Vibrational entropy of disordering in omphacite

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Abstract

The cations of an ordered omphacite from the Tauern window were gradually disordered in piston cylinder experiments at temperatures between 850 and 1150 °C. The samples were examined by X-ray powder diffraction and then investigated using low-temperature calorimetry and IR spectroscopy. The low-temperature heat capacity data were used to obtain the vibrational entropies, and the line broadening of the IR spectra served as a tool to investigate the disordering enthalpy. These data were then used to calculate the configurational entropy as a function of temperature. The vibrational entropy does not change during the cation ordering phase transition from space group C2/c to P2/n at 865 °C but increases with a further temperature increase due to the reduction of short-range order.

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Benisek, A., Dachs, E., Carpenter, M. A., Joachim-Mrosko, B., Vielreicher, N. M., & Wildner, M. (2023). Vibrational entropy of disordering in omphacite. Physics and Chemistry of Minerals, 50(4). https://doi.org/10.1007/s00269-023-01260-7

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