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arXiv 2610.01226astro-ph.SR

通过高分辨率光学光谱探测V1180 Cas中的吸积与外流

Probing Accretion and Outflow in V1180 Cas through High-Resolution Optical Spectroscopy

  • Aryabhatta Research Institute of Observational Sciences (ARIES)(阿里亚巴塔观测科学研究所)
  • M.J.P. Rohilkhand University(M.J.P.罗希尔坎德大学)
  • Department of Astronomy and Astrophysics Tata Institute of Fundamental Research (TIFR)(塔塔基础研究院天文与天体物理系)
  • Instituto de Radioastronomía y Astrofísica, Universidad Nacional Autónoma de México(墨西哥国立自治大学射电天文学与天体物理研究所)
  • Indian Institute of Technology (IIT) Roorkee(印度理工学院勒克瑙分校)
  • Bareilly College(巴雷利学院)

机构由 AI 辅助整理,请以论文原文为准。

Tarak Chand, Saurabh Sharma, Koshvendra Singh, Joe P. Ninan, Arpan Ghosh, Devendra K. Ojha, Jyotirmoy Dey, Manojit Chakraborty, Kartik Gokhe, Aayushi Verma, Mamta, Ajay Kumar Singh

AI总结:

通过Keck HIRES高分辨率光谱分析V1180 Cas,首次测定其视向速度与盘倾角,揭示吸积与外流特征,支持多成分外流模型。

AI中文摘要:

我们展示了在W. M. Keck天文台使用HIRES获取的V1180 Cas高分辨率光学光谱的分析结果,该光谱是在源处于明亮光度状态时获得的。光谱以强发射线为主,包括H$\alpha$、Ca II红外三重线、He I和O I,以及众多Fe I和Fe II跃迁线和若干禁线如[O I]和[S II],表明正在进行的吸积和质量损失活动。微弱的Li I $\lambda$6708吸收特征证实了该源的年轻性。利用Li I吸收线和选定的Fe I发射线,我们首次报告了V1180 Cas的视向速度为$-16 \pm 3$ km s$^{-1}$。H$\alpha$和H$\beta$轮廓呈现出不对称结构,带有蓝移吸收成分,表明沿视线方向存在外流物质。He I $\lambda$5876线显示出窄成分,可能与激波后吸积区域相关,以及一个宽的、略微蓝移的成分,可能来自磁层流和/或内盘风。[O I] $\lambda$6300轮廓被分解为低速和高速成分,分别追踪慢盘风和快喷流。利用禁线[O I],我们首次估计了盘倾角约为$50^\circ$。推导出的质量吸积率和喷流质量损失率表明$\dot{M}_{jet}/\dot{M}_{acc} \sim 0.01$--$0.03$,处于Class II YSOs观测范围的下端,但与其一致。禁线诊断表明密度约为$10^{3}$和$10^{6}$ cm$^{-3}$,温度约为$10^{4}$ K,支持多成分外流情景。总体而言,结果支持V1180 Cas是一个活跃吸积、中等倾角系统,拥有多成分外流的图像。

英文摘要:

We present an analysis of a high-resolution optical spectrum of V1180 Cas obtained with HIRES at the W. M. Keck Observatory during a bright photometric state of the source. The spectrum is dominated by strong emission lines, including H$α$, the Ca II infrared triplet, He I, and O I, along with numerous Fe I and Fe II transitions and several forbidden lines such as [O I] and [S II], indicating ongoing accretion and mass-loss activity. A weak Li I $λ$6708 absorption feature confirms the youth of the source. Using the Li I absorption and selected Fe I emission lines, we report for the first time a radial velocity of $-16 \pm 3$ km s$^{-1}$ for V1180 Cas. The H$α$ and H$β$ profiles exhibit asymmetric structures with blueshifted absorption components, suggesting outflowing material along the line of sight. The He I $λ$5876 line displays a narrow component likely associated with post-shock accretion regions and a broad, slightly blueshifted component probably arising from magnetospheric flows and/or inner disk winds. The [O I] $λ$6300 profile is decomposed into low- and high-velocity components, tracing a slow disk wind and a fast jet. Using the forbidden [O I] line, we estimate for the first time a disk inclination angle of $\approx50^\circ$. The derived mass accretion and jet mass-loss rates imply $\dot{M}_{jet}/\dot{M}_{acc} \sim 0.01$--$0.03$, at the lower end of, but consistent with, the range observed for Class II YSOs. Forbidden-line diagnostics indicate densities $\sim10^{3}$ and $10^{6}$ cm$^{-3}$ with temperatures of $\sim10^{4}$ K, supporting a multi-component outflow scenario. Overall, the results support a picture in which V1180 Cas is an actively accreting, moderately inclined system hosting a multi-component outflow.

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