The Dynamical Fate of Self-Gravitating Disc Fragments After Tidal Downsizing
Duncan Forgan, Richard Parker, Ken Rice

TL;DR
This study investigates the long-term dynamical evolution of self-gravitating disc fragments, showing that scattering and cluster interactions can produce free-floating substellar objects, with implications for understanding planet and brown dwarf populations.
Contribution
It provides the first detailed N-body simulations of post-formation dynamical evolution of disc fragments in various environments, linking formation models to observed free-floating objects.
Findings
25% ejection rate of fragments due to scattering
Ejecta velocity dispersion matches hydrodynamic simulations
13% of objects ejected from planetary systems in clusters
Abstract
The gravitational instability model of planet/brown dwarf formation proposes that protostellar discs can fragment into objects with masses above a few Jupiter masses at large semimajor axis. Tidal downsizing may reduce both the object mass and semimajor axis. However, most studies of tidal downsizing end when the protostellar disc disperses, while the system is embedded in its parent star-forming region. To compare disc fragment descendants with exoplanet and brown dwarf observations, the subsequent dynamical evolution must be explored. We carry out N-Body integrations of fragment-fragment scattering in multi-object star systems, and star systems embedded in substructured clusters. In both cases, we use initial conditions generated by population synthesis models of tidal downsizing. The scattering simulations produce a wide range of eccentricities. The ejection rate is around 25%.…
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