On the Formation and Chemical Composition of Super Earths
Matthew Alessi, Ralph E. Pudritz, and Alex J. Cridland

TL;DR
This paper presents a model combining disk chemistry and core accretion to explain the formation and diverse compositions of super Earths, emphasizing the role of disk inhomogeneities called traps.
Contribution
It introduces a new integrated model that links disk chemistry, planet traps, and accretion processes to explain super Earth diversity.
Findings
Super Earth compositions vary from dry to water-rich.
Disk lifetime influences planet type, with short-lived disks favoring super Earths.
Disk traps determine planet formation locations and compositions.
Abstract
Super Earths are the largest population of exoplanets and are seen to exhibit a rich diversity of compositions as inferred through their mean densities. Here we present a model that combines equilibrium chemistry in evolving disks with core accretion that tracks materials accreted onto planets during their formation. In doing so, we aim to explain why super Earths form so frequently and how they acquire such a diverse range of compositions. A key feature of our model is disk inhomogeneities, or planet traps, that act as barriers to rapid type-I migration. The traps we include are the dead zone, which can be caused by either cosmic ray or X-ray ionization, the ice line, and the heat transition. We find that in disks with sufficiently long lifetimes ( 4 Myr), all traps produce Jovian planets. In these disks, planet formation in the heat transition and X-ray dead zone produces hot…
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