• A general imperfect thermal contact model and a general imperfect flow contact model are developed to capture interfacial resistance in multilayered saturated soils.
• Thermal contact resistance induces a relative thermal gradient at the interface, increasing pore water pressure and reducing displacement near the interface.
• Flow contact resistance generates a relative pore pressure gradient, enhancing displacement in the saturated soil while having minimal impact on temperature distribution.
• The proposed analytical solutions, validated against degeneration solutions, provide a robust tool for predicting thermal consolidation behavior under ramp-type heating.
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