Ejected Surface Regolith as a Potential Source Material for Centaur Rings

Ring systems have been observed around Centaur Chariklo (10199) and other small bodies but their origin and dynamical histories are still debated. These small body ring systems challenge conventional models for the origin of planetary rings, especially when considering Centaurs' often erratic cometary activity, their non-spherical shapes, and their relatively short dynamical lifetimes (~$10^7$ years). A collisional origin for these rings is disfavored based on the low probability of collisions within their lifetimes, and so their mechanism of formation remains an open question. In this work, we use Swiftest, a N-body integrator with collisional fragmentation and higher-order gravitational harmonics, to test a hypothesis that rings could be formed from regolith ejected from a cometary outburst that is subsequently captured into a stable orbit. We show that ejected surface regolith is captured in orbit around ellipsoidal Centaurs like Chariklo and Chiron to form a proto-ring disk for at least 100 rotations. This captured disk may serve as a starting point that can evolve into observed ring systems. Inter-particle collisions and the ellipsoidal gravity field facilitate this capture. Among the tested scenarios, a landslide or avalanche-like ejection from the equatorial plane shows the highest rate of capture, ~30 - 90% depending on the initial ejection parameters. This implies that rings could be an indicator of past activity on a Centaur and may be a more common feature among Centaurs depending on their shape and frequency of outbursts.