, previously proposed in literature. The structure of sideronatrite-2M is based on ferric-sulfate chains of 7 Å periodicity, similar to those observed in the structures of the orthorhombic polytype and of metasideronatrite. The system of hydrogen bonds has been determined.
- Organisation(en)
- Institut für Mineralogie und Kristallographie
- Externe Organisation(en)
- Chinese Academy of Sciences (CAS)
- Journal
- European Journal of Mineralogy: an international journal of mineralogy, geochemistry and related sciences
- Band
- 27
- Seiten
- 427-432
- Anzahl der Seiten
- 6
- ISSN
- 0935-1221
- DOI
- https://doi.org/10.1127/ejm/2015/0027-2441
- Publikationsdatum
- 06-2015
- Peer-reviewed
- Ja
- ÖFOS 2012
- 105116 Mineralogie, 105113 Kristallographie
- Schlagwörter
- ASJC Scopus Sachgebiete
- Geochemistry and Petrology
- Link zum Portal
- https://ucrisportal.univie.ac.at/de/publications/crystal-structure-of-sideronatrite2m-na2feso42ohh2o3-a-new-polytype-from-xitieshan-leadzinc-deposit-qinghai-province-china(9c313dfc-3841-4c82-8c16-469876ad6ed4).html