Geothermal energy is a clean and sustainable alternative energy, and enhanced geothermal systems are an essential technology offering an industrial-scale method to tap geothermal energy. This technology stimulates numerous reservoir fractures, creating primary flow channels for fluids to extract heat. The important question of how the permeability of fracture swarm evolves during fluid circulation and how this evolution potentially affects the geothermal system life remains to be further answered. To address this, we develop and validate a fully coupled thermo-hydro-mechanical model based on the discrete fracture network. Results show a positive feedback mechanism between pore pressure/temperature changes and fracture permeability evolution, leading to monotone permeability-increasing in a limited number of specific fractures, indicating uneven permeability evolution of fracture swarm is crucial in shortening reservoir lifetime. Furthermore, we conduct a comparative analysis of multiple factors to determine what most significantly affects reservoir lifetime, including fracture heterogeneity, the local thermal non-equilibrium effect, and layout strategies. Results indicate the strong heterogeneity of the fracture network is dominant, and the inherent heterogeneity of hydraulic fractures is further exacerbated during geothermal production. Neglecting fractures’ mechanical response leads to an overestimated outcome. A simplified thermal-hydraulic analysis indicates a 34 % higher temperature and a 6 % higher heat extraction rate than the coupled thermo-hydro-mechanical modeling. In contrast, the impact of the local thermal non-equilibrium effect is negligible, with comparable results between equilibrium and non-equilibrium models. We further find the multi-well layout can effectively suppress the heterogeneity impact and prevent preferential flow paths. Compared to dual-well systems, the multi-well scheme has a 24 % higher temperature and a 6 % higher heat extraction rate.
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