Disruption of co-orbital (1:1) planetary resonances during gas-driven orbital migration
Arnaud Pierens, Sean Raymond

TL;DR
This study demonstrates that gas-driven orbital migration in protoplanetary disks disrupts co-orbital planetary resonances, explaining the absence of observed co-orbital systems in Kepler data, especially for planets in the super-Earth to Saturn mass range.
Contribution
The paper reveals a mechanism by which co-orbital resonances are destabilized during migration due to gap formation, a novel insight into planetary system evolution.
Findings
Co-orbital systems are disrupted during large-scale migration.
Gap formation alters disk torques, breaking resonance.
Disruption occurs for planets with masses near the gap-opening threshold.
Abstract
Planets close to their stars are thought to form farther out and migrate inward due to angular momentum exchange with gaseous protoplanetary disks. This process can produce systems of planets in co-orbital (Trojan or 1:1) resonance, in which two planets share the same orbit, usually separated by 60 degrees. Co-orbital systems are detectable among the planetary systems found by the Kepler mission either directly or by transit timing variations. However, no co-orbital systems have been found within the thousands of Kepler planets and candidates. Here we study the orbital evolution of co-orbital planets embedded in a protoplanetary disk using a grid-based hydrodynamics code. We show that pairs of similar-mass planets in co-orbital resonance are disrupted during large-scale orbital migration. Destabilization occurs when one or both planets is near the critical mass needed to open a gap in…
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