Abstract
Context. Water is a key molecule in the star formation process, but its spatial distribution in star-forming regions is not well known. Aims. We study the distribution of dust continuum and H2O and 13CO line emission in DR21, a luminous star-forming region with a powerful outflow and a compact H ii region. Methods. Herschel-HIFI spectra near 1100 GHz show narrow 13CO 10-9 emission and H2O 111-000 absorption from the dense core and broad emission from the outflow in both lines. The H2O line also shows absorption by a foreground cloud known from ground-based observations of low-J CO lines. Results. The dust continuum emission is extended over 36" FWHM, while the 13CO and H 2O lines are confined to ≈ 24" or less. The foreground absorption appears to peak further North than the other components. Radiative transfer models indicate very low abundances of ∼2×10-10 for H2O and ∼8×10-7 for 13CO in the dense core, and higher H2O abundances of ∼4×10-9 in the foreground cloud and ∼7×10-7 in the outflow. Conclusions. The high H2O abundance in the warm outflow is probably due to the evaporation of water-rich icy grain mantles, while the H2O abundance is kept down by freeze-out in the dense core and by photodissociation in the foreground cloud.
Originalsprog | Engelsk |
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Artikelnummer | L107 |
Tidsskrift | Astronomy and Astrophysics |
Vol/bind | 518 |
Udgave nummer | 4 |
ISSN | 0004-6361 |
DOI | |
Status | Udgivet - 15 okt. 2010 |