Geothermal Doublet

Application ID: 29751

This is one of the two models from the blog post about heat transfer in the subsurface:

The animated gifs show the propagation 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:

Subsurface Flow Module