Harnessing geothermal energy and storing carbon dioxide in volcanic systems require reliable constitutive models to predict rock deformation and failure under extreme pressure and temperature. However, existing models are limited, especially when compared to the more advanced predictive tools available for sedimentary rocks. In this study, we integrate elastoplasticity, strain hardening, nonassociative plasticity, phenomenological thermomechanics, and bifurcation analysis to establish a novel constitutive model for porous lava. The model is calibrated against a unique dataset that provides the stress–strain and strain localization responses of porous andesite deformed at temperatures ranging from room temperature up to 800 °C and at effective confining pressures from room pressure to 50 MPa. These mechanical and thermal conditions are representative of deep geothermal reservoirs. Finite element simulations of laboratory experiments are used to demonstrate the model’s capabilities in terms of reproducing key mechanical characteristics, including the differential stress required for the first stress drop and deformation mechanisms, across varying pressure and temperature conditions. Further validation via full-field finite element computations, simulating borehole excavation in low- to high-temperature systems, underscores the model’s predictive capabilities. In particular, the field-scale simulations demonstrate the model’s efficacy in reproducing variable forms of deformation structures and deformation modes around boreholes with capabilities to provide more information about the displacement in the borehole walls. The proposed modeling framework can be integrated into commercial numerical tools and used to facilitate the engineering of safe and cost-effective geothermal energy production and carbon geostorage, as well as numerical models designed to better understand the stability and therefore the hazard potential of volcanic structures.
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