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Physical Conditions in Shocked Regions of Orion from Ground-based Observations of H[TINF]2[/TINF]O
Author(s) -
J. Cernicharo,
J. R. Pardo,
E. González-Alfonso,
Eugene Serabyn,
T. G. Phillips,
Dominic J. Benford,
David M. Mehringer
Publication year - 1999
Publication title -
the astrophysical journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.376
H-Index - 489
eISSN - 1538-4357
pISSN - 0004-637X
DOI - 10.1086/312164
Subject(s) - ridge , plateau (mathematics) , observatory , telescope , physics , astrophysics , line (geometry) , water vapor , orion nebula , meteorology , geology , stars , mathematical analysis , paleontology , geometry , mathematics
We present observations of the 5$_{1,5}\to4_{2,2}$ transition of water vaporat 325.15 GHz taken with the CSO telescope towards Orion IRc2. The emission ismore extended than that of other molecular species such as CH$_3$OH. However,it is much less extended than the emission of water vapor at 183.31 GHzreported by Cernicharo et al (1994). A comparison of the line intensities at325.15 GHz and 183.31 GHz puts useful constraints on the density andtemperature of the emitting regions and allows an estimate of H_2O abundance,x(H_2O), of $\simeq10^{-4}$ in the Plateau and $\simeq10^{-6}-10^{-5}$ in theRidge.Comment: 4 figure

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