论文标题

尘埃辐射的喷气式飞机I.固定磁盘风中的分子形成

Molecule formation in dust-poor irradiated jets I. Stationary disk winds

论文作者

Tabone, B., Godard, B., Forêts, G. Pineau des, Cabrit, S., van Dishoeck, E. F.

论文摘要

最近的ALMA观察结果表明,分子原始喷气机的最高速度部分是从增生磁盘的尘埃 - 燃烧区域发射的(<0.3 AU)。然而,在存在刺激性的宽辐射场和没有灰尘的情况下,内部原始磁盘风中分子的形成和存活仍未得到探索。我们的目的是确定在快速且无限制的无尘盘风中可以合成和幸免的简单分子,或者是否需要一小部分灰尘来解释观察到的分子丰度。这项工作基于旨在建模辐照环境的巴黎 - 德拉姆冲击法规。从单点模型研究了无尘化学的基本特性。然后,使用参数流几何形状构建层层1D磁盘风模型。该模型包括时间依赖性化学和通过气相光程序对辐射场的衰减。我们表明,主要通过H-途径形成的一小部分H2(<1E-2)可以有效地启动分子合成,例如CO和SIO在TK〜800 K上方。原子种类(例如C,Si,S)通过连续的自我射击进行原子种类(例如C,SI,SI)进行辐射场的衰减。此过程可确保通过中性反应和这些分子的存活率有效地形成CO,OH,SIO,H2O。如果温暖(TK> 800 K),则0类无尘风降低质量损失率($ \ dot {m} _W> $ 2e-6 msun/yr)的分子富含分子(TK> 800 K)。磁盘风的分子含量对灰尘的存在非常敏感,而存活的灰尘的质量小至1E-5显着增加了H2O和SIO的丰度。高速喷气机的化学反应是一种强大的工具,可以在灰尘中探测其内容并揭示其发射点。需要内部冲击模型,以充分利用当前(亚)毫米观测并准备未来的JWST观测值。

Recent ALMA observations suggest that the highest velocity part of molecular protostellar jets are launched from the dust-sublimation regions of the accretion disks (<0.3 au). However, formation and survival of molecules in inner protostellar disk winds, in the presence of a harsh FUV radiation field and the absence of dust, remain unexplored. We aim at determining if simple molecules can be synthesized and spared in fast and collimated dust-free disk winds or if a fraction of dust is necessary to explain the observed molecular abundances. This work is based on the Paris-Durham shock code designed to model irradiated environments. Fundamental properties of the dust-free chemistry are investigated from single point models. A laminar 1D disk wind model is then built using a parametric flow geometry. This model includes time-dependent chemistry and the attenuation of the radiation field by gas-phase photoprocesses. We show that a small fraction of H2 (< 1e-2), primarily formed through the H- route, can efficiently initiate molecule synthesis such as CO and SiO above TK ~ 800 K. The attenuation of the radiation field by atomic species (eg. C, Si, S) proceeds through continuum self-shielding. This process ensures efficient formation of CO, OH, SiO, H2O through neutral-neutral reactions, and the survival of these molecules. Class 0 dust-free winds with high mass-loss rates ($\dot{M}_w >$ 2e-6 Msun/yr) are predicted to be rich in molecules if warm (TK > 800 K). The molecular content of disk winds is very sensitive to the presence of dust and a mass-fraction of surviving dust as small as 1e-5 significantly increases the H2O and SiO abundances. Chemistry of high-velocity jets is a powerful tool to probe their content in dust and uncover their launching point. Models of internal shocks are required to fully exploit the current (sub-)millimeter observations and prepare future JWST observations.

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