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Tidal synchronization of close-in satellites and exoplanets: II. Spin dynamics and extension to Mercury and exoplanet host stars

机译:近距离卫星和系外行星的潮汐同步:II。自旋动力学并扩展到水星和系外行星宿主星

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This paper deals with the application of the creep tide theory (Ferraz-Mello, Celest Mech Dyn Astron 116: 109, 2013a) to the rotation of close-in satellites, Mercury, close-in exoplanets, and their host stars. The solutions show different behaviors with two extreme cases: close-in giant gaseous planets with fast relaxation (low viscosity) and satellites and Earth-like planets with slow relaxation (high viscosity). The rotation of close-in gaseous planets follows the classical Darwinian pattern: it is tidally driven toward a stationary solution that is synchronized with the orbital motion when the orbit is circular, but if the orbit is elliptical, it has a frequency larger than the orbital mean motion. The rotation of rocky bodies, however, may be driven to several attractors whose frequencies are 1/2, 1, 3/2, 2, 5/2, ... times the mean motion. The number of attractors increases with the viscosity of the body and with the orbital eccentricity. The final stationary state depends on the initial conditions. The classical example is Mercury, whose rotational period is 2/3 of the orbital period (3/2 attractor). The planet behaves as a molten body with a relaxation that allowed it to cross the 2/1 attractor without being trapped but not to escape being trapped in the 3/2 one. In that case, the relaxation is estimated to lie in the interval 4.6 < gamma < 27x10(-9) s(-1) (equivalent to a quality factor roughly constrained to the interval 5 < Q < 50). The stars have a relaxation similar to the hot Jupiters, and their rotation is also driven to the only stationary solution existing in these cases. However, solar-type stars may lose angular momentum due to stellar wind, braking the rotation and displacing the attractor toward larger periods. Old, active host stars with big close-in companions generally have rotational periods larger than the orbital periods of the companions. The paper also includes a study of energy dissipation and the evolution of orbital eccentricity.
机译:本文讨论了蠕变潮理论(Ferraz-Mello,Celest Mech Dyn Astron 116:109,2013a)在近距离卫星,水星,近地系外行星及其宿主恒星自转中的应用。这些解决方案在两种极端情况下表现出不同的行为:具有快速弛豫(低粘度)的近距离巨型气态行星和具有缓慢弛豫(高粘度)的人造卫星和类似地球的行星。近距离气态行星的旋转遵循经典的达尔文式:当轨道为圆形时,它以潮汐方向朝着与轨道运动同步的平稳解运动,但是如果轨道是椭圆形,则其频率大于轨道平均运动。然而,岩石体的旋转可能被驱动到多个吸引子,其频率是平均运动的1 / 2、1、3 / 2、2、5 / 2,...倍。吸引子的数量随着物体的粘度和轨道偏心率而增加。最终的静止状态取决于初始条件。经典的例子是水星,其旋转周期是轨道周期的2/3(3/2吸引子)。行星表现为具有松弛的熔融体,使它能够越过2/1吸引子而不会被困住,但无法逃脱而被困在3/2吸引子中。在那种情况下,松弛估计在4.6

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