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arXiv 1007.5128astro-ph.GA
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赫歇尔空间望远镜对Sgr B2(M)方向氘代水的观测

Herschel observations of deuterated water towards Sgr B2(M)

Max-Planck-Institut für Radioastronomie(马克斯·普朗克射电天文研究所);I. Physikalisches Institut, Universität zu Köln(科隆大学第一物理研究所);California Institute of Technology(加州理工学院);Department of Astronomy, University of Michigan(密歇根大学天文学系)
Claudia Comito, Peter Schilke, Rainer Rolffs, D. C. Lis, A. Belloche, E. A. Bergin, T. G. Phillips, T. A. Bell, N. R. Crockett, S. Wang, G. A. Blake, E. Caux, C… 展开作者

Claudia Comito, Peter Schilke, Rainer Rolffs, D. C. Lis, A. Belloche, E. A. Bergin, T. G. Phillips, T. A. Bell, N. R. Crockett, S. Wang, G. A. Blake, E. Caux, C. Ceccarelli, J. Cernicharo, F. Daniel, M. -L. Dubernet, M. Emprechtinger, P. Encrenaz, M. Gerin, T. F. Giesen, J. R. Goicoechea, P. F. Goldsmith, H. Gupta, E. Herbst, C. Joblin, D. Johnstone, W. D. Langer, W. D. Latter, S. D. Lord, S. Maret, P. G. Martin, G. J. Melnick, K. M. Menten, P. Morris, H. S. P. Mueller, J. A. Murphy, D. A. Neufeld, V. Ossenkopf, J. C. Pearson, M. Perault, R. Plume, S. -L. Qin, S. Schlemmer, J. Stutzki, N. Trappe, F. F. S. van der Tak, C. Vastel, H. W. Yorke, S. Yu, M. Olberg, R. Szczerba, B. Larsson, R. Liseau, R. H. Lin, L. A. Samoska, E. Schlecht

AI总结:

本研究利用赫歇尔望远镜HIFI观测Sgr B2(M)的多条HDO跃迁线,结合RATRAN辐射转移模型,首次测定该区域全包层氘代水丰度随温度的分层分布,为水形成机制研究提供约束。

摘要:

HDO(氘代水)观测是水研究的重要补充,因为它们能对水的形成过程——即尘埃颗粒表面形成与气相高能过程(如激波中的过程)——给出强约束。本文呈现的利用HIFI(远红外外差仪器)对Sgr B2(M)中多条HDO跃迁线的观测,得以测定整个包层内的HDO丰度,这在以往仅依靠地面观测是无法实现的。研究采用球形蒙特卡洛辐射转移代码RATRAN对丰度结构进行建模,该模型还考虑了尘埃连续谱辐射产生的辐射抽运效应。建模结果显示,HDO丰度随温度急剧上升:温度低于100K的外包层丰度较低(2.5×10^-11),温度在100至200K之间的内包层/外核区域丰度中等(1.5×10^-9),而温度高于200K的热核区域丰度较高(3.5×10^-9)。

英文摘要:

Observations of HDO are an important complement for studies of water, because they give strong constraints on the formation processes -- grain surfaces versus energetic process in the gas phase, e.g. in shocks. The HIFI observations of multiple transitions of HDO in Sgr~B2(M) presented here allow the determination of the HDO abundance throughout the envelope, which has not been possible before with ground-based observations only. The abundance structure has been modeled with the spherical Monte Carlo radiative transfer code RATRAN, which also takes radiative pumping by continuum emission from dust into account. The modeling reveals that the abundance of HDO rises steeply with temperature from a low abundance ($2.5\times 10^{-11}$) in the outer envelope at temperatures below 100~K through a medium abundance ($1.5\times 10^{-9}$) in the inner envelope/outer core, at temperatures between 100 and 200~K, and finally a high abundance ($3.5\times 10^{-9}$) at temperatures above 200~K in the hot core.

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。

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