期刊
MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
卷 506, 期 4, 页码 5093-5107出版社
OXFORD UNIV PRESS
DOI: 10.1093/mnras/stab1733
关键词
planets and satellites: dynamical evolution and stability; planetary systems
资金
- Fapesp [2020/06807-7]
This work examines the orbital evolution and dynamical stability near the small Saturnian moons Aegaeon, Methone, Anthe, and Pallene. Results show that for massless small moons, orbiting particles remain stable for at least 10(4) yr, while massive bodies cause significant perturbations and destabilization of particle orbits. Initial arcs around the moons are eroded within hundreds of years, providing insights into gravitational forces' time-scales for removing particles.
In this work we analyse the orbital evolution and dynamical stability in the vicinity of the small Saturnian moons Aegaeon, Methone, Anthe, and Pallene. We numerically resolve the exact equations of motions to investigate the orbital motion of thousands of test particles within and near the domain of the 7/6, 14/15, 10/11 mean-motion resonances of Aegaeon, Methone, and Anthe with Mimas, respectively. We show that, for massless small moons, the orbits of particles initially restricted to the resonant domains remain stable for at least 10(4) yr. We also conduct numerical simulations considering Aegaeon, Methone, Anthe, and Pallene as massive bodies. The results show that most particles undergo significant perturbations in their orbital motions, ultimately destabilizing on time-scales of a few hundreds of years or even less through collisions with the four small moons. In addition, we also simulate the orbital evolution of test particles initially distributed in the form of arcs around Aegaeon, Methone, and Anthe. We show that the initial arcs are dynamically eroded on time-scales of hundreds of years, allowing us to constrain the time-scales on which gravitational forces operate to remove particles from the observed arcs.
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