Linking the primordial composition of planet building disks to the present-day composition of rocky exoplanets
V. Adibekyan, M. Deal, C. Dorn, I. Dittrich, B. M. T. B. Soares, S. G., Sousa, N. C. Santos, B. Bitsch, C. Mordasini, S. C. C. Barros, D. Bossini, T., L. Campante, E. Delgado Mena, O. D. S. Demangeon, P. Figueira, N. Moedas, Zh., Martirosyan, G. Israelian, and A. A. Hakobyan

TL;DR
This study links the primordial compositions of protoplanetary disks, inferred from host star abundances, to the resulting rocky planet compositions, revealing correlations and deviations that inform exoplanet characterization.
Contribution
It introduces a method combining stellar abundances and planetary interior models to estimate planet compositions and examines the variability and correlation of elemental ratios.
Findings
Strong correlation between disk iron-to-silicate mass fraction and planets.
No significant correlation between water mass fractions of disks and planets.
Fe/Mg ratio varies significantly, indicating disk-driven compositional diversity.
Abstract
The composition of rocky planets is strongly driven by the primordial materials in the protoplanetary disk, which can be inferred from the abundances of the host star. Understanding this compositional link is crucial for characterizing exoplanets. We aim to investigate the relationship between the compositions of low-mass planets and their host stars. We determined the primordial compositions of host stars using high-precision present-day stellar abundances and stellar evolutionary models. These primordial abundances were then input into a stoichiometric model to estimate the composition of planet-building blocks. Additionally, we employed a three-component planetary interior model (core, mantle, water in different phases) to estimate planetary compositions based only on their radius and mass. We found that although stellar abundances vary over time, relevant abundance ratios like Fe/Mg…
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