Enhanced constraints on the interior composition and structure of terrestrial exoplanets
Haiyang S. Wang, Fan Liu, Trevor R. Ireland, Ramon Brasser, David, Yong, Charles H. Lineweaver

TL;DR
This paper improves exoplanet interior models by accounting for devolatilized stellar abundances and core composition constraints, enabling more accurate assessments of terrestrial exoplanets' similarity to Earth.
Contribution
It introduces an extended chemical network for planetary cores and applies it to both the Earth and exoplanet host stars, refining interior composition predictions.
Findings
Model reproduces Earth's core and mantle composition.
Identifies Kepler-21 as hosting the most Earth-like planet.
Stresses the need for high-precision stellar abundances (<0.04 dex) for accurate comparisons.
Abstract
Exoplanet interior modelling usually makes the assumption that the elemental abundances of a planet are identical to those of its host star. Host stellar abundances are good proxies of planetary abundances, but only for refractory elements. This is particularly true for terrestrial planets, as evidenced by the relative differences in bulk chemical composition between the Sun and the Earth and other inner solar system bodies. The elemental abundances of a planet host star must therefore be devolatilised in order to correctly represent the bulk chemical composition of its terrestrial planets. Furthermore, nickel and light elements make an important contribution alongside iron to the core of terrestrial planets. We therefore adopt an extended chemical network of the core, constrained by an Fe/Ni ratio of 18 4 (by number). By applying these constraints to the Sun, our modelling…
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