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