Diversity of disc viscosities can explain the period ratios of resonant and non-resonant systems of hot super-Earths and mini-Neptunes

IF 5.4 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Astronomy & Astrophysics Pub Date : 2024-12-17 DOI:10.1051/0004-6361/202451017
Bertram Bitsch, Andre Izidoro
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Abstract

Migration is a key ingredient in the formation of close-in super-Earth and mini-Neptune systems. The migration rate sets the resonances in which planets can be trapped, where slower migration rates result in wider resonance configurations compared to higher migration rates. We investigate the influence of different migration rates – set by disc viscosity – on the structure of multi-planet systems via N-body simulations, where planets grow via pebble accretion. Planets in low-viscosity environments migrate slower due to partial gap opening compared to planets forming in high-viscosity environments. Consequently, systems formed in low-viscosity environments tend to have planets trapped in wider resonant configurations (typically 4:3, 3:2, and 2:1 configurations). Simulations of high-viscosity discs mostly produce planetary systems in 7:6, 5:4, and 4:3 resonances. After the gas disc dissipates, the damping forces of eccentricity and inclination cease to exist and the systems can undergo instities on timescales of a few tens of millions of years, rearranging their configurations and breaking the resonance chains. We show that low-viscosity discs naturally account for the configurations of resonant chains, such as Trappist-1, TOI-178, and Kepler-223, unlike high-viscosity simulations, which produce chains that are more compact. Following dispersal of the gas disc, about 95% of our low-viscosity resonant chains became unstable, experiencing a phase of giant impacts. Dynamical instabilities in our low-viscosity simulations are more violent than those of high-viscosity simulations due to the effects of leftover external perturbers (P>200 days). About 50% of our final systems end with no planets within 200 days, while all our systems harbour remaining outer planets. We speculate that this process could be qualitatively consistent with the lack of inner planets in a large fraction of the Sun-like stars. Systems produced in low-viscosity simulations alone do not match the overall period ratio distribution of observations, but give a better match to the period distributions of chains, which may suggest that systems of super-Earths and mini-Neptunes form in natal discs with a diversity of viscosities.
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迁移是形成近邻超地和小海王星系统的关键因素。迁移率设定了行星可能被困其中的共振,与较高的迁移率相比,较慢的迁移率会导致较宽的共振配置。我们通过 N-体模拟研究了由圆盘粘度设定的不同迁移率对多行星系统结构的影响。与在高粘度环境中形成的行星相比,低粘度环境中的行星由于部分间隙打开而迁移较慢。因此,在低粘度环境中形成的系统往往会有行星被困在较宽的共振构型中(通常为 4:3、3:2 和 2:1 构型)。对高粘度圆盘的模拟大多会产生 7:6、5:4 和 4:3 共振的行星系统。在气体圆盘消散后,偏心率和倾角的阻尼力不再存在,系统可能会发生时间尺度为几千万年的不稳定现象,从而重新排列其构型并打破共振链。我们的研究表明,低粘度圆盘可以自然地解释共振链的构型,如Trappist-1、TOI-178和开普勒-223,而不像高粘度模拟产生的共振链更加紧凑。在气体圆盘分散之后,大约 95% 的低粘度共振链变得不稳定,经历了巨型撞击阶段。由于残留外部扰动(P>200 天)的影响,低粘度模拟中的动态不稳定性比高粘度模拟中的更剧烈。大约 50%的最终系统在 200 天内没有行星,而所有系统都有剩余的外行星。我们推测,这一过程可能与大部分类太阳恒星缺乏内行星的现象在本质上是一致的。仅在低粘度模拟中产生的系统与观测数据的总体周期比分布并不匹配,但与链的周期分布匹配度较高,这可能表明超地球和小海王星系统是在具有不同粘度的原生星盘中形成的。
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来源期刊
Astronomy & Astrophysics
Astronomy & Astrophysics 地学天文-天文与天体物理
CiteScore
10.20
自引率
27.70%
发文量
2105
审稿时长
1-2 weeks
期刊介绍: Astronomy & Astrophysics is an international Journal that publishes papers on all aspects of astronomy and astrophysics (theoretical, observational, and instrumental) independently of the techniques used to obtain the results.
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