On the formation of planetary systems via oligarchic growth in thermally evolving viscous discs
Gavin A. L. Coleman, Richard P. Nelson

TL;DR
This study uses advanced N-body simulations to explore planetary system formation via oligarchic growth in thermally evolving viscous discs, revealing challenges in forming gas giants due to rapid inward migration.
Contribution
It demonstrates that current models struggle to produce gas giants, highlighting the impact of migration prescriptions and disc evolution on planet formation outcomes.
Findings
Low mass discs form close-packed terrestrial planets.
Higher mass discs produce multiple planetary generations.
Gas giants are rarely formed due to rapid inward migration.
Abstract
We present N-body simulations of planetary system formation in thermally-evolving, viscous disc models. The simulations incorporate type I migration (including corotation torques and their saturation), gap formation, type II migration, gas accretion onto planetary cores, and gas disc dispersal through photoevaporation. The aim is to examine whether or not the oligarchic growth scenario, when combined with self-consistent disc models and up-to-date prescriptions for disc-driven migration, can produce planetary systems similar to those that have been observed. The results correlate with the initial disc mass. Low mass discs form close-packed systems of terrestrial-mass planets and super-Earths. Higher mass discs form multiple generations of planets, with masses in the range 10 < mp < 45M_Earth. These planets generally type I migrate into the inner disc, because of corotation torque…
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