论文标题

全局GRHD模拟中的流式流和河盘相互作用形成和馈送的潮汐破坏磁盘

Tidal Disruption Disks Formed and Fed by Stream-Stream and Stream-Disk Interactions in Global GRHD Simulations

论文作者

Andalman, Zachary L., Liska, Matthew T. P., Tchekhovskoy, Alexander, Coughlin, Eric R., Stone, Nicholas

论文摘要

当一颗星星靠近超级质量黑洞(BH)时,BH的潮汐力将其撕成薄的溪流,导致潮汐破坏事件(TDE)。在这项工作中,我们使用我们的GPU加速代码H-AMR研究了一般相对论流体动力学(GRHD)中TDE的干扰后阶段。我们对具有现实系统参数的深渗透TDE($β$ = 7)进行了第一个基于网格的模拟:黑洞与星级的质量比为$ 10^6 $,抛物线质体轨迹和非零BH旋转。我们还对倾斜的TDE进行了模拟,其恒星轨道相对于BH中平面倾斜。我们表明,对于我们对齐的TDE,由于轨道能量耗散$ \ sim,$ \ sim $ 20%到达BH的轨道能量而导致的积聚盘形式。耗散最初是由暴力自我交流所占据的,后来又由周围的溪流相互作用。自我交流完全破坏了传入的流,导致五个不同的自我交流事件大约12小时分开,并散发出积聚率。我们还发现,磁盘是偏心的,平均偏心度E $ \ $ \ $ 0.88。对于我们倾斜的TDE,我们只发现由于周围的淋巴结进攻而导致部分自身交流。尽管这些部分相交从轨道平面弹出气体,但积聚的盘仍形成,其材料的积分分数与对齐情况相似。这些结果对磁盘形成在现实的潮汐破坏中具有重要意义。例如,完全流中断引起的积聚率的周期性可能解释了Swift J1644+57的爆发事件。

When a star passes close to a supermassive black hole (BH), the BH's tidal forces rip it apart into a thin stream, leading to a tidal disruption event (TDE). In this work, we study the post-disruption phase of TDEs in general relativistic hydrodynamics (GRHD) using our GPU-accelerated code H-AMR. We carry out the first grid-based simulation of a deep-penetration TDE ($β$=7) with realistic system parameters: a black-hole-to-star mass ratio of $10^6$, a parabolic stellar trajectory, and a nonzero BH spin. We also carry out a simulation of a tilted TDE whose stellar orbit is inclined relative to the BH midplane. We show that for our aligned TDE, an accretion disk forms due to the dissipation of orbital energy with $\sim$20 percent of the infalling material reaching the BH. The dissipation is initially dominated by violent self-intersections and later by stream-disk interactions near the pericenter. The self-intersections completely disrupt the incoming stream, resulting in five distinct self-intersection events separated by approximately 12 hours and a flaring in the accretion rate. We also find that the disk is eccentric with mean eccentricity e$\approx$0.88. For our tilted TDE, we find only partial self-intersections due to nodal precession near pericenter. Although these partial intersections eject gas out of the orbital plane, an accretion disk still forms with a similar accreted fraction of the material to the aligned case. These results have important implications for disk formation in realistic tidal disruptions. For instance, the periodicity in accretion rate induced by the complete stream disruption may explain the flaring events from Swift J1644+57.

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