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arXiv 1003.4471astro-ph.SRastro-ph.GA
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粘性电阻性吸积盘中的大尺度磁场。I.弱磁化圆盘的抛射

Large scale magnetic fields in viscous resistive accretion disks. I. Ejection from weakly magnetized disks

Gareth C. Murphy, Jonathan Ferreira, Claudio Zanni

摘要:

来自开普勒吸积盘附近的冷稳态盘风理论需要接近均分强度的大尺度磁场。然而,从未测试过最小磁化强度。研究了弱垂直磁场穿过吸积盘的时间演化。磁场的强度使得磁盘的磁化强度随半径迅速下降。利用磁流体动力学程序PLUTO对粘性阻力吸积盘进行了4个2.5维数值模拟。在这些模拟中,使用平均场方法,并假设湍流引起异常传输系数(α处方)。大尺度的磁场只对盘结构引入小的扰动,吸积由占主导地位的粘性力矩驱动。观测到一个超快磁声喷流从最内层区域发射,并在超过953个开普勒轨道上保持静止。自约束射流从圆盘中的有限径向区域发射,该区域随时间保持恒定。喷射是可能的,因为磁化达到统一的磁盘表面,由于陡峭的密度下降。然而,当中平面磁化变得太小时,没有喷射报告。然而,渐近射流速度仍然太低,无法解释观察到的射流,因为射流带走的功率可以忽略不计。具有过热表面层的天体物理盘可以驱动类似的外流,即使它们的中平面磁化很低。湍流粘滞性将提取足够的角动量,使吸积过程继续下去。磁化的外流只不过是副产品,而不是吸积的基本驱动力。然而,如果中平面磁化向中心增加,则可以实现向内部射流主导的盘的自然过渡。

英文摘要:

Cold steady-state disk wind theory from near Keplerian accretion disks requires a large scale magnetic field at near equipartition strength. However the minimum magnetization has never been tested. We investigate the time evolution of an accretion disk threaded by a weak vertical magnetic field. The strength of the field is such that the disk magnetization falls off rapidly with radius. Four 2.5D numerical simulations of viscous resistive accretion disk are performed using the magnetohydrodynamic code PLUTO. In these simulations, a mean field approach is used and turbulence is assumed to give rise to anomalous transport coefficients (alpha prescription). The large scale magnetic field introduces only a small perturbation to the disk structure, with accretion driven by the dominant viscous torque. A super fast magnetosonic jet is observed to be launched from the innermost regions and remains stationary over more than 953 Keplerian orbits. The self-confined jet is launched from a finite radial zone in the disk which remains constant over time. Ejection is made possible because the magnetization reaches unity at the disk surface, due to the steep density decrease. However, no ejection is reported when the midplane magnetization becomes too small. The asymptotic jet velocity remains nevertheless too low to explain observed jets due to the negligible power carried away by the jet. Astrophysical disks with superheated surface layers could drive analogous outflows even if their midplane magnetization is low. Sufficient angular momentum would be extracted by the turbulent viscosity to allow the accretion process to continue. The magnetized outflows would be no more than byproducts, rather than a fundamental driver of accretion. However, if the midplane magnetization increases towards the center, a natural transition to an inner jet dominated disk could be achieved.

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