The Great Inequality and the Dynamical Disintegration of the Outer Solar System
Jon K. Zink, Konstantin Batygin, and Fred C. Adams

TL;DR
This study uses N-body simulations to explore the long-term dynamical evolution and eventual disintegration of the outer solar system after the Sun's stellar evolution, revealing a timescale of about 100 billion years for complete dissolution.
Contribution
It provides a detailed dynamical model of the outer solar system's evolution post-stellar mass loss, highlighting the role of mean-motion resonances and stellar encounters in system disintegration.
Findings
The outer planets' orbits expand due to solar mass loss.
Resonance capture leads to increased system instability.
Complete system dissolution occurs in roughly 100 billion years.
Abstract
Using an ensemble of N-body simulations, this paper considers the fate of the outer gas giants (Jupiter, Saturn, Uranus, and Neptune) after the Sun leaves the main sequence and completes its stellar evolution. Due to solar mass-loss -- which is expected to remove roughly half of the star's mass -- the orbits of the giant planets expand. This adiabatic process maintains the orbital period ratios, but the mutual interactions between planets and the width of mean-motion resonances (MMR) increase, leading to the capture of Jupiter and Saturn into a stable 5:2 resonant configuration. The expanded orbits, coupled with the large-amplitude librations of the critical MMR angle, make the system more susceptible to perturbations from stellar flyby interactions. Accordingly, within about 30 Gyr, stellar encounters perturb the planets onto the chaotic sub-domain of the 5:2 resonance, triggering a…
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