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Squeezed between shells? The origin of the Lupus I molecular cloud - II. APEX CO and GASS H?i observations

机译:夹在壳之间?狼疮I分子云的起源-II。 APEX CO和GASS H?i观测

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Context. Lupus I cloud is found between the Upper Scorpius (USco) and Upper Centaurus-Lupus (UCL) subgroups of the Scorpius-Centaurus OB association, where the expanding USco H?I shell appears to interact with a bubble currently driven by the winds of the remaining B stars of UCL. Aims. We investigate whether the Lupus I molecular could have formed in a colliding flow, and in particular, how the kinematics of the cloud might have been influenced by the larger scale gas dynamics. Methods. We performed APEX ~(13)CO (2–1)and C~(18)O (2–1) line observations of three distinct parts of Lupus I that provide kinematic information on the cloud at high angular and spectral resolution. We compare those results to the atomic hydrogen data from the GASS H? i survey and our dust emission results presented in the previous paper. Based on the velocity information, we present a geometric model for the interaction zone between the USco shell and the UCL wind bubble. Results. We present evidence that the molecular gas of Lupus Iis tightly linked to the atomic material of the USco shell. The CO emission in Lupus Iis found mainly at velocities between v _(LSR)= 3 – 6 km s~(-1) , which is in the same range as the H? i velocities. Thus, the molecular cloud is co-moving with the expanding USco atomic H? i shell. The gas in the cloud shows a complex kinematic structure with several line-of-sight components that overlay each other. The nonthermal velocity dispersion is in the transonic regime in all parts of the cloud and could be injected by external compression. Our observations and the derived geometric model agree with a scenario in which Lupus Iis located in the interaction zone between the USco shell and the UCL wind bubble. Conclusions. The kinematics observations are consistent with a scenario in which the Lupus Icloud formed via shell instabilities. The particular location of Lupus I between USco and UCL suggests that counterpressure from the UCL wind bubble and pre-existing density enhancements, perhaps left over from the gas stream that formed the stellar subgroups, may have played a role in its formation.
机译:上下文。在天蝎座-半人马座OB协会的上天蝎座(USco)和上半人马座-天蝎座(UCL)子群之间发现了狼疮I云,正在膨胀的USco H?I壳似乎与当前由大风推动的泡沫相互作用。 UCL剩下的B星。目的我们研究了狼疮I分子是否可能在碰撞流中形成,特别是,大尺度的气体动力学如何影响云的运动学。方法。我们对狼疮I的三个不同部分进行了APEX〜(13)CO(2-1)和C〜(18)O(2-1)线观测,以高角度和光谱分辨率在云上提供了运动学信息。我们将这些结果与来自GASS H?的氢原子数据进行比较。我进行了调查,并在上一篇论文中介绍了我们的粉尘排放结果。基于速度信息,我们提出了USco壳层和UCL气泡之间相互作用区域的几何模型。结果。我们提供的证据表明狼疮I的分子气体与USco壳的原子材料紧密相连。狼疮I的CO排放主要在v _(LSR)= 3 – 6 km s〜(-1)之间的速度范围内,该速度与H?的范围相同。我的速度。因此,分子云正在与不断扩展的USco原子H?我炮弹。云中的气体显示出复杂的运动学结构,具有多个相互重叠的视线组件。非热速度色散在云的所有部分都处于跨音速状态,可以通过外部压缩来注入。我们的观察结果和导出的几何模型与“狼疮” Iis位于USco壳层和UCL气泡之间的相互作用带中的情况相吻合。结论。运动学观察结果与通过壳层不稳定性形成狼疮Icloud的情况一致。狼疮一号位于USco和UCL之间的特殊位置表明,来自UCL气泡的反压和先前存在的密度增强(可能是形成恒星亚组的气流遗留下来的)可能在其形成中发挥了作用。

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