Super-Earth formation with slow migration from a ring in an evolving peaked disk compatible with terrestrial planet formation
Masahiro Ogihara, Alessandro Morbidelli, Masanobu Kunitomo

TL;DR
This study explores planet formation from rings in evolving disks, showing that low-mass planets remain near 1 au while more massive ones migrate inward, reproducing solar system and super-Earth system features.
Contribution
It demonstrates a unified disk model that explains both terrestrial and super-Earth planet formation through different migration behaviors within a single framework.
Findings
Low-mass planets (<1 Earth mass) stay near 1 au without migrating inward.
More massive planets (>1 Earth mass) slowly migrate inward, reaching about 10-day orbits.
The model reproduces observed properties of the solar system and super-Earth systems.
Abstract
For the origin of the radially concentrated solar system's terrestrial planets, planet formation from a ring of solids at about 1 au from the Sun with convergent/suppressed type I migration is preferred. On the other hand, many super-Earths and sub-Neptunes are found in the close-in region with orbital periods of 10-100 days, so that planet formation from rings in the 1-au region would require some degree of inward migration. One way to realize these different formation scenarios is to use different gas disk models. In this study we investigate whether different scenarios can be realized within a single framework. We consider a disk model that evolves via disk winds and develops a density peak, and study planet formation and orbital evolution using N-body simulations. Planets with masses less than an Earth mass formed from a low-mass ring resembling the solar system do not migrate…
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Taxonomy
TopicsAstro and Planetary Science · High-pressure geophysics and materials · Methane Hydrates and Related Phenomena
