Article, 2024

How the presence of a giant planet affects the outcome of terrestrial planet formation simulations

Astronomy & Astrophysics, ISSN 0004-6361, 1432-0746, Volume 687, Page a121, 10.1051/0004-6361/202349043

Contributors

Kong, Zhihui 0000-0002-2236-0627 (Corresponding author) [1] [2] Johansen, Anders Sewerin 0000-0002-5893-6165 [1] [3] Lambrechts, Michiel 0000-0001-9321-5198 [1] Jiang, Jonathan H (Corresponding author) [4] Zhu, Zong-Hong [2]

Affiliations

  1. [1] University of Copenhagen
  2. [NORA names: KU University of Copenhagen; University; Denmark; Europe, EU; Nordic; OECD];
  3. [2] Beijing Normal University
  4. [NORA names: China; Asia, East];
  5. [3] Lund University
  6. [NORA names: Sweden; Europe, EU; Nordic; OECD];
  7. [4] Jet Propulsion Laboratory
  8. [NORA names: United States; America, North; OECD]

Abstract

The architecture and masses of planetary systems in the habitable zone could be strongly influenced by the presence of outer giant planets. Here, we investigate the impact of outer giants on terrestrial planet formation, under the assumption that the final assembly of the planetary system is set by a giant impact phase. Utilizing a state-of-the-art N -body simulation software, GENGA, we interpret how the late stage of terrestrial planet formation contributes to diversity among planetary systems. We designed two global model setups: 1) we placed a gas giant on the outer side of planetesimals and embryo disk and 2) we only included planetesimals and embryos, but no giant. For the model including the outer giant, we studied the effect of different giant initial masses in the range of 1.0–3.0 Jupiter masses, as well as a range of orbital radii from 2.0–5.8 AU. We also studied the influence of different initial positions of planetesimals and embryos on the results. Our N -body simulation time is approximately 50 Myr. The results show that the existence of an outer giant will promote the interaction between planetesimals and embryos, making the orbits of the formed terrestrial planets more compact. However, placing the giant planet too close to the planetesimals and embryo disk suppresses the formation of massive rocky planets. In addition, under the classical theory, where planetary embryos and planetesimals collide to form terrestrial planets, our results show that the presence of a giant planet actually decreases the gap complexity of the inner planetary system.

Keywords

GAP complex, GENGA, Jupiter, Jupiter masses, Myr, architecture, assembly, classical theory, complex, disk, diversity, effect, embryos, formation, formation simulations, gap, gas, gas giants, giant impact phase, giant planets, giants, habitable zone, impact, impact phase, influence, initial mass, initial position, inner planetary system, interaction, late stage, late stages of terrestrial planet formation, mass, massive rocky planets, model, model setup, orbit, orbital radius, outcomes, outer giant, outer giant planets, outer side, phase, planet, planet formation, planet formation simulations, planetary embryos, planetary systems, planetesimals, presence, radius, results, rocky planets, setup, simulation, simulation software, simulation time, software, stage of terrestrial planet formation, state-of-the-art, system, terrestrial planet formation, terrestrial planet formation simulations, terrestrial planets, theory, time, zone

Funders

  • National Natural Science Foundation of China
  • Jet Propulsion Laboratory
  • European Research Council
  • Danish National Research Foundation
  • Knut and Alice Wallenberg Foundation
  • Carlsberg Foundation
  • Swedish Research Council
  • Göran Gustafsson Foundation
  • Chinese Academy of Sciences

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