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Evidence for Solid Planets from Kepler's Near-Resonance Systems

机译:开普勒近谐振系统的实体的证据

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The multiple-planet systems discovered by the Kepler mission show an excess of planet pairs with period ratios just wide of exact commensurability for first-order resonances like 2:1 and 3:2. In principle, these planet pairs could be in resonance if their orbital eccentricities are sufficiently small, because the width of first-order resonances diverges in the limit of vanishingly small eccentricity. We consider a widely-held scenario in which pairs of planets were captured into first-order resonances by migration due to planet-disk interactions, and subsequently became detached from the resonances, due to tidal dissipation in the planets. In the context of this scenario, we find a constraint on the ratio of the planet's tidal dissipation function and Love number that implies that some of the Kepler planets are likely solid. However, tides are not strong enough to move many of the planet pairs to the observed separations, suggesting that additional processes are at play.
机译:开普勒任务发现的多个行星系统显示出多余的行星对,周期比对于一阶共振的精确符合性,如2:1和3:2。原则上,如果它们的轨道偏心足够小,则这些行星对可以是共振的,因为一阶共振的宽度在缺失的小偏心率的极限中发散。我们考虑了一种广泛的场景,其中由于行星盘相互作用,通过迁移捕获一对行星的行星,并且由于行星中的潮汐散流,随后从共振拆分。在这种情况的上下文中,我们发现了一个关于行星潮汐耗散函数和爱情的比率的约束,意味着一些开普勒行星可能是坚实的。然而,潮汐足以让许多行星对移动到观察到的分离,这表明额外的过程在播放。

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