Japan Geoscience Union Meeting 2023

Presentation information

[J] Online Poster

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

[M-GI30] Computational sciences on the universe, galaxies, stars, planets, and their environments

Thu. May 25, 2023 10:45 AM - 12:15 PM Online Poster Zoom Room (25) (Online Poster)

convener:Yoshi-Yuki Hayashi(Department of Planetology/CPS, Graduate School of Science, Kobe University), Junichiro Makino(Kobe University), Eiichiro Kokubo(Division of Science, National Astronomical Observatory of Japan), Masaki Ogawa

On-site poster schedule(2023/5/26 17:15-18:45)

10:45 AM - 12:15 PM

[MGI30-P03] Development of simulation code for planetary system formation (GPLUM) : Prospects by high-resolution N-body simulation

*Yota Ishigaki1, Eiichiro Kokubo1, Masaki Fujimoto2, Junichiro Makino3,4 (1.National Institutes of Natural Sciences, National Astronomical Observatory of Japan, 2.Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, 3.Kobe University, 4.RIKEN Center for computational Science)

Keywords:Planet Formation, N-body Simulation

It is generally accepted that planetary systems are formed from protoplanetary disks surrounding a central star. In standard model, planets are formed by the accretion of planetesimals in the disk. The accretion process of planetesimals is mainly investigated using N-body simulations of planetesimal systems.

In this study, we have developed a new N-body simulation code, GPLUM, using the particle-particle particle-tree scheme (P3T scheme). We have implemented a more efficient algorithm than the conventional P3T code in GPLUM, which enables us to perform global, high-resolution N-body simulations. It is expected to enable new discussions such as parameter surveys using N-body simulations.

We present results of large-scale N-body simulations of the formation process of planetary systems by GPLUM using the supercomputer Fugaku. We discuss the resolution dependence of N-body simulations of the planet formation process by the high-resolution simulation. By comparing the results of N-body simulations with N=104, 105, and 106, we discuss how the accretion process of planetesimals and protoplanets is affected by changes in the resolution of N-body simulations.

We also discuss the dependence of the results of N-body simulations with new collision model, which is modeled SPH simulation. We discuss the dependence of the results of N-body simulations on the conditions of collisin of planetesimal systems. We will also present the future prospects of planet formation simulations using high-resolution N-body simulations with GPLUM and Fugaku.