arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2212.00514astro-ph.SRastro-ph.EPastro-ph.GA
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模拟DG Tau B中CO外流:后掠壳体与扰动MHD盘风

Modeling the CO outflow in DG Tau B: Swept-up shells versus perturbed MHD disk wind

A. de Valon, C. Dougados, S. Cabrit, F. Louvet, L. A. Zapata, D. Mardones

摘要:

外流的起源及其对盘演化和行星形成的确切影响仍然是关键的悬而未决的问题。DG Tau B是一颗I类原恒星,伴随着旋转的锥形CO外流和结构盘。因此,它是研究这些问题的理想对象。我们的目标是描述DG Tau B外流的形态和运动学特征,以阐明其起源和对磁盘的潜在影响。我们的分析基于阿塔卡马大型毫米波阵列(ALMA)12 CO(2-1)以20 au角分辨率对DG Tau B的观测。我们表征三种不同类型的子结构在这个流出(拱,手指,尖)与明显的加速度。具有哈勃定律的风力驱动的壳模型无法解释这些子结构。相反,锥形流的形态学和运动学都可以用稳定的锥形磁流体动力(MHD)盘风来解释,其足点半径r 0 = 0.7-3.4 au,小磁水平臂参数λ < 1.6)和准周期性亮度增强。这些可能是由喷气弓冲击,源轨道运动所造成的25兆焦耳的同伴在50天文单位,或磁盘密度扰动通过风发射区吸积的影响。大的CO风质量通量(吸积率的四倍到中心恒星)也可以解释,如果MHD磁盘风删除了大部分的角动量所需的稳定磁盘吸积。我们的研究结果提供了最有力的证据,到目前为止,存在大量的MHD盘风在I类源与残留的下落,他们认为,初始阶段的行星形成发生在一个高度动态的环境。

英文摘要:

The origin of outflows and their exact impact on disk evolution and planet formation remain crucial open questions. DG Tau B is a Class I protostar associated with a rotating conical CO outflow and a structured disk. Hence it is an ideal target to study these questions. We aim to characterize the morphology and kinematics of the DG Tau B outflow in order to elucidate its origin and potential impact on the disk. Our analysis is based on Atacama Large Millimeter Array (ALMA) 12CO(2-1) observations of DG Tau B at 20 au angular resolution. We characterize three different types of substructures in this outflow (arches, fingers, and cusps) with apparent acceleration. Wind-driven shell models with a Hubble law fail to explain these substructures. In contrast, both the morphology and kinematics of the conical flow can be explained by a steady conical magnetohydrodynamic (MHD) disk wind with foot-point radii r0= 0.7-3.4 au, a small magnetic level arm parameter lambda < 1.6), and quasi periodic brightness enhancements. These might be caused by the impact of jet bow shocks, source orbital motion caused by a 25 MJ companion at 50 au, or disk density perturbations accreting through the wind launching region. The large CO wind mass flux (four times the accretion rate onto the central star) can also be explained if the MHD disk wind removes most of the angular momentum required for steady disk accretion. Our results provide the strongest evidence so far for the presence of massive MHD disk winds in Class I sources with residual infall, and they suggest that the initial stages of planet formation take place in a highly dynamic environment.

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