Abstract

Crystals of the hydrous magnesium orthotellurate(VI) Mg(H2O)2[TeO2(OH)4] were grown by slow diffusion of an aqueous MgCl2 solution into a KOH/Te(OH)6 solution immobilized in gelatin. The crystal structure is built of sheets of nearly regular corner-sharing [MgO6] and [TeO6] octahedra. Half of the bridging O atoms are connected to disordered H atoms, which are located in rhomboidal voids (long and short diameters of ∼5.0 and ∼2.5 Å, respectively) of these layers. Moreover, the TeVI atom connects to two OH− ions and the MgII atom to two H2O molecules. The OH− ions and H2O molecules connect adjacent layers forming a disordered hydrogen-bonding network. In a given layer, an adjacent layer may be positioned in four ways, which can be characterized by one of two origin shifts and one of two orientations with respect to [100]. The crystals feature a disordered stacking arrangement, leading to rods of diffuse scattering in the diffraction pattern. The polytypism is explained by application of the order–disorder (OD) theory. Different refinement models are compared and the diffuse scattering is evaluated with structure factor calculations. The correlation coefficient of subsequent origin shifts is ∼ −0.33, whereas the orientation of the layers is essentially random. Determining the latter is particularly difficult owing to a small contribution to the diffraction pattern and virtually indistinguishable diffraction patterns for pairs of correlations with the same absolute value. On longer standing in a glass vial, an ordered polytype forms.

Highlights

  • Orthotellurates(VI) of alkaline earth metals with general formula M2M0[TeVIO6] bear interesting crystal-chemical and physico-chemical aspects, and a number of these phases and their solid solutions are structurally well characterized (Prior et al, 2005; Fu et al, 2008)

  • The crucial point in an OD description is that pairs of adjacent layers are equivalent, which corresponds to the vicinity condition (VC)

  • The correlated disorder of Mg(H2O)2[TeO2(OH)4] is notable because it can be decomposed into two modes, which can be treated separately

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Summary

Introduction

Orthotellurates(VI) of alkaline earth metals with general formula M2M0[TeVIO6] bear interesting crystal-chemical and physico-chemical aspects, and a number of these phases and their solid solutions are structurally well characterized (Prior et al, 2005; Fu et al, 2008). The structures of most alkaline earth metal tellurates (except Be) with a single MII cation and the general formula M3II[TeVIO6] have been elucidated [M = Mg: Schulz & Bayer (1971); M = Ca: Hottentot & Loopstra (1981); M = Sr, Ba: Stoger et al (2010)]. The structures of these tellurates are characterized by rigid, practically regular, octahedral [TeO6]6À units.

Synthesis and crystal growth
Data collection
Refinement
Thermal analysis
Calculation of diffuse scattering
Crystal chemistry
Polytypism
Order–disorder description
Maximum degree of order polytypes
Family structure
Diffraction pattern
Rods with insignificant contribution of O3
Classical refinements
Disorder model
3.10. Diffuse scattering
3.11. Estimation of the correlation coefficients
3.13. Rearrangement of the crystal structure over time
3.14. Thermal behavior
Conclusion and outlook
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