A Validated Low-to-Intermediate Mass Planetary Interior Structure Model and New Mass-Radius Relations
Bennett Neil Skinner, Ralph E. Pudritz, Ryan Cloutier

TL;DR
This paper introduces a comprehensive planetary interior structure model incorporating advanced physics, validated against known planetary data, and provides extensive mass-radius relations for various planet types, aiding interpretation of observational data.
Contribution
The authors develop a new, physics-rich interior structure model that accurately replicates planetary properties and generates extensive mass-radius relations for diverse exoplanet compositions.
Findings
Model replicates Earth's radius and inertia within 0.2%
Mass-radius relations are provided for planets from 0.01 to 100 Earth masses
Radii predictions differ from literature, highlighting the need for advanced models
Abstract
The increasing precision of planetary mass and radius observations is bringing major questions about the structure and formation of planets--such as the nature of the radius valley and origin of super-Mercuries--within reach, demanding the development of interior structure models with more physics to more accurately determine planetary radii for a given composition. Here, we present a new model that includes state-of-the-art equations of state following the latest experimental and computational results, a physically-motivated mineralogy allowing multiple species to coexist within planetary layers, a non-adiabatic temperature profile, melting, and other features. This model replicates Earth's radius and moment of inertia coefficient to within , Mars and the Moon's to within , and Mercury, Venus, and Europa's to within or 3. We use this model to calculate…
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