Dynamical Evolution of Planetary Systems
Antoine C. Petit, Gabriele Pichierri, Max Goldberg, Alessandro Morbidelli

TL;DR
This paper reviews how planetary systems evolve dynamically after formation, highlighting the processes that lead to their current orbital configurations through instabilities, resonances, and external influences.
Contribution
It synthesizes current understanding of post-formation dynamical evolution, emphasizing the importance of long-term processes in shaping planetary system architectures.
Findings
Resonant chains are common in young systems but often disrupted over time.
External perturbations like tides and stellar companions influence system stability.
The Solar System's current configuration reflects a history of resonant disruption and planetary impacts.
Abstract
Planetary systems can evolve dynamically even after the planets themselves have fully formed, and there is circumstantial evidence that most planetary systems become unstable after the disappearance of the gaseous protoplanetary disk. Theories of planet formation predict that chains of mean motion resonances are the natural outcome of disk-driven planet migration, leading to the pile up of super-Earths resonant chains close to the inner edge of the disk and the formation of fragile chains for distant giant planets. Observations of young systems suggest that they are more often locked in these chains than older ones, which are instead mostly non-resonant. The instabilities thought responsible for this trend can arise intrinsically if the original systems are too closely packed, or be due to external perturbations such as tides, planetesimal scattering, or torques from distant stellar…
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