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首页> 外文期刊>Astronomy and astrophysics >The Herschel HIFI water line survey in the low-mass proto-stellar outflow L1448
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The Herschel HIFI water line survey in the low-mass proto-stellar outflow L1448

机译:低质量原恒星流出中的赫歇尔HIFI水线调查L1448

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Aims. As part of the WISH (Water In Star-forming regions with Herschel) key project, systematic observations of H2O transitions in young outflows are being carried out with the aim of understanding the role of water in shock chemistry and its physical and dynamical properties. We report on the observations of several ortho- and para-H2O lines performed with the HIFI instrument toward two bright shock spots (R4 and B2) along the outflow driven by the L1448 low-mass proto-stellar system, located in the Perseus cloud. These data are used to identify the physical conditions giving rise to the H2O emission and to infer any dependence on velocity. Methods. We used a large velocity gradient (LVG) analysis to derive the main physical parameters of the emitting regions, namely n(H2), Tkin, N(H2O) and emitting-region size. We compared these with other main shock tracers, such as CO, SiO and H2 and with shock models available in the literature. Results. These observations provide evidence that the observed water lines probe a warm (Tkin?~?400?600?K) and very dense (n?~?106?107?cm-3) gas that is not traced by other molecules, such as low-J CO and SiO, but is traced by mid-IR H2 emission. In particular, H2O shows strong differences with SiO in the excitation conditions and in the line profiles in the two observed shocked positions, pointing to chemical variations across the various velocity regimes and chemical evolution in the different shock spots. Physical and kinematical differences can be seen at the two shocked positions. At the R4 position, two velocity components with different excitation can be distinguished, of which the component at higher velocity (R4-HV) is less extended and less dense than the low velocity component (R4-LV). H2O column densities of about 2?×?1013 and 4?×?1014?cm-2 were derived for the R4-LV and the R4-HV components, respectively. The conditions inferred for the B2 position are similar to those of the R4-HV component, with H2O column density in the range 1014?5?×?1014?cm-2, corresponding to H2O/H2 abundances in the range 0.5?1?×?10-5. The observed line ratios and the derived physical conditions seem to be more consistent with excitation in a low-velocity J-type shock with strong compression rather than in a stationary C-shock, although none of these stationary models seems able to reproduce the whole characteristics of the observed emission.
机译:目的作为WISH(具有Herschel的恒星形成区域中的水)重点项目的一部分,正在对年轻流出物中H2O过渡进行系统观察,目的是了解水在冲击化学中的作用及其物理和动力学性质。我们报告了使用HIFI仪器对沿Perseus云中的L1448低质量原恒星系统驱动的流出流向两个明亮的冲击点(R4和B2)进行观测的正交和对H2O线的观测结果。这些数据用于识别引起H2O排放的物理条件,并推断对速度的任何依赖性。方法。我们使用大速度梯度(LVG)分析来得出发射区域的主要物理参数,即n(H2),Tkin,N(H2O)和发射区域大小。我们将它们与其他主要的冲击示踪剂(例如CO,SiO和H2)以及文献中可用的冲击模型进行了比较。结果。这些观察结果提供了证据,表明所观察到的水线探测到温暖的(Tkin?〜?400?600?K)和非常稠密的(n?〜?106?107?cm-3)气体,而其他分子(例如:低J CO和SiO,但可通过中红外H2排放来追踪。特别是,H2O在激发条件下和在两个观察到的冲击位置的线轮廓中显示出与SiO的强烈差异,这表明在各种速度范围内化学变化以及在不同冲击点的化学演化。在两个震惊位置可以看到身体和运动上的差异。在R4位置,可以区分出两个具有不同激励的速度分量,其中速度较高的分量(R4-HV)的扩展性和密度都低于低速分量(R4-LV)。对于R4-LV和R4-HV组分,分别得出约2Ω×≤1013和4Ω×≤1014Ω·cm-2的H 2 O柱密度。 B2位置的推断条件与R4-HV组分的条件相似,H2O柱密度在1014?5?×?1014?cm-2的范围内,对应于H2O / H2丰度在0.5?1?3的范围内。 ××10-5。观察到的线宽比和导出的物理条件似乎与在强压缩下的低速J型冲击而不是固定C冲击中的激励更加一致,尽管这些固定模型似乎都无法重现整个特征观察到的排放量。

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