Abstract
We use a coupled thermodynamically consistent framework to model reactive chemo-mechanical responses of solid solutions. Specifically, we focus on chemically active solid solutions that are subject to mechanical effects due to heterogeneous stress distributions. The stress generation process is driven solely by volume changes associated with the chemical processes. We use this model to describe the underlying physics during standard geological processes. Furthermore, simulation results of a three-species solid solution provide insights into the phenomena and verify the interleaving between mechanical and chemical responses in the solid. In particular, we show the evolution of the thermodynamic pressure as the system goes to a steady state.
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Acknowledgements
This publication was also made possible in part by the CSIRO Professorial Chair in Computational Geoscience at Curtin University and the Deep Earth Imaging Enterprise Future Science Platforms of the Commonwealth Scientific Industrial Research Organisation, CSIRO, of Australia. This project has received funding from the European Union’s Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No 777778 (MATHROCKS). The Institute for Geoscience Research (TIGeR) and the Curtin Institute for Computation kindly provide continuing support at Curtin University.
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Communicated by Andreas Öchsner.
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Clavijo, S.P., Espath, L. & Calo, V.M. The effects of chemical and mechanical interactions on the thermodynamic pressure for mineral solid solutions. Continuum Mech. Thermodyn. 35, 1821–1840 (2023). https://doi.org/10.1007/s00161-023-01200-4
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DOI: https://doi.org/10.1007/s00161-023-01200-4