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.
Some conditions where porosity is not modeled can result in negative values for masses in pore fluid salt or water content. These values should probably just be set to NaN when porosity is not modeled, or explicitly zeroed out.
Some conditions where porosity is not modeled can result in negative values for masses in pore fluid salt or water content. These values should probably just be set to NaN when porosity is not modeled, or explicitly zeroed out.