Abstract
Muscovite (Ms) and phlogopite (Phl) belong to the 2:1 dioctahedral and trioctahedral layer silicates, respectively, and are the end members of Ms-Phl series minerals. This series was studied in the 2M1 polytype and modeled by the substitution of three Mg2+ cations in the Phl octahedral sites by two Al3+ and one vacancy, increasing the substitution up to reach the Ms. The series was computationally examined at DFT level as a function of pressure to 9 GPa. Cell parameters as a function of pressure and composition, and bulk moduli as a function of the composition agrees with the existing experimental results. The mixing Gibbs free energy was calculated as a function of composition. From these data, approximated solvi were calculated at increasing pressure. A gap of solubility is found, decreasing the gap of solubility at high pressure.
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Acknowledgements
The authors thank the “Centro de Supercomputación de Galicia” (CESGA) and “Centro de Servicios de Informática y Redes de Comunicaciones (CSIRC), Universidad de Granada” for providing the computing time. The authors are thankful to F. Muñoz-Izquierdo, J. Rodríguez-Fernández, and M. Mookherjee for fruitful suggestions. This work was supported by Spanish MCINN and European FEDER grants CGL2008-02850/BTE, FIS2013-48444-C2-2P, FIS2016-77692-C2-2P, and PCIN-2017-098 and by the regional agency “Junta de Andalucía” for the RNM-264, -363, and -1897 PAI-grants.
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Hernández-Laguna, A., Pérez del Valle, C., Hernández-Haro, N. et al. Compressibility of 2M1 muscovite-phlogopite series minerals. J Mol Model 25, 341 (2019). https://doi.org/10.1007/s00894-019-4218-x
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DOI: https://doi.org/10.1007/s00894-019-4218-x