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arXiv 0907.1829astro-ph.EP
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初始和边界条件如何影响湍流亚开普勒吸积盘中的原行星迁移:二维非粘性SPH模拟

How initial and boundary conditions affect protoplanetary migration in a turbulent sub-Keplerian accretion disc: 2D non viscous SPH simulations

Vincenzo Costa, Valerio Pirronello, Gaetano Belvedere, Antonino Del Popolo, Diego Molteni, Giuseppe Lanzafame

摘要:

目前关于行星形成的理论认为,巨行星的形成应该与它们快速向中央恒星迁移有关,这是由于原行星与盘的相互作用,对于近10个地球质量的天体来说,时间尺度为$10^5$年。这样的时间尺度应该比原行星通过与其他小天体碰撞而分层成长期间气体吸积到原行星上的时间尺度小一个数量级。这些参数最近被分析使用N体和/或流体动力学代码或它们的混合。在这项工作中,无粘性的2D模拟进行,使用SPH方法,研究一个原行星的迁移,评估吸积盘的有效性的原行星拖向中央恒星,作为一个函数的行星本身的质量,盘切向运动。为此,SPH方案被认为是适合研究湍流,运动学和边界条件的作用,由于其固有的平流湍流,特别是在2D和3D代码。模拟都在光盘子开普勒和开普勒运动学条件下进行的参数研究的原行星迁移,如果发生中度和一致的偏离开普勒动力学。我们的研究结果表明,在亚开普勒条件下,类地行星的几个轨道周期的迁移时间,而对于类地行星的估计给出了大约$10^4$轨道周期需要一半的轨道大小。行星迁移的时间尺度在很大程度上取决于行星相对于盘流的离心屏障附近的激波区域的相对位置。

英文摘要:

Current theories on planetary formation establish that giant planet formation should be contextual to their quick migration towards the central star due to the protoplanets-disc interactions on a timescale of the order of $10^5$ years, for objects of nearly 10 terrestrial masses. Such a timescale should be smaller by an order of magnitude than that of gas accretion onto the protoplanet during the hierarchical growing-up of protoplanets by collisions with other minor objects. These arguments have recently been analysed using N-body and/or fluid-dynamics codes or a mixing of them. In this work, inviscid 2D simulations are performed, using the SPH method, to study the migration of one protoplanet, to evaluate the effectiveness of the accretion disc in the protoplanet dragging towards the central star, as a function of the mass of the planet itself, of disc tangential kinematics. To this purpose, the SPH scheme is considered suitable to study the roles of turbulence, kinematic and boundary conditions, due to its intrinsic advective turbulence, especially in 2D and in 3D codes. Simulations are performed both in disc sub-Keplerian and in Keplerian kinematic conditions as a parameter study of protoplanetary migration if moderate and consistent deviations from Keplerian Kinematics occur. Our results show migration times of a few orbital periods for Earth-like planets in sub-Keplerian conditions, while for Jupiter-like planets estimates give that about $10^4$ orbital periods are needed to half the orbital size. Timescales of planet migration are strongly dependent on the relative position of the planet with respect to the shock region near the centrifugal barrier of the disc flow.

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