arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1007.5470astro-ph.GA
收藏

赫歇尔对异常源的观测(HEXOS):对猎户座KL方向H2O及其同位素体的观测

Herschel observations of EXtra-Ordinary Sources (HEXOS): Observations of H2O and its isotopologues towards Orion KL

Harvard-Smithsonian Center for Astrophysics(哈佛-史密森天体物理中心);Johns Hopkins University(约翰斯·霍普金斯大学);University of Michigan(密歇根大学);California Institute of Technology(加州理工学院);LERMA & UMR8112 du CNRS, Observatoire de Paris(巴黎天文台 LERMA 及 CNRS UMR8112)
G. J. Melnick, V. Tolls, D. A. Neufeld, E. A. Bergin, T. G. Phillips, S. Wang, N. R. Crockett, T. A. Bell, G. A. Blake, S. Cabrit, E. Caux, C. Ceccarelli, J. Ce… 展开作者

G. J. Melnick, V. Tolls, D. A. Neufeld, E. A. Bergin, T. G. Phillips, S. Wang, N. R. Crockett, T. A. Bell, G. A. Blake, S. Cabrit, E. Caux, C. Ceccarelli, J. Cernicharo, C. Comito, F. Daniel, M. -L. Dubernet, M. Emprechtinger, P. Encrenaz, E. Falgarone, M. Gerin, T. F. Giesen, J. R. Goicoechea, P. F. Goldsmith, E. Herbst, C. Joblin, D. Johnstone, W. D. Langer, W. D. Latter, D. C. Lis, S. D. Lord, S. Maret, P. G. Martin, K. M. Menten, P. Morris, H. S. P. Muller, J. A. Murphy, V. Ossenkopf, L. Pagani, J. C. Pearson, M. Perault, R. Plume, S. -L. Qin, M. Salez, P. Schilke, S. Schlemmer, J. Stutzki, N. Trappe, F. F. S. van der Tak, C. Vastel, H. W. Yorke, S. Yu, J. Zmuidzinas

AI总结:

本研究利用Herschel/HIFI首次在猎户座KL探测到大量水及其同位素的基转动态跃迁谱线,通过拟合和逃逸概率法推导各成分水丰度,揭示暖尘埃导致的水冰升华增强现象。

摘要:

我们利用Herschel/HIFI(赫歇尔空间天文台的外差式远红外仪),报告了在猎户座KL方向的发射和吸收谱中,探测到超过48条速度分辨的H₂¹⁶O、H₂¹⁸O和H₂¹⁷O基转动态跃迁谱线——其中大部分为首次探测。我们表明,通过约束以匹配视线方向已知发射和吸收成分的简单拟合,与所有水谱线的谱形吻合极佳。利用受线 opacity(不透明度)影响小于H₂¹⁶O对应谱线的H₂¹⁸O谱线流量,结合逃逸概率方法,我们推导了与每个发射成分相关的H₂¹⁸O柱密度。我们推断出平台区、热核和延展暖气体的总水丰度分别为7.4E-5、1.0E-5和1.6E-5。对于平台区,该值与此前猎户座KL水丰度的测量结果以及其他分子外流的水丰度一致。对于热核和延展暖气体,这些值略高于其他静止云团推导的水丰度,表明这些区域可能正因源内更暖的尘埃,而经历着颗粒表面水冰升华增强(以及冻结减少)的过程。

英文摘要:

We report the detection of more than 48 velocity-resolved ground rotational state transitions of H2(16)O, H2(18)O, and H2(17)O - most for the first time - in both emission and absorption toward Orion KL using Herschel/HIFI. We show that a simple fit, constrained to match the known emission and absorption components along the line of sight, is in excellent agreement with the spectral profiles of all the water lines. Using the measured H2(18)O line fluxes, which are less affected by line opacity than their H2(16)O counterparts, and an escape probability method, the column densities of H2(18)O associated with each emission component are derived. We infer total water abundances of 7.4E-5, 1.0E-5, and 1.6E-5 for the plateau, hot core, and extended warm gas, respectively. In the case of the plateau, this value is consistent with previous measures of the Orion-KL water abundance as well as those of other molecular outflows. In the case of the hot core and extended warm gas, these values are somewhat higher than water abundances derived for other quiescent clouds, suggesting that these regions are likely experiencing enhanced water-ice sublimation from (and reduced freeze-out onto) grain surfaces due to the warmer dust in these sources.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑