论多行星系统中初始条件的动态消除

Kevin Marimbu, Eve J. Lee
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引用次数: 0

摘要

亚海王星是在我们看到的地方附近聚集,还是在远离主恒星的地方形成完整的海王星,然后向内迁移?我们利用测量到的轨道周期分布(最基本的观测参数之一)来探讨这个问题。在磁盘诱导迁移的情况下,行星出现率预计会向更短的轨道周期下降。目前,观测到的海王星以下的周期分布在对数周期上是平的,介于 10 天和 300 天之间。我们利用 N-体积分显示了多行星系统中的盘后动力学不稳定性和合并是如何在 10 秒到 100 Myr 的时间尺度上消除周期分布中的迁移初始条件的,这与共振对的丰度在小于 100 Myr 的系统中的观测提示基本一致,而在进化程度更高的系统中,共振对的丰度会急剧下降。我们对注意事项和未来工作进行了评论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On the Dynamical Erasure of Initial Conditions in Multi-planetary Systems
Do sub-Neptunes assemble close to where we see them or do they form full-fledged farther away from their host star then migrate inwards? We explore this question using the distribution of measured orbital periods, one of the most fundamental observable parameters. Under disk-induced migration, planet occurrence rate is expected to decrease toward shorter orbital periods. Presently, the observed sub-Neptune period distribution is flat in log period, between 10 and 300 days. We show, using N-body integration, how post-disk dynamical instabilities and mergers in multi-planetary systems erase the initial conditions of migration emplaced in period distributions over 10 s to 100 Myr timescale, in rough agreement with an observational hint of the abundance of resonant pairs for systems younger than 100 Myr which drops dramatically for more evolved systems. We comment on caveats and future work.
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