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Effect of wind-driven accretion on planetary migration

机译:风力驱动造成对行星迁移的影响

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Context. Planetary migration is a key link between planet formation models and observed exoplanet statistics. So far, the theory of planetary migration has focused on the interaction of one or more planets with an inviscid or viscously evolving gaseous disk. Turbulent viscosity is thought to be the main driver of the secular evolution of the disk, and it is known to affect the migration process for intermediate- to high-mass planets. Recently, however, the topic of wind-driven accretion has experienced a renaissance because evidence is mounting that protoplanetary disks may be less turbulent than previously thought, and 3D non-ideal magnetohydrodynamic modeling of the wind-launching process is maturing. Aims. We investigate how wind-driven accretion may affect planetary migration. We aim for a qualitative exploration of the main effects and not for a quantitative prediction. Methods. We performed 2D hydrodynamic planet-disk interaction simulations with the FARGO3D code in the ( r , ? ) plane. The vertical coordinate in the disk and the launching of the wind are not treated explicitly. Instead, the torque caused by the wind onto the disk is treated using a simple two-parameter formula. The parameters are the wind mass-loss rate and the lever arm. Results. We find that the wind-driven accretion process replenishes the co-orbital region in a different way than the viscous accretion process. The former always injects mass from the outer edge of the co-orbital region, and always removes mass from the inner edge, while the latter injects or removes mass from the co-orbital region depending on the radial density gradients in the disk. As a consequence, the migration behavior can differ strongly, and can under certain conditions drive rapid type-III-like outward migration. We derive an analytic expression for the parameters under which this outward migration occurs. Conclusions. If wind-driven accretion plays a role in the secular evolution of protoplanetary disks, planetary migration studies have to include this process as well because it can strongly affect the resulting migration rate and migration direction.
机译:语境。行星迁移是行星形成模型和观察到的Exoplanet统计数据之间的关键联系。到目前为止,行星迁移理论集中于一个或多个行星与耐粘性或粘性不断发展的气体盘的相互作用。湍流粘度被认为是磁盘的世俗演变的主要驱动器,并且已知它会影响中间至高质量行星的迁移过程。然而,最近,风力驱动的吸收的主题经历了一个文艺复兴,因为证据安装了原子象象盘可能比以前认为的湍流不那么湍流,并且风力发射过程的3D非理想磁流学模型正在成熟。目标。我们调查风力驱动的吸收程度如何影响行星迁移。我们的目标是对主要效果的定性探索,而不是用于定量预测。方法。我们在(r,a)平面中使用Fargo3D代码执行了2D流体动力行星磁盘交互模拟。磁盘中的垂直坐标和风的发射未明确对待。相反,使用简单的双参数公式处理由风引起的扭矩。参数是风体损耗率和杠杆臂。结果。我们发现风力驱动的增齿过程以不同于粘性的增量过程补充了共轨区域。前者总是从共轨区域的外边缘注射质量,并且总是从内边缘移除质量,而后者根据盘中的径向密度梯度从共轨区域注射或移除质量。因此,迁移行为可能强烈差异,并且可以在某些条件下驱动快速类型-III样外迁移。我们派生了对此外迁移发生的参数的分析表达式。结论。如果风力驱动的吸收在原始磁盘的世俗演变中发挥作用,则行星迁移研究也必须包括该过程,因为它可以强烈影响所产生的迁移率和迁移方向。

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