Breaking mean-motion resonances during Type I planet migration

被引:11
|
作者
Hands, T. O. [1 ,2 ]
Alexander, R. D. [1 ]
机构
[1] Univ Leicester, Dept Phys & Astron, Univ Rd, Leicester LE1 7RH, Leics, England
[2] Univ Zurich, Inst Comp Gestutzte Wissensch, Winterthurerstr 190, CH-8057 Zurich, Switzerland
基金
瑞士国家科学基金会; 欧洲研究理事会;
关键词
hydrodynamics; methods: numerical; planets and satellites: dynamical evolution and stability; planets and satellites: formation; planet-disc interactions; planetary systems; ISOTHERMAL GASEOUS DISK; LOW-MASS; TORQUE FORMULA; 3-DIMENSIONAL INTERACTION; HORSESHOE DRAG; SITU FORMATION; GIANT PLANETS; PERIOD RATIOS; ACCRETION; SYSTEMS;
D O I
10.1093/mnras/stx2711
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We present 2D hydrodynamical simulations of pairs of planets migrating simultaneously in the Type I regime in a protoplanetary disc. Convergent migration naturally leads to the trapping of these planets in mean-motion resonances. Once in resonance the planets' eccentricity grows rapidly, and disc-planet torques cause the planets to escape resonance on a time-scale of a few hundred orbits. The effect is more pronounced in highly viscous discs, but operates efficiently even in inviscid discs. We attribute this resonance-breaking to overstable librations driven by moderate eccentricity damping, but find that this mechanism operates differently in hydrodynamic simulations than in previous analytic calculations. Planets escaping resonance in this manner can potentially explain the observed paucity of resonances in Kepler multitransiting systems, and we suggest that simultaneous disc-driven migration remains the most plausible means of assembling tightly packed planetary systems.
引用
收藏
页码:3998 / 4009
页数:12
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