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arXiv 2503.02433astro-ph.SRastro-ph.GA
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DG Tau A 低速星风的光谱天体测量研究

A Spectroastrometric Study of the Low-velocity Wind from DG Tau A

Yu-Ru Chou, Michihiro Takami, Shin-Ping Lai, Emma Whelan, Noah B. Otten, Min Fang, Akito Tajitsu, Masaaki Otsuka, Hsien Shang, Chun-Fan Liu, Jennifer Karr, Aisling Murphy

AI总结:

利用昴星团HDS首次对DG Tau A开展高分辨率光谱天体测量,在禁线中探测到低速广角星风并估算其质量损失率下限,同时识别出与准直喷流激波相关的高速成分,指出观测更支持X-wind模型。

摘要:

我们首次使用昴星团高色散光谱仪(HDS)获得了 DG Tau A 在 4800 Å 至 7500 Å 范围内的高光谱分辨率光谱(Δv ∼ 2.5 km s⁻¹)。在 [O I] 5577、6300、6364 Å 和 [S II] 6716、6731 Å 谱线中观测到了低速成分(LVCs,|v| < 100 km s⁻¹)。在 LVCs 中观测到的偏移位置光谱显示出“负速度梯度”,支持存在与 LVC 发射相关的广角星风。在 LVC 速度范围内介于 -16 km s⁻¹ 至 -41 km s⁻¹ 之间的一个成分,即 LVC-M,其偏移位置光谱也显示出“负速度梯度”,支持广角星风的存在。利用光谱天体测量法测得的风长度为 12–70 au,我们估计风的质量损失率下限约为 10⁻⁸ M⊙ yr⁻¹。除 LVCs 外,我们在 26 条谱线([N I]、[N II]、[O I]、[O II]、[O III]、[S II]、[Ca II]、[Fe II]、Hα、Hβ、He I)中识别出两个与准直喷流相关的高速成分(HVCs,|v| > 100 km s⁻¹)。其中一个相对恒星具有明显空间偏移(n_e ∼ 10⁴ cm⁻³,HVC1),与喷流的内部激波面相关;另一个位于喷流底部(n_e ∼ 10⁶ cm⁻³,HVC2),可能是驻定激波成分。我们发现观测到的谱线轮廓和 LVC 发射的空间尺度与现有光致蒸发盘风或磁流体动力学(MHD)盘风的预测不一致。这些现象可以用 X-wind 模型解释,但详细比较仍需合成观测。

英文摘要:

We obtained high spectral resolution spectra ($Δv$ $\sim$ 2.5 km s$^{-1}$) for DG Tau A from 4800 Å to 7500 Å using Subaru High Dispersion Spectrograph (HDS) for the first time. The low-velocity components (LVCs, |$v$| < 100 km s$^{-1}$) were observed in the [O I] 5577, 6300, 6364 Å, [S II] 6716, 6731 Å lines. The offset position spectra observed in the LVCs show a "negative velocity gradient", supporting the presence of a wide-angled wind associated with the LVC emission. The offset position spectra observed in a component within the LVC velocity range between -16 km s$^{-1}$ to -41 km s$^{-1}$, namely, LVC-M, show a "negative velocity gradient'', supporting the presence of a wide-angled wind. With 12-70 au wind lengths measured using spectroastrometry, we estimate a lower limit to the wind mass-loss rate of $\sim$10$^{-8}$ M$_\odot$ yr$^{-1}$. In addition to the LVCs, we identify two high-velocity components (HVCs, |$v$| > 100 km s$^{-1}$) associated with the collimated jet in 26 lines ([N I], [N II], [O I], [O II], [O III], [S II], [Ca II], [Fe II], H$α$, H$β$, He I). The one with a clear spatial offset from the star ($n_e$ $\sim$10$^4$ cm$^{-3}$, HVC1) is associated with an internal shock surface of the jet, while the other at the base ($n_e$ $\sim$10$^6$ cm$^{-3}$, HVC2) may be a stationary shock component. We find that the observed line profiles and the spatial scales of the LVC emission do not agree with the existing predictions for photoevaporative or magnetohydrodynamical (MHD) disk winds. These could be explained by the X-wind model, but synthetic observations are required for detailed comparisons.

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