Constraints on the formation history and composition of Kepler planets from their distribution of orbital period ratios

IF 5.4 2区 物理与天体物理 Q1 ASTRONOMY & ASTROPHYSICS Astronomy & Astrophysics Pub Date : 2024-06-27 DOI:10.1051/0004-6361/202449371
Di-Chang Chen, Christoph Mordasini, Ji-Wei Xie, Ji-Lin Zhou, Alexandre Emsenhuber
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Abstract

Context. The Kepler high-precision planetary sample has revealed a ‘radius valley’ separating compact super-Earths from sub-Neptunes with lower densities. Super-Earths are generally assumed to be rocky planets that were probably born in situ, while the composition and formation of sub-Neptunes remains debated. Numerous statistical studies have explored planetary and stellar properties and their correlations to provide observational clues. However, no conclusive result on the origin of the radius valley or the composition of sub-Neptunes has been derived to date.Aims. To provide more constraints, our aim is to investigate the distributions of the orbital spacing of sub-Neptunes and super-Earth planets in Kepler systems and compare their distributions with theoretical predictions of planet pairs of different formation pathways and compositions in synthetic planetary systems.Methods. Based on the Kepler planetary sample, we derived the distributions of period ratios of sub-Neptune and super-Earth planet pairs. Using synthetic planetary systems generated by the Generation III Bern Model, we also obtained theoretical predictions of period ratio distributions of planet pairs of different compositions and origins.Results. We find that Kepler sub-Neptune pairs show a significant preference to be near first-order mean motion resonances by a factor of 1.7−0.3+0.3. This is smaller than the model predictions for ‘water-rich’ pairs but larger than that of ‘water-poor’ pairs by confidence levels of ~2σ. Kepler super-Earth pairs show no significant preference for mean motion resonances from a random distribution. The derived normalised fraction of near first-order resonances of actual Kepler super-Earth pairs is consistent with that of synthetic water-poor planet pairs but significantly (≳3σ) smaller than that of synthetic water-rich planet pairs.Conclusions. The orbital migration has been more important for sub-Neptunes than for super-Earths, suggesting a partial ex situ formation of the former and an origin of the radius valley caused in part by distinct formation pathways. However, the model comparisons also show that sub-Neptunes in Kepler multiple systems are not likely (~2σ) to all be water-rich planets born ex situ but a mixture of the two (in situ and ex situ) pathways. Whereas, Kepler super-Earth planets are predominantly composed of water-poor planets that were born inside the ice line, likely through a series of giant impacts without large-scale migration.
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从开普勒行星的轨道周期比分布看它们的形成历史和组成的制约因素
背景开普勒高精度行星样本揭示了一个 "半径谷",它将紧凑的超级地球与密度较低的亚海王星分开。超地星一般被认为是岩石行星,很可能是在原地诞生的,而亚海王星的组成和形成仍有争议。许多统计研究探讨了行星和恒星的特性及其相关性,以提供观测线索。然而,关于半径谷的起源或次海王星的成分,迄今为止还没有定论。为了提供更多的约束条件,我们的目的是研究开普勒系统中的亚海王星和超地行星的轨道间距分布,并将它们的分布与合成行星系统中不同形成途径和成分的行星对的理论预测进行比较。基于开普勒行星样本,我们得出了亚海王星和超地球行星对的周期比分布。我们还利用第三代伯尔尼模型生成的合成行星系统,对不同成分和起源的行星对的周期比分布进行了理论预测。我们发现,开普勒海王星以下的行星对明显倾向于接近一阶平均运动共振,系数为1.7-0.3+0.3。这比 "富水 "配对的模型预测值要小,但比 "贫水 "配对的预测值要大,置信度为~2σ。从随机分布来看,开普勒超地星对并不明显偏好平均运动共振。实际开普勒超地星对的近一阶共振的归一化分数与合成的贫水行星对一致,但明显(≳3σ)小于合成的富水行星对。亚海王星的轨道迁移比超地星更重要,这表明前者部分是在原地形成的,而半径谷的形成部分是由不同的形成途径造成的。不过,模型比较也表明,开普勒多重系统中的亚海王星不可能(~2σ)都是原地诞生的富含水的行星,而是两种(原地和原地)形成途径的混合体。而开普勒超地行星主要是由在冰线内诞生的贫水行星组成的,它们很可能是通过一系列巨型撞击而诞生的,没有大规模的迁移。
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