Abstract

Single-crystal X-ray data were collected in steps of 25 °C up to 200 °C on a natural sample of zemannite, Mg0.5[ZnFe3+(TeO3)3]·4.5H2O. Ab initio simulations were performed to determine the hydrogen-bonding network to get better insight into the mechanism of the dehydration process.

At room temperature, zemannite is hexagonal with cell parameters a = 9.4301(12) Å, c = 7.6692(10) Å, V = 590.63(13) Å3. The structure was refined in the non-centrosymmetric space group P63, instead of P63/m. Ab initio simulations suggested an ordered Fe/Zn distribution at the octahedral sites that resulted in agreement with P63 symmetry.

The dehydration starts at 100 °C and proceeds with continuous loss of the non-Mg-bonded H2O up to 125 °C. At 150 °C, the interstitial water is lost leading to 3H2O pfu. The polyhedral framework does not undergo significant modifications. The unit-cell volume slightly decreases from 590.63(13) Å3 at room temperature to 577(2) Å3 at 200 °C.

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