GSN 069盘演化和长周期潮汐破坏事件性质的时间依赖解

M. Guolo, A. Mummery, A. Ingram, M. Nicholl, S. Gezari and E. Nathan
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引用次数: 0

摘要

我们提出了一个基于光曲线拟合包的完全时变相对论盘模型的实现,该模型拟合到x射线光谱拟合环境pyXspec中。这种实现可以同时拟合多历元和多波长的光谱数据,其中唯一的自由参数是描述黑洞和初始条件的参数,而随后的演化则由不断演化的吸积流的动力学方程控制。我们用它拟合了从2010年到2019年底的“长寿命”潮汐破坏事件(TDE)和准周期性喷发(QPE)源GSN 069的7个x射线光谱和2个紫外光谱。我们的研究结果表明,这种“长寿命”的x射线明亮的tdes (GSN 069是一个主要的例子,但不是唯一的例子)可以自然地用与ASASSN-14li和AT2019dsg等短寿命x射线发射事件相同的框架来解释。它们的区别在于“粘性”时间尺度参数——与圆盘的角动量传输效率有关——在模拟瞬态事件的圆盘演化时,它应该被视为一个自由参数。我们通过跟踪磁盘属性(如质量表面密度和吸积速率)的时间演化来研究QPE模型的含义。我们认为,现有的QPE模型可能无法重现观测到的喷发存在(2018年)或不存在(2014年)与圆盘性质之间的联系。在轨道-圆盘碰撞模型的背景下,质量表面密度的变化似乎不足以解释喷发温度所需的变化。GSN 069在2014年没有爆发,这对QPE模型来说仍然是一个挑战。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Time-dependent Solution for GSN 069 Disk Evolution and the Nature of Long-lived Tidal Disruption Events
We present the implementation of a fully time-dependent relativistic disk model—based on the light-curve fitting package FitTeD—into the X-ray spectral fitting environment, pyXspec. This implementation enables simultaneous fitting of multi-epoch and multiwavelength spectral data, where the only free parameters are those describing the black hole and the initial conditions, while the subsequent evolution is governed by the dynamical equations of an evolving accretion flow. We use it to fit seven epochs of X-ray spectra and two epochs of UV spectra of the “long-lived” tidal disruption event (TDE) and quasiperiodic eruption (QPE) source GSN 069, from 2010 through late-2019. Our results show that such “long-lived,” X-ray-bright TDEs—of which GSN 069 is a prime, but not unique, example—can naturally be explained within the same framework as events with shorter-lived X-ray emission, like ASASSN-14li and AT2019dsg. Their distinction lies in the “viscous” timescale parameter—tied to the disk’s angular momentum transport efficiency—which should be treated as a free parameter when modeling the disk evolution of transient events. We examine the implications for QPE models by tracking the time evolution of disk properties such as mass surface density and accretion rate. We argue that existing QPE models may not be able to reproduce the observed connection between the presence (2018) or absence (2014) of eruptions and the disk properties. In the context of orbiter–disk collision models, the change in mass surface density appears insufficient to explain the needed variation in the eruption’s temperature. The absence of eruptions in GSN 069 in 2014 remains a challenge for QPE models.
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