Crystal structures and crystal chemical relationships of kröhnkite- and collinsite-type compounds Na2Me<sup>2+</sup>(XO<sub>4</sub>)<sub>2</sub> · 2 H<sub>2</sub>O (X = S, Me = Mn, Cd; and X = Se, Me = Mn, Co, Ni, Zn, Cd) and K<sub>2</sub>Co(SeO<sub>4</sub>)<sub>2</sub> · 2 H<sub>2</sub>O
- Autor(en)
- Manfred Wildner, Donka Stoilova
- Abstrakt
The crystal structures of eight compounds with compositions A2Me2+(XO4)2 · 2H2O (A = Na, X = S, Me2+ = Mn, Cd; A = Na, X = Se, Me2+ = Mn, Co, Ni, Zn, Cd; and A = K, X = Se, Me2+ = Co) were investigated using single crystal X-ray CCD diffraction data. The Mn- and Cd-compounds crystallize in the monoclinic kröhnkite structure type [Na2Cu(SO4)2 · 2 H2O, space group P21/c], the Co-, Ni-, and Zn-selenates in the closely related triclinic structure type of collinsite [Ca2Mg(PO4)2 · 2 H2O, space group P1̅]. Both types are built up from infinite Me(XO4)2(H2O)2 chains, composed of MeO4(H2O)2 octahedra alternating with each two XO4 tetrahedra by sharing corners. A—O bonds and hydrogen bonds link the chains to layers and further on to the three-dimensional structures. The influence of the ionic radii of the various A, Me, and X cations on the distances between these structural units is discussed. Special attention is paid to polyhedral distortions as well as to individual peculiarities of the alkaline coordinations and the hydrogen bonding systems. Thus, the crystal chemical relationships between the two structure types as well as to isotypic copper compounds, which are characterized by the strong octahedral Jahn-Teller distortions, are elucidated.
- Organisation(en)
- Institut für Mineralogie und Kristallographie
- Externe Organisation(en)
- Bulgarian Academy of Sciences (BAS)
- Journal
- Zeitschrift für Kristallographie : international journal for structural, physical, and chemical aspects of crystalline materials
- Band
- 218
- Seiten
- 201-209
- Anzahl der Seiten
- 9
- ISSN
- 0044-2968
- DOI
- https://doi.org/10.1524/zkri.218.3.201.20751
- Publikationsdatum
- 2003
- Peer-reviewed
- Ja
- ÖFOS 2012
- 1051 Geologie, Mineralogie
- Link zum Portal
- https://ucrisportal.univie.ac.at/de/publications/bb0ae771-91ae-487c-964c-2b23c081af1c