Accurate prediction of the Effective Thermal Conductivity (ETC) of fluid-saturated consolidated rock is essential in geo-energy development and CCUS applications. The present empirical models are usually derived based on ideal or simplified geometries, and vary significantly on the prediction results. With help of digital rock technology, 3D matrix-pore integrated porous domains are reconstructed and the pore-scale numerical studies are carried out on the solid‒fluid coupled heat conduction processes. First, the methodology is validated on the basis of satisfactory agreements between the numerical and reported measurement ETC results for water-, oil- and air-saturated rock samples. Then, comprehensive simulation studies are performed at various rock porosities ranging from 14.5% to 27.2%, various matrix thermal conductivities ranging from 2.7 to 7.7 W/(m·K), and various saturated fluid types of water, hydrogen, oil and air. Evaluation of some classical empirical ETC models is performed, and the widely scattered model estimations, especially under high rock/fluid thermal conductivity ratio (ks/kf) conditions, demonstrates the key role of the precise description of the porous internal geometry on accurate ETC predictions. Finally, a new ETC model is proposed on the basis of the pore-scale numerical results. The new model shows a proper applicability across multiple fluid and rock types, covering a ks/kf range of 4.5-320.8.
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