Geothermal Doublet

Application ID: 29751


This is one of the two models from the blog post about heat transfer in the subsurface: https://www.comsol.de/blogs/coupling-heat-transfer-subsurface-porous-media-flow/

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