Anisotropic wind in tidal disruption events
潮汐瓦解事件中的各向异性风
Over the coming years, the number of tidal disruption events (TDEs) is expected to substantially increase with observations from the Vera Rubin Observatory (g and r band) and {\it ULTRASAT} (near UV) wide-field surveys. These future samples have great promise to characterize the bottom end of the massive black hole mass function, but existing detections of intermediate mass black hole TDEs are primarily in X-rays, leaving their optical/UV emission largely unexplored. We present a time- and angle-dependent analysis of the outflow produced by dissipation near pericentre in a three-dimensional end-to-end radiation-hydrodynamics simulation of a TDE by a $10^4 M_\odot$ black hole with realistic parameters, run with the code RICH. We find that outflow anisotropy produces viewing-angle-dependent observables. Towards the poles and the pericentre region, mass-loss rates are low and bolometric luminosities reach $\sim2$--$3$ times the Eddington luminosity. Towards the stream, the properties show a stronger dependence on latitude: the mass-loss rate increases and the bolometric luminosity decreases as the line of sight approaches the orbital plane. These denser regions favour H$α$ and H$β$ emission. Despite these variations, all viewing directions show a common spectral evolution, with an initial soft X-ray flare followed (around $1.25t_{\rm fb}\approx3$~days) by the reprocessing of shock-powered emission into the UV and optical bands. Although the optical/UV luminosities we predict for this TDE are likely too dim for past surveys (e.g. ASAS-SN, ZTF), they are within the detection capabilities of LSST and ULTRASAT to horizons of $\sim 790$ and $\sim 340$ Mpc, respectively, for the brightest viewing directions.
展开 ▾在无吸积盘情况下,由喷嘴激波驱动的各向异性风即可形成再处理层,且外流性质同时依赖纬度和经度;对 IMBH TDE 的光学/UV 可探测性给出视向角相关的预测,为未来巡天发现 IMBH TDE 提供依据。
过去对 TDE 早期光学/UV 辐射的起源长期存在吸积盘再处理与激波耗散之争;统一模型提出视向角决定 X 射线与光学辐射比例,如 Dai+ 2018、Thomsen+ 2022,而 Parkinson+ 2025 指出三维辐射转移对避免高估光子俘获至关重要。本文延续 Martire+ 2026 的端到端三维辐射流体模拟,进一步分析 IMBH TDE 中由喷嘴激波驱动的各向异性风,发现无需吸积盘即可形成再处理层,且外流性质同时依赖纬度和经度,这与 Steinberg+ 2024 及 Giron+ 2026 的方法相互印证。展望上,未来需结合蒙特卡洛后处理(如 Roth+ 2016、Mockler+ 2026)细化谱线预测,而 LSST 与 ULTRASAT 有望突破现有 ZTF 局限,发现一批 IMBH TDE,为检验黑洞质量函数低端与种子黑洞形成模型提供关键样本。
预印本 2026-09-09 · 收录 2026-09-10