Construct 1D interior structure models based on planetary properties. Self-consistent thermodynamics are used for fluid, rock, and mineral phases. Sound speeds, attenuation, and electrical conductivities are computed as outputs.
According to Vance et al. 2018, inside the silicate layer, gravity is set to one mean value, and in the core, gravity is set to zero. This seems to be born out by output plots of the gravitational acceleration.
There appears to be commented lines propagating g to the deeper layers. This seems like a beneficial feature for profiles considering the deeper interior.
According to Vance et al. 2018, inside the silicate layer, gravity is set to one mean value, and in the core, gravity is set to zero. This seems to be born out by output plots of the gravitational acceleration.
g(r) is calculated within the ice and ocean layers here: https://github.com/vancesteven/PlanetProfile/blob/b751522098010750f25da8fcc4472169e1203468/PlanetProfile.m#L177
There appears to be commented lines propagating g to the deeper layers. This seems like a beneficial feature for profiles considering the deeper interior.