湍流吸积盘的磁流出

J. Jacquemin-Ide, G. Lesur, J. Ferreira
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引用次数: 8

摘要

天体物理盘可能嵌在环境垂直磁场中。众所周知,这个环境场驱动磁盘体中的磁旋转湍流,但也负责在天体物理喷流的起源处发射磁化流出物。这种系统的垂直结构和长期(长期)演化缺乏定量预测。然而,正是这种长期演化被用来解释许多吸积系统(如x射线双星)的时间变异性。我们计算并分析了由大尺度磁场引导的吸积盘的全局三维理想mhd模拟。我们评估了湍流项在系统平衡中的作用。然后,我们计算质量的传输,角动量,和磁场在磁盘表征其长期演变。我们进行了一项参数调查,以表征磁盘性质对长期传输的影响。我们发现,弱磁化的磁盘驱动的射流带走了磁盘角动量的一小部分。虽然质量加权吸积速度保持亚音速,但总是存在一个发生跨音速吸积的上层湍流大气区域。我们证明了磁旋转不稳定性的强磁化版本驱动了这种湍流。圆盘结构与传统的流体静力学图像截然不同。磁场在磁盘中总是被向内拉,其速度随着磁盘磁化强度的增加而增加。超过了后者的阈值,圆盘就会经历一次深刻的径向调整。它导致形成一个内部吸积弹射区,其吸积速度为超音速质量加权,磁场分布趋于稳定,与热压接近均分。这种内部结构与费雷拉(1997)描述的喷射发射盘模型有许多相同的性质。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Magnetic outflows from turbulent accretion disks
Astrophysical disks are likely embedded in an ambient vertical magnetic field. This ambient field is known to drive magneto-rotational turbulence in the disk bulk but is also responsible for the launching of magnetized outflows at the origin of astrophysical jets. The vertical structure and long-term (secular) evolution of such a system lack quantitative predictions. It is nevertheless this secular evolution that is proposed to explain time variability in many accreting systems such as X-ray binaries. We compute and analyze global 3D ideal-MHD simulations of an accretion disk threaded by a large-scale magnetic field. We evaluate the role of the turbulent terms in the equilibrium of the system. We then compute the transport of mass, angular momentum, and magnetic fields in the disk to characterize its secular evolution. We perform a parameter survey to characterize the influence of disk properties on secular transport. We find that weakly magnetized disks drive jets that carry away a small fraction of the disk angular momentum. The mass-weighted accretion speed remains subsonic although, there is always an upper turbulent atmospheric region where transonic accretion takes place. We show that a strongly magnetized version of the magneto-rotational instability drives this turbulence. The disk structure is drastically different from the conventional hydrostatic picture. The magnetic field is always dragged inwards in the disk, at a velocity that increases with the disk magnetization. Beyond a threshold on the latter, the disk undergoes a profound radial readjustment. It leads to the formation of an inner accretion-ejection region with a supersonic mass-weighted accretion speed and where the magnetic field distribution becomes steady, near equipartition with the thermal pressure. This inner structure shares many properties with the Jet Emitting Disk model described by Ferreira (1997).
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