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Neptune’s Migration into a Stirred-Up Kuiper Belt: A Detailed Comparison of Simulations to Observations

机译:海王星向搅动的柯伊伯带的迁移:模拟与观测的详细比较

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We use N-body simulations to examine the consequences of Neptune's outward migration into the Kuiper Belt, with the simulated end states being compared rigorously and quantitatively to the observations. These simulations confirm the 2003 findings of Chiang and coworkers, who showed that Neptune's migration into a previously stirred-up Kuiper Belt can account for the Kuiper Belt objects (KBOs) known to librate at Neptune's 5?:?2 resonance. We also find that capture is possible at many other weak, high-order mean-motion resonances, such as 11?:?6, 13?:?7, 13?:?6, 9?:?4, 7?:?3, 12?:?5, 8?:?3, 3?:?1, 7?:?2, and 4?:?1. The more distant of these resonances, such as the 9?:?4, 7?:?3, 5?:?2, and 3?:?1, can also capture particles in stable, eccentric orbits beyond 50 AU, in the region of phase space conventionally known as the "Scattered Disk." Indeed, 90% of the simulated particles that persist over the age of the solar system in the Scattered-Disk zone never had a close encounter with Neptune but instead were promoted into these eccentric orbits by Neptune's resonances during the migration epoch. This indicates that the observed Scattered Disk might not be so scattered. This model also produced only a handful of Centaurs, all of which originated at Neptune's mean-motion resonances in the Kuiper Belt. However, a noteworthy deficiency of the migration model considered here is that it does not account for the observed abundance of Main Belt KBOs having inclinations higher than 15°. In order to rigorously compare the model end state with the observed Kuiper Belt in a manner that accounts for telescopic selection effects, Monte Carlo methods are used to assign sizes and magnitudes to the simulated particles that survive over the age of the solar system. If the model considered here is indeed representative of the outer solar system's early history, then the following conclusions are obtained: (1) The observed 3?:?2 and 2?:?1 resonant populations are both depleted by a factor of ~20 relative to model expectations; this depletion is likely due to unmodeled effects, possibly perturbations by other large planetesimals. (2) The size distribution of those KBOs inhabiting the 3?:?2 resonance is significantly shallower than the Main Belt's size distribution. (3) The total number of KBOs having radii R > 50 km and orbiting interior to Neptune's 2?:?1 resonance is N ~ 1.7 × 105; these bodies have a total mass of M ~ 0.08(ρ/1 g cm-3)(p/0.04)-3/2 M⊕, assuming they have a material density ρ and an albedo p. We also report estimates of the abundances and masses of the Belt's various subpopulations (e.g., the resonant KBOs, the Main Belt, and the so-called Scattered Disk) and provide upper limits on the abundance of Centaurs and Neptune's Trojans, as well as upper limits on the sizes and abundances of hypothetical KBOs that might inhabit the a > 50 AU zone.
机译:我们使用N体模拟来检查海王星向外迁移到柯伊伯带的后果,并将模拟的最终状态与观测值进行严格和定量的比较。这些模拟结果证实了Chiang和他的同事在2003年的发现,他们表明海王星向先前激起的柯伊伯带的迁移可以解释已知以海王星5?:?2共振释放的柯伊伯带天体(KBO)。我们还发现在许多其他弱,高阶平均运动共振中也可以捕获,例如11?:?6,13?:?7,13?:?6,9?:?4,7?:?。 3,12?:?5,8?:?3,3?:?1,7?:?2和4?:?1。这些共振距离越远,例如9?:?4、7?:?3、5?:?2和3?:?1,也可以捕获超过50 AU的稳定,偏心轨道中的粒子。通常称为“分散磁盘”的相空间区域。的确,在散盘区中太阳系中持续存在的90%的模拟粒子从未与海王星有过近距离接触,而是在迁移时期由海王星的共振提升到了这些偏心轨道。这表明观察到的分散磁盘可能没有那么分散。该模型也只产生了少量的半人马座,所有这些都起源于海王星在柯伊伯带的平均运动共振。但是,这里考虑的迁移模型的一个值得注意的缺陷是,它不能解释观察到的倾斜度大于15°的主带KBO的丰度。为了通过考虑伸缩选择效应的方式将模型的最终状态与观察到的柯伊伯带严格进行比较,使用了蒙特卡洛方法为模拟的粒子分配大小和大小,这些粒子在太阳系的整个寿命中都可以存活。如果这里考虑的模型确实代表了外部太阳系的早期历史,那么可以得出以下结论:(1)观察到的3?:?2和2?:?1共振人口都被减少了约20倍。相对于模型期望;这种耗竭很可能是由于未建模的影响,也可能是其他大型行星的干扰。 (2)处于3?:?2共振的KBO的尺寸分布明显比主带的尺寸分布浅。 (3)半径R> 50 km且在海王星2π:?1共振内部轨道的KBO总数为N〜1.7×105;这些物体的总质量为M〜0.08(ρ/ 1 g cm-3)(p / 0.04)-3/2M⊕,假设它们具有材料密度ρ和反照率p。我们还报告了带的各种亚群(例如,共振的KBO,主带和所谓的分散磁盘)的丰度和质量的估计值,并提供了半人马和海王星木马的丰度上限以及上限。对可能居住在> 50 AU区的假设KBO的大小和丰度的限制。

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