论文标题

高能中微子发射后,超级质量黑洞合并后重力波辐射

High-energy neutrino emission subsequent to gravitational wave radiation from supermassive black hole mergers

论文作者

Yuan, Chengchao, Murase, Kohta, Kimura, Shigeo S., Mészáros, Péter

论文摘要

超级质量黑洞(SMBH)融合在宇宙的历史上无处不在,并且经常表现出强大的积聚活动和强大的喷气机。这些SMBH合并也是未来重力波探测器(例如激光空间内部天线(LISA))的有前途的候选。在这项工作中,我们认为中微子对应物发射来自喷射引起的冲击。实际情况是,在合并将向前推进磁盘材料之后,相对论的喷气式飞机发起,然后他们随后被直接进行,导致内部冲击,直接冲击,前向冲击和反向冲击形成。宇宙射线可以在这些地点加速,并通过摄影生产过程预期中微子。我们在其中制定了喷气结构和相关相互作用,然后评估每个冲击部位的中微子发射。我们发现,在宇宙射线载荷足够高并且可以实现极度超级埃德丁顿的振兴之后,在运行大约五到十年之内,Icecube-gen2可以在大约五到十年的运行案例中检测到引力波事件后的月份高能中微子发射。我们还估计了SMBH合并对弥漫性中微子强度的贡献,并发现观察到的非常高的能力($e_ν\ gtrsim1 $ pev)的很大一部分是Icecube中微子在乐观的情况下可能起源于它们。将来,这种中微子对应物以及引力波观测可以用多通电机的方法使用,以更详细地阐明SMBH合并的进化和物理机制。

Supermassive black hole (SMBH) coalescences are ubiquitous in the history of the Universe and often exhibit strong accretion activities and powerful jets. These SMBH mergers are also promising candidates for future gravitational wave detectors such as Laser Space Inteferometric Antenna (LISA). In this work, we consider neutrino counterpart emission originating from the jet-induced shocks. The physical picture is that relativistic jets launched after the merger will push forward inside the premerger disk wind material, and then they subsequently get collimated, leading to the formation of internal shocks, collimation shocks, forward shocks and reverse shocks. Cosmic rays can be accelerated in these sites and neutrinos are expected via the photomeson production process. We formulate the jet structures and relevant interactions therein, and then evaluate neutrino emission from each shock site. We find that month-to-year high-energy neutrino emission from the postmerger jet after the gravitational wave event is detectable by IceCube-Gen2 within approximately five to ten years of operation in optimistic cases where the cosmic-ray loading is sufficiently high and a mildly super-Eddington accretion is achieved. We also estimate the contribution of SMBH mergers to the diffuse neutrino intensity, and find that a significant fraction of the observed very high-energy ($E_ν\gtrsim1$ PeV) IceCube neutrinos could originate from them in the optimistic cases. In the future, such neutrino counterparts together with gravitational wave observations can be used in a multimessenger approach to elucidate in greater detail the evolution and the physical mechanism of SMBH mergers.

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