Japan Geoscience Union Meeting 2024

Presentation information

[J] Poster

M (Multidisciplinary and Interdisciplinary) » M-GI General Geosciences, Information Geosciences & Simulations

[M-GI29] Computational sciences on the universe, galaxies, stars, planets and their environments

Wed. May 29, 2024 5:15 PM - 6:45 PM Poster Hall (Exhibition Hall 6, Makuhari Messe)

convener:Wataru Ohfuchi(Kobe University), Junichiro Makino(Kobe University), Masanori Kameyama(Geodynamics Research Center, Ehime University), Hideyuki Hotta(Nagoya University)

5:15 PM - 6:45 PM

[MGI29-P02] Planetesimal accretion in planetesimal rings

*Yuki Kambara1,2, Eiichiro Kokubo2,1 (1.Department of Astronomy, Graduate School of Science, The University of Tokyo, 2.Division of Science, National Astronomical Observatory of Japan)

Keywords:Planet formation, N-body simulation

In the standard planet formation scenario, planetesimals have been assumed to form throughout the protoplanetary disk and to be smoothly distributed in the radial direction except for the snowline. Recently, however, simulations of gas and dust evolution have shown that planetesimals form only in radially limited locations, such as gas pressure bumps and snowlines, and are concentrated in ring-like regions. On the other hand, simulations starting from protoplanets arranged in a narrow annulus successfully reproduced the mass distribution of terrestrial planets in the solar system. In addition, the existence of ring structures in the planet formation process has been supported by the observations of protoplanetary disks. The evolution process of planetesimals distributed in a ring is crucial to understanding planet formation theory. However, the evolution of planetesimal rings has not been studied in detail.
In this work, we investigate the evolution of planetesimal rings using N-body simulations. We systematically change the initial width and the total mass of planetesimal rings and investigate the dependence of protoplanet properties on the initial conditions. In all simulations, growing protoplanets start to scatter small planetesimals effectively. The ring width expands as protoplanets undergo oligarchic growth. In planetesimal rings, massive protoplanets tend to be formed around the ring center, while protoplanets far from the center of rings are less massive. Scaled orbital separation depends neither on the initial ring width nor the total mass and is consistent with the estimate in the oligarchic growth model. The width of the expanded planetesimal ring does not depend on the initial ring width but on the total ring mass. The maximum mass of protoplanets depends strongly on the total ring mass and weakly on the initial ring width. In the presentation, we discuss the physics of these dependencies in detail.