K[(Cu<sup>II</sup>,Mn<sup>II</sup>,Mn<sup>III</sup>)<sub>2</sub>(TeO<sub>3</sub>)<sub>3</sub>·2H<sub>2</sub>O,the first zemannite-type structure based on a Jahn-Teller-distorted framework

Autor(en)
Felix Eder, Ronald Miletich, Matthias Weil
Abstrakt

Synthetic single crystals of K[(CuII,MnII,MnIII)2(TeO3)3]·2H2O were obtained from an overconcentrated alkaline aqueous solution in the system K2O-MnO-CuO-TeO2 under hydrothermal conditions at T ≤ 220 °C.

Subeuhedral single crystals have been investigated by means of

single-crystal X-ray diffraction. The crystal structure of this new

zemannite-type representative adopts a monoclinic twofold

superstructure. The doubling of the unit-cell volume is accompanied by a

hexagonal-to-monoclinic symmetry reduction, resulting in threefold

twinning with individual crystal domains following the space group

symmetry P21. Refinements of site-occupation factors

and the evaluation of bond valences suggest a distribution of di- and

trivalent cations at the octahedrally coordinated M sites with a ratio (CuII + MnII):MnIII approximating 1:1. Based on arguments about the cation sizes and the individual bond valence sums, a distribution of CuII1–xMnIIIx and MnIIx MnIII1–x at each two of the four M sites can be assumed with x between ~ 0.14 and ~ 0.50. The K+ cations and H2O

molecules inside the channels are located off the central channel axis.

In contrast to most other known zemannite-type phases, the

extra-framework atoms show full occupancies and are not disordered. The

distribution of the channel contents supports the anisotropic

deformation of the surrounding framework, which follows the local

symmetry reduction as required for the Jahn-Teller distortion of the

octahedrally coordinated M sites within the framework. The

arrangement of the deformed channels can be understood as the origin of

the existing superstructure.

Organisation(en)
Institut für Mineralogie und Kristallographie
Externe Organisation(en)
Technische Universität Wien
Journal
Mineralogy and Petrology
Band
117
Seiten
133-143
Anzahl der Seiten
11
ISSN
0930-0708
DOI
https://doi.org/10.1007/s00710-022-00808-9
Publikationsdatum
06-2023
Peer-reviewed
Ja
ÖFOS 2012
105116 Mineralogie, 105113 Kristallographie
Schlagwörter
ASJC Scopus Sachgebiete
Geochemistry and Petrology, Geophysics
Link zum Portal
https://ucrisportal.univie.ac.at/de/publications/7956cd80-32d7-442b-840d-dc6032d2da2e