Abstract
We report the detection of more than 48 velocity-resolved ground
rotational state transitions of H_216O, H_218O,
and H_217O - 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 H_218O
line fluxes, which are less affected by line opacity than their H_2
16O counterparts, and an escape probability method, the column
densities of H_218O associated with each emission component
are derived. We infer total water abundances of 7.4 ×
10-5, 1.0 × 10-5, and 1.6 ×
10-5 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.
Herschel is an ESA space observatory with science instruments provided
by European-led Principal Investigator consortia and with important
participation from NASA.Table 3 (page 5) is only available in electronic
form at http://www.aanda.org
| Original language | English |
|---|---|
| Article number | L27 |
| Number of pages | 5 |
| Journal | Astronomy & Astrophysics |
| Volume | 521 |
| DOIs | |
| Publication status | Published - Oct-2010 |
Keywords
- ISM: abundances
- ISM: molecules