奥尔特云内部的自引力动力学

Konstantin Batygin, David Nesvorný
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摘要

内奥尔特云(IOC)的形成是太阳系在恒星簇内原始演化的一个预期结果。最近的模型显示,在跨海王星区域内的早期行星俘获过程可能足以使云的累积质量接近几个地球质量。有鉴于此,我们在此研究了IOC在自身引力驱动下的动力学演化。我们证明 IOC 的集体引力势可以用宫本长井模型充分近似,并使用半解析框架证明由此产生的周期振荡类似于 von Zeipel-Lidov-Kozai 共振。我们用直接的 N 体计算验证了我们的结果,并通过详细的模拟研究了 IOC 自引力对太阳系小天体长期行为的影响。我们发现,虽然近日点距离和倾角的调节发生在与观测相关的范围内,但相关的时间尺度远远超过了太阳的年龄,这表明海委会自引力对太阳系结构的影响可以忽略不计。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Self-gravitational dynamics within the inner Oort cloud

Self-gravitational dynamics within the inner Oort cloud

The formation of the Inner Oort Cloud (IOC)—a vast halo of icy bodies residing far beyond Neptune’s orbit—is an expected outcome of the solar system’s primordial evolution within a stellar cluster. Recent models have shown that the process of early planetesimal capture within the trans-Neptunian region may have been sufficiently high for the cumulative mass of the Cloud to approach several Earth masses. In light of this, here we examine the dynamical evolution of the IOC, driven by its own self-gravity. We show that the collective gravitational potential of the IOC is adequately approximated by the Miyamoto–Nagai model and use a semi-analytic framework to demonstrate that the resulting secular oscillations are akin to the von Zeipel–Lidov–Kozai resonance. We verify our results with direct N-body calculations and examine the effects of IOC self-gravity on the long-term behavior of the solar system’s minor bodies using a detailed simulation. Cumulatively, we find that while the modulation of perihelion distances and inclinations can occur within an observationally relevant range, the associated timescales vastly surpass the age of the sun, indicating that the influence of IOC self-gravity on the architecture of the solar system is negligible.

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