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American Mineralogist; January; v. 94; no. 1; p. 74-82; DOI: 10.2138/am.2009.2898
© 2009 Mineralogical Society of America
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Structural features in Tutton’s salts K2[M2+(H2O)6](SO4)2, with M2+ = Mg, Fe, Co, Ni, Cu, and Zn

Ferdinando Bosi1,2,*, Girolamo Belardi3 and Paolo Ballirano1,3

1 Dipartimento di Scienze della Terra, Università di Roma "La Sapienza," Piazzale Aldo.Moro 5, 00185 Roma, Italy
2 Department of Mineralogy, Swedish Museum of Natural History, Box 50007, 10405 Stockholm, Sweden
3 CNR-IGAG Istituto di Geologia Ambientale e Geoingegneria, Sede di Roma, Via Bolognola 7, 00138 Roma, Italy

Correspondence: * E-mail: ferdinando.bosi{at}uniroma1.it

The crystal chemistry of six crystals of general formula K2[M2+ (H2O)6](SO4)2, with M2+ = Mg, Fe, Co, Ni, Cu, and Zn, was investigated by single-crystal structure analysis to determine the effects of the chemical variation of M2+ on the structural environment surrounding K, M, and S sites. Results indicate that the distortion in the SO4 tetrahedron and the MO6 octahedron is very small, except for CuO6 where it is pronounced because of the Jahn-Teller effect. The KO8-octacoordinate polyhedron has the highest degree of distortion, and its idealized shape may be referred to as a bicapped trigonal prism. The SO4 size is not affected by changes in cation occupancies at the adjacent M site. In contrast, changes in the KO8 size, which are accompanied by changes in the bond valence sum at K, depend on interaction with the first and second coordination sphere of M. This interaction results by changes in M-O individual lengths, by expansion of the second coordination sphere of M, and by changes in the distribution of the bond strengths over the O atoms coordinated to K. The MO6 size follows the expected trend from the increased ionic radius at the M site. The latter is also correlated with the unit-cell volume except for the Cu- and Mg-phase, which show a larger cell volume with respect to that expected. Although the relevant octahedral distortion around the Cu2+ cation explains the volume excess in the Cu-phase, an expansion of the second coordination sphere of Mg2+, compared to those of cations of larger ionic radius (such as Zn and Co), explains the excess of the unit-cell volume in the Mg-phase. As the CuO6 distortion can be caused by the Jahn-Teller effect, the higher ionicity of the Mg atom could be the cause for its anomalous behavior observed in Tutton’s salts. This stereochemical behavior of the Mg atom seems to be consistent with the weakening of the hydrogen bonds in the structure connected to differences in the bonding character of Mg and transition metals when coordinated by water molecules.

Key Words: Crystal synthesis • Tutton’s salts • crystal structure • bond valence




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