A bond-based peridynamics formulation is developed and verified for modeling pressure-driven water flow with phase change and heat transfer in saturated porous media.
Modeling of groundwater flow at depth in crystalline rock beneath a moving ice-sheet margin, exemplified by the Fennoscandian Shield, Sweden
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Analysis of heat transfer and water flow with phase change in saturated porous media by bond-based peridynamics
A bond-based peridynamics formulation is developed and verified for modeling pressure-driven water flow with phase change and heat transfer in saturated porous media.