N$`_2`$ is injected in an aquifer previously saturated with water with an injection rate of 0.0001 kg/(s*m$`^2`$).
The aquifer is situated 2700 m below sea level and the domain size is 60 m x 40 m. It consists of two layers, a moderately permeable one ($`\Omega_1`$) and a lower permeable one ($`\Omega_2`$).
@@ -93,6 +93,6 @@ make exercise1_2pni # builds new executable
__Initial conditions:__ The same temperature gradient as in the boundary conditions with an additional lens (with position: 20 < x < 30, 5 < y < 35), which has an initial temperature of 380 K.
The non-isothermal model requires additional parameters like the thermal conductivity of the solid component. They are already implemented and set in `exercise1.input`, you just need to _uncomment_ them.
