Building Giant-Planet Cores at a Planet Trap
Alessandro Morbidelli (OCA), Aurelien Crida, Frederic Masset, Richard, P. Nelson

TL;DR
This study investigates how planet traps at disk density gradients influence the formation and stability of multiple planetary cores, revealing that such traps can lead to stable configurations or cause embryo loss through scattering and migration.
Contribution
The paper demonstrates through hydrodynamical simulations that planet traps can stabilize multiple planetary embryos and explains the limited number of giant planets in our solar system.
Findings
Stable, separated, non-migrating orbits form with embryo at the trap.
Multiple embryos are inherently unstable and can lead to collisions.
System stability increases as the number of embryos decreases to 2-4.
Abstract
A well-known bottleneck for the core-accretion model of giant-planet formation is the loss of the cores into the star by Type-I migration, due to the tidal interactions with the gas disk. It has been shown that a steep surface-density gradient in the disk, such as the one expected at the boundary between an active and a dead zone, acts as a planet trap and prevents isolated cores from migrating down to the central star. We study the relevance of the planet trap concept for the accretion and evolution of systems of multiple planetary embryos/cores. We performed hydrodynamical simulations of the evolution of systems of multiple massive objects in the vicinity of a planet trap. The planetary embryos evolve in 3 dimensions, whereas the disk is modeled with a 2D grid. Synthetic forces are applied onto the embryos to mimic the damping effect that the disk has on their inclinations. Systems…
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Taxonomy
TopicsAstrophysics and Star Formation Studies · Astronomy and Astrophysical Research · Stellar, planetary, and galactic studies
