Hot super-Earths and giant planet cores from different migration histories
Christophe Cossou, Sean N. Raymond, Franck Hersant, Arnaud Pierens

TL;DR
This paper presents a model explaining how planetary embryos' migration histories in protoplanetary disks determine whether they become hot super-Earths or giant planet cores, supported by simulations matching observed exoplanet properties.
Contribution
It introduces a new migration-based framework for planetary formation, linking embryo migration paths to final planetary types and reproducing observed exoplanet distributions.
Findings
Hot super-Earths form in resonant chains near the disk edge.
Giant planet cores migrate outward and are stranded at 1-5 AU.
Giant planet core frequency correlates with solid mass, matching metallicity trends.
Abstract
Planetary embryos embedded in gaseous protoplanetary disks undergo Type I orbital migration. Migration can be inward or outward depending on the local disk properties but, in general, only planets more massive than several can migrate outward. Here we propose that an embryo's migration history determines whether it becomes a hot super-Earth or the core of a giant planet. Systems of hot super-Earths (or mini-Neptunes) form when embryos migrate inward and pile up at the inner edge of the disk. Giant planet cores form when inward-migrating embryos become massive enough to switch direction and migrate outward. We present simulations of this process using a modified N-body code, starting from a swarm of planetary embryos. Systems of hot super-Earths form in resonant chains with the innermost planet at or interior to the disk inner edge. Resonant chains are disrupted by late…
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