A pebbles accretion model with chemistry and implications for the solar system
Mohamad Ali-Dib

TL;DR
This paper presents a chemical accretion model for the formation of solar system giant planets, incorporating disk evolution, chemistry, and migration, to predict their atmospheric compositions and internal structures.
Contribution
It introduces a comprehensive formation model including chemistry and photoevaporation effects, providing new insights into giant planet compositions and core masses.
Findings
Jupiter and Saturn likely have small residual cores with significant heavy elements.
Oxygen and other element enrichments are predicted to be similar in both planets.
Models with disk photoevaporation better reproduce Jupiter's nitrogen abundance.
Abstract
We investigate the chemical composition of the solar system's giant planets atmospheres using a physical formation model with chemistry. The model incorporate disk evolution, pebbles and gas accretion, type I and II migration, simplified disk photoevaporation and solar system chemical measurements. We track the chemical compositions of the formed giant planets and compare them to the observed values. Two categories of models are studied: with and without disk chemical enrichment via photoevaporation. Predictions for the Oxygen and Nitrogen abundances, core masses, and total amount of heavy elements for the planets are made for each case. We find that in the case without disk PE, both Jupiter and Saturn will have a small residual core and comparable total amounts of heavy elements in the envelopes. We predict oxygen abundances enrichments in the same order as carbon, phosphorus and…
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