Japan Geoscience Union Meeting 2024

Presentation information

[J] Oral

P (Space and Planetary Sciences ) » P-PS Planetary Sciences

[P-PS07] Planetary Sciences

Fri. May 31, 2024 10:45 AM - 12:00 PM 102 (International Conference Hall, Makuhari Messe)

convener:Sota Arakawa(Japan Agency for Marine-Earth Science and Technology), Haruhisa Tabata(Department of Earth and Planetary Science, University of Tokyo), Ryosuke Tominaga(School of Science, Department of Earth and Planetary Sciences, Tokyo Institute of Technology), Chairperson:Yukihiko Hasegawa(Tohoku University), Sota Arakawa(Japan Agency for Marine-Earth Science and Technology), Ryosuke Tominaga(Star and Planet Formation Laboratory, RIKEN Cluster for Pioneering Research), Haruhisa Tabata(Department of Earth and Planetary Science, University of Tokyo)

11:45 AM - 12:00 PM

[PPS07-10] Global N-body Simulation of Gap Edge Structures Created by Perturbations from a Small Satellite Embedded in Saturn’s Rings

*Naoya Torii1, Shigeru Ida1, Eiichiro Kokubo2, Shugo Michikoshi3 (1.Tokyo Institute of Technology, 2.National Astronomical Observatory of Japan, 3.Kyoto Women's University)

Keywords:Saturn's ring, Saturn's satellite, N-body simulation

Small satellites embedded in Saturn's ring - Daphnis and Pan - open a clear gap. Observations by the Voyager and Cassini spacecrafts have revealed various striking features of the gap structure, such as the density waves, sharp edge, and vertical wall structure. In order to explain these features in a single simulation, we perform a high-resolution (N~10^6-10^7) global full N-body simulation of gap formation by an embedded satellite considering gravitational interactions and inelastic collisions among all ring particles and the satellite, while these features have been mostly investigated separately with different theoretical approaches: the streamline models, 1D diffusion models, and local N-body simulation. As a first attempt of a series of papers, we here focus on the gap formation by separating satellite migration with fixing the satellite orbit in a Keplerian circular orbit.

We reveal how the striking gap features - the density waves, sharp edge, and vertical wall structure - are simultaneously formed by an interplay of the satellite-ring and ring particle-particle interactions. In particular, we propose a new mechanism to quantitatively explain the creation of the vertical wall structure at the gap edge. Inelastic collisions between ring particles damp their eccentricity excited by the satellite's perturbations to enhance the surface density at the gap edge, making its sharp edges more pronounced. We find the eccentricity damping process inevitably raises the vertical wall structures the most effectively in the second epicycle waves. Particle-particle collisions generally convert their lateral epicyclic motion into vertical motion. Because the excited epicyclic motion is the greatest near the ring edge and the epicycle motions are aligned in the first waves, the conversion is the most efficient in the gap edge of the second waves and the wall height is scaled by the satellite Hill radius, which are consistent with the observations.