Heat Transfer Modeling in Enhanced Geothermal Energy: A Three-Temperature Approach for Solid, Injected, and Residing Fluids
Yi-Yung Yang, Sanghyun Lee, Dmitri Kuzmin

TL;DR
This paper introduces a three-temperature LTNE model for enhanced geothermal systems, explicitly tracking injected fluid temperature to improve thermal predictions in fractured reservoirs.
Contribution
It develops a novel three-way LTNE coupling framework with an enriched Galerkin method and flux-corrected transport to accurately model heat transfer in EGS.
Findings
Captures injected-fluid heating paths more accurately.
Predicts thermal breakthrough behavior beyond standard models.
Demonstrates effectiveness in fractured EGS simulations.
Abstract
Enhanced geothermal systems (EGS) involve strongly coupled, advection-dominated flow and heat transfer in fractured porous media. Conventional models typically assume local thermal equilibrium with a single effective fluid temperature or, at best, an averaged pore-fluid temperature, so the thermal evolution of injected cold fluid is only inferred indirectly. In this work, we develop a local thermal non-equilibrium (LTNE) model that explicitly resolves the temperature of injected fluid as it moves through the reservoir and exchanges heat with the hot rock and resident fluid. The key ingredient is a concentration variable that tracks the injected fluid and induces a three-way LTNE coupling among rock, resident-fluid, and injected-fluid temperatures. This framework distinguishes, at the continuum scale, how newly injected fluid parcels are heated by conductive and convective exchange, and…
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