Uses the rheology traits from GeoParams to dispatch on specialized methods. This makes it trivial to avoid, e.g., updating the buoyancy forces or the viscosity within the PT iterations when any of those are constant through the pseudo-time steps.
Example in a 64 x 64 grid with three phases of constant density and viscosity:
Uses the rheology traits from
GeoParams
to dispatch on specialized methods. This makes it trivial to avoid, e.g., updating the buoyancy forces or the viscosity within the PT iterations when any of those are constant through the pseudo-time steps.Example in a
64 x 64
grid with three phases of constant density and viscosity: