论文标题
圆盘上的停车行星
Parking planets in circumbinary discs
论文作者
论文摘要
开普勒太空任务发现了大约十几个围绕二进制恒星系统的行星。这些环形行星中的大多数都在其不稳定边界附近,约为3至5个二元分离。过去通过向内迁移过程匹配这些最终位置的尝试仅在开普勒16系统中成功。在这里,我们研究了10个电路系统,并尝试将行星的最终停车位和轨道参数与光盘驱动的迁移情况相匹配。 我们对带有嵌入行星的环形盘进行了2D局部等温流体动力学模拟,并使用盘式粘度和纵横比的不同值遵循其迁移进化。我们发现,对于具有中间二进制偏心率的六个系统($ 0.1 \ le e_ {bin} \ le 0.21 $),最终的行星轨道与单个光盘参数的观测值紧密匹配,特别是$α= 10^{ - 4} $的圆盘粘度,以及$ h/r $ h/r $ h/r $ 0.04 $ 0.04。对于这些系统,行星质量足够大,可以在二进制二进制时至少在椎间盘上张开部分间隙,从而迫使圆盘变得圆形,并允许进一步向二进制迁移,从而与观察到的行星轨道参数达成了良好的一致性。 对于具有很小或大二进制偏心率的系统,匹配不太好,因为在这些情况下,非常偏心的圆盘和大型内部空腔阻止了行星的近距离迁移。在高于观察到的行星质量的测试模拟中,可以找到这些系统更好的一致性。 在10个建模的系统中,有6个良好的协议,其中观察到的最终行星轨道和模拟的最终行星之间的相对差异为$ \ leq 10 \%$,这强烈支持了碟片中的行星迁移将行星带到当前位置的想法。
The Kepler space mission discovered about a dozen planets orbiting around binary stars systems. Most of these circumbinary planets lie near their instability boundaries at about 3 to 5 binary separations. Past attempts to match these final locations through an inward migration process were only successful for the Kepler-16 system. Here, we study 10 circumbinary systems and try to match the final parking locations and orbital parameters of the planets with a disc driven migration scenario. We performed 2D locally isothermal hydrodynamical simulations of circumbinary discs with embedded planets and followed their migration evolution using different values for the disc viscosity and aspect ratio. We found that for the six systems with intermediate binary eccentricities ($0.1 \le e_{bin}\le 0.21$) the final planetary orbits matched the observations closely for a single set of disc parameters, specifically a disc viscosity of $α= 10^{-4}$, and an aspect ratio of $H/r \sim 0.04$. For these systems the planet masses were large enough to open at least a partial gap in their discs as they approach the binary, forcing the discs to become circularized and allowing for further migration towards the binary, leading to good agreement with the observed planetary orbital parameters. For systems with very small or large binary eccentricities the match was not as good because the very eccentric discs and large inner cavities in these cases prevented close-in planet migration. In test simulations with higher than observed planet masses better agreement could be found for those systems. The good agreement for 6 out of the 10 modelled systems, where the relative difference between observed and simulated final planet orbit is $\leq 10\%$, strongly supports the idea that planet migration in the disc brought the planets to their present locations.