论文标题
关于紧凑型超级地球展示的偏心二分法的起源:冷巨人的动态加热
On the origin of the eccentricity dichotomy displayed by compact super-Earths: dynamical heating by cold giants
论文作者
论文摘要
NASA的开普勒任务发现的大约一半的行星都在一个系统中,只有一个行星将其寄主恒星驶过,并且观察到其余的行星在多行星系统中。最近的分析报道了系统在系统中显示的偏心分布中的二分法,其中单个行星与多行星系统所显示的行星相比。使用$ n $ - 体模拟,我们研究了这种二分法已经出现的假设,因为超级毕业生的内部系统经常伴随着巨型行星的外部系统,这些系统可能会动态不稳定并扰乱内部系统。我们的初始条件是使用已知的开普勒五个平面系统的子集作为内部系统的模板,以及在轨道半径和土星之间具有质量的外部巨型行星的模板,这些行星的质量为轨道半径$ 2 \ le a _ {\ rm p} \ le 10 $ au。选择外部系统的参数,以便它们始终低于假定的径向速度检测阈值3 ms $^{ - 1} $。结果表明,平均偏心率与系统的多个物质之间存在反向关系。对最终系统的合成传输观察揭示了几乎与开普勒数据一致的偏心和多样性分布的二分法。因此,理解开普勒发现的超收获物的紧凑型系统的观察到的轨道和物理性能可能需要整体建模,从而在形成时期内及之后伴随着行星内部和外部系统的动力学。
Approximately half of the planets discovered by NASA's Kepler mission are in systems where just a single planet transits its host star, and the remaining planets are observed to be in multi-planet systems. Recent analyses have reported a dichotomy in the eccentricity distribution displayed by systems where a single planet transits compared with that displayed by the multi-planet systems. Using $N$-body simulations, we examine the hypothesis that this dichotomy has arisen because inner systems of super-Earths are frequently accompanied by outer systems of giant planets that can become dynamically unstable and perturb the inner systems. Our initial conditions are constructed using a subset of the known Kepler five-planet systems as templates for the inner systems, and systems of outer giant planets with masses between those of Neptune and Saturn that are centred on orbital radii $2 \le a_{\rm p} \le 10$ au. The parameters of the outer systems are chosen so that they are always below an assumed radial velocity detection threshold of 3 ms$^{-1}$. The results show an inverse relation between the mean eccentricities and the multiplicites of the systems. Performing synthetic transit observation of the final systems reveals dichotomies in both the eccentricity and multiplicity distributions that are close to being in agreement with the Kepler data. Hence, understanding the observed orbital and physical properties of the compact systems of super-Earths discovered by Kepler may require holistic modelling that couples the dynamics of both inner and outer systems of planets during and after the epoch of formation.