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arXiv 0712.2198astro-ph
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冥王星以外的外行星和海王星带结构的起源

An Outer Planet Beyond Pluto and Origin of the Trans-Neptunian Belt Architecture

Patryk Sofia Lykawka, Tadashi Mukai

摘要:

海王星外天体(TNO)是外太阳系中碰撞和动力演化的小行星盘的残留物。这种复杂的结构,被称为外海王星带(或埃奇奥-柯伊伯带),可以揭示有关盘的性质,行星形成和其他演化过程的重要线索。与吸积理论的预测相反,TNO表现出令人惊讶的大偏心率,e和倾角,i,可以分为不同的动力学类。有几个模型讨论了TNO的起源和轨道演变,但没有一个模型再现了详细的观测,例如,所有的动力学类和特殊的对象,或提供有见地的预测。基于大量的模拟的存在下的四个巨大的行星和巨大的星子的星子盘,我们建议,一个外行星的轨道历史十分之一的地球质量可以解释跨海王星带轨道结构。这个巨大的天体可能被其中一颗巨行星分散,然后将原始的星子盘搅拌到40-50 AU的水平,并在行星迁移前将其截断约48 AU。这颗外行星后来获得了一个倾斜的稳定轨道(>100 AU; 20-40 deg),因为它与海王星的共振相互作用(r:1或r:2共振可能与Kozai机制相结合),保证了海王星带的稳定性。我们的模型始终如一地再现了每个动力学类的主要特征,具有前所未有的细节;它还满足其他约束条件,如目前的小总质量的trans-Neptunian带和海王星的当前轨道在30.1 AU。我们还提供了观测可检验的预测。

英文摘要:

Trans-Neptunian objects (TNOs) are remnants of a collisionally and dynamically evolved planetesimal disk in the outer solar system. This complex structure, known as the trans-Neptunian belt (or Edgeworth-Kuiper belt), can reveal important clues about disk properties, planet formation, and other evolutionary processes. In contrast to the predictions of accretion theory, TNOs exhibit surprisingly large eccentricities, e, and inclinations, i, which can be grouped into distinct dynamical classes. Several models have addressed the origin and orbital evolution of TNOs, but none have reproduced detailed observations, e.g., all dynamical classes and peculiar objects, or provided insightful predictions. Based on extensive simulations of planetesimal disks with the presence of the four giant planets and massive planetesimals, we propose that the orbital history of an outer planet with tenths of Earth's mass can explain the trans-Neptunian belt orbital structure. This massive body was likely scattered by one of the giant planets, which then stirred the primordial planetesimal disk to the levels observed at 40-50 AU and truncated it at about 48 AU before planet migration. The outer planet later acquired an inclined stable orbit (>100 AU; 20-40 deg) because of a resonant interaction with Neptune (an r:1 or r:2 resonance possibly coupled with the Kozai mechanism), guaranteeing the stability of the trans-Neptunian belt. Our model consistently reproduces the main features of each dynamical class with unprecedented detail; it also satisfies other constraints such as the current small total mass of the trans-Neptunian belt and Neptune's current orbit at 30.1 AU. We also provide observationally testable predictions.

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