Geothermal Doublet

Application ID: 29751

This is one of the two models from the blog post about heat transfer in the subsurface: Coupling Heat Transfer with Subsurface Porous Media Flow

The animated GIFs show the propagation of an isothermal cold front (295 K) for different groundwater velocities caused by different horizontal hydraulic gradients (0, 1, 5 mm/m).

Note: Poroelasticity is not included here.

This model example illustrates applications of this type that would nominally be built using the following products: