4.6 Article

Odin observations of water in molecular outflows and shocks

Journal

ASTRONOMY & ASTROPHYSICS
Volume 507, Issue 3, Pages 1455-U296

Publisher

EDP SCIENCES S A
DOI: 10.1051/0004-6361/200912064

Keywords

ISM: jets and outflows; ISM: molecules; stars: pre-main sequence; ISM: supernova remnants

Funding

  1. Swedish National Space Board (SNSB)
  2. Canadian Space Agency (CSA)
  3. National Technology Agency of Finland (Tekes)
  4. Centre National d'Etude Spatiale (CNES)

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Aims. We investigate the ortho-water abundance in outflows and shocks in order to improve our knowledge of shock chemistry and of the physics behind molecular outflows. Methods. We used the Odin space observatory to observe the H(2)O(1(10)-1(01)) line. We obtain strip maps and single pointings of 13 outflows and two supernova remnants where we report detections for eight sources. We used RADEX to compute the beam averaged abundances of o-H(2)O relative to H(2). In the case of non-detection, we derive upper limits on the abundance. Results. Observations of CO emission from the literature show that the volume density of H(2) can vary to a large extent, a parameter that puts severe uncertainties on the derived abundances. Our analysis shows a wide range of abundances reflecting the degree to which shock chemistry affects the formation and destruction of water. We also compare our results with recent results from the SWAS team. Conclusions. Elevated abundances of ortho-water are found in several sources. The abundance reaches values as high as what would be expected from a theoretical C-type shock where all oxygen, not in the form of CO, is converted to water. However, the high abundances we derive could also be due to the low densities (derived from CO observations) that we assume. The water emission may in reality stem from high density regions much smaller than the Odin beam. We do not find any relationship between the abundance and the mass loss rate. On the other hand, there is a relation between the derived water abundance and the observed maximum outflow velocity.

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