Investigating the Formation of Planets Interior to in situ Hot Jupiters
Devansh Mathur, Juliette Becker
TL;DR
This study tests the feasibility of forming hot Jupiters and their interior companions in situ during the gas-free, late-stage phase of planetary systems. Using REBOUND TRACE to run 159 simulations with 30 interior embryos across a range of solid-surface densities, the authors find that higher embryo densities produce more massive interior planets (up to ~$10\ M_\oplus$) and that about $75$–$80\%$ of the initial solid mass remains in planets after 1 Myr. A second suite varying the hot Jupiter's semi-major axis shows that closer-in giants drive more embryo-embryo mergers, while more distant giants lead to less dramatic growth; overall, the giant's position modulates outcomes but disk density dominates. The results imply that in situ formation is a viable pathway for some hot Jupiter systems with interior companions, but the mechanism cannot explain the full diversity of observed architectures and must be integrated with migration dynamics and long-term dynamical evolution in future work.
Abstract
The population of hot Jupiters with adjacent planetary companions is small but growing, and inner companions appear to be a nearly ubiquitous outcome within this subset of the exoplanet census. While most hot Jupiters are believed to form via tidal migration, the presence of adjacent companions is not easily explained by this formation mechanism, requiring consideration of additional formation mechanisms such as disk migration and in situ formation. In this work, we explore the possibility of in situ formation for both hot Jupiters and their interior companions. Using numerical simulations performed with the N-body integrator REBOUND, we investigate the growth of interior companions under various assumptions about disk conditions and hot Jupiter final orbital positions. Our results show that if a sufficiently high density of planetary embryos is transported to short orbital radii, it is feasible for both hot Jupiters and their interior companions to form in situ, providing a viable explanation for a subset of observed planetary architectures.
