The dynamical history of the Kepler-221 planet system

被引:0
|
作者
Yi, Tian [1 ]
Ormel, Chris W. [1 ]
Huang, Shuo [1 ,2 ]
Petit, Antoine C. [3 ]
机构
[1] Tsinghua Univ, Dept Astron, Beijing 100084, Peoples R China
[2] Leiden Univ, Leiden Observ, POB 9513, NL-2300 RA Leiden, Netherlands
[3] Univ Cote Azur, CNRS, Observ Cote Azur, Lab Lagrange, Nice, France
基金
中国国家自然科学基金;
关键词
planets and satellites: dynamical evolution and stability; planets and satellites: formation; stars: individual: Kepler-221; MEAN-MOTION RESONANCES; TIDAL DISSIPATION; RADIUS DISTRIBUTION; ORBITAL EVOLUTION; MASS; CHAIN; MIGRATION; ORIGIN; BREAKING; PAIRS;
D O I
10.1051/0004-6361/202452005
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Kepler-221 is a G-type star hosting four planets. In this system, planets b, c, and e are in (or near) a 6:3:1 three-body resonance even though the planets' period ratios show significant departures from exact two-body commensurability. Importantly, the intermediate planet d is not part of the resonance chain. To reach this resonance configuration, we propose a scenario in which there were originally five planets in the system in a chain of first-order resonances. After disk dispersal, the resonance chain became unstable, and two planets quickly merged to become the current planet d. In addition, the (b, c, e) three-body resonance was re-established. We ran N body simulations using REBOUND to investigate the parameter space under which this scenario can operate. We find that our envisioned scenario is possible when certain conditions are met. First, the reformation of the three-body resonance after planet merging requires convergent migration between planets b and c. Second, as has been previously pointed out, an efficient damping mechanism must operate to power the expansion of the (b, c, e) system. We find that planet d plays a crucial role during the orbital expansion phase due to destabilizing encounters of a three-body resonance between c, d, and e. A successful orbital expansion phase puts constraints on the planet properties in the Kepler-221 system including the planet mass ratios and the tidal quality factors for the planets. Our model can also be applied to other planet systems in resonance, such as Kepler-402 and K2-138.
引用
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页数:20
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