Redetermination and new description of the crystal structure of vanthoffite, Na6Mg(SO4)4

Acta Crystallographica Section E: Crystallographic Communications

Fabrizio Nestola¹  Martha G. Pamato¹  Tonči Balić-Žunić² 

[1] Department of Geosciences, University of Padova, Italy;University of Copenhagen, Department of Geosciences, Denmark;

关键词: crystal structure;    vanthoffite;    na-mg sulfate;    atomic coordinations;    redetermination;   

DOI  :  10.1107/S2056989020005873

来源: DOAJ

【 摘 要 】

The crystal structure of vanthoffite {hexasodium magnesium tetrakis[sulfate(VI)]}, Na6Mg(SO4)4, was solved in the year 1964 on a synthetic sample [Fischer & Hellner (1964). Acta Cryst. 17, 1613]. Here we report a redetermination of its crystal structure on a mineral sample with improved precision. It was refined in the space group P21/c from a crystal originating from Surtsey, Iceland. The unique Mg (site symmetry \overline{1}) and the two S atoms are in usual, only slightly distorted octahedral and tetrahedral coordinations, respectively. The three independent Na atoms are in a distorted octahedral coordination (1×) and distorted 7-coordinations intermediate between a `split octahedron' and a pentagonal bipyramid (2×). [MgO6] coordination polyhedra interchange with one half of the sulfate tetrahedra in <011> chains forming a (100) meshed layer, with dimers formed by edge-sharing [NaO7] polyhedra filling the interchain spaces. The other [NaO7] polyhedra are organized in a parallel layer formed by [010] and [001] chains united through edge sharing and bonds to the remaining half of sulfate groups and to [NaO6] octahedra. The two types of layers interconnect through tight bonding, which explains the lack of morphological characteristics typical of layered structures.

【 授权许可】

Unknown