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Exoplanet Interior

Layered terrestrial planet under the constant-density approximation: an iron core, a silicate mantle, an optional water/ice layer, an optional H/He envelope, each at its characteristic density. Mass conservation fixes the interface radii, hydrostatic equilibrium gives a closed-form central pressure, and the mass-radius curve falls on the standard families (pure iron is the densest, an H/He envelope inflates the planet). The 3D cutaway shows the layered structure as the planet rotates; the side panels track the mass-radius position and the pressure profile from centre to surface.

Figure 1. Layered planet cutaway with the mass-radius curve and pressure profile.

WHAT TO TRY

  • Vary each control and watch the rail readouts respond.
  • Compare the diagnostic plot against the live scene.