Linking interstellar and cometary O: a deep search for OO in the solar-type protostar IRAS 16293--2422
arXiv:1805.12492 · doi:10.1051/0004-6361/201833175
Abstract
Recent measurements carried out at comet 67P/C-G with the probe revealed that molecular oxygen, O, is the fourth most abundant molecule in comets. Models show that O is likely of primordial nature, coming from the interstellar cloud from which our Solar System was formed. However, gaseous O is an elusive molecule in the interstellar medium with only one detection towards quiescent molecular clouds, in the Oph A core. We perform a deep search for molecular oxygen, through the rotational transition at 234 GHz of its OO isotopologue, towards the warm compact gas surrounding the nearby Class 0 protostar IRAS 16293--2422 B with the ALMA interferometer. The targeted OO transition is surrounded by two brighter transitions at km s relative to the expected OO transition frequency. After subtraction of these two transitions, residual emission at a 3 level remains, but with a velocity offset of km s relative to the source velocity, rendering the detection "tentative". We derive the O column density for two excitation temperatures of 125 and 300 K, as indicated by other molecules, in order to compare the O abundance between IRAS16293 and comet 67P/C-G. Assuming that OO is not detected and using methanol CHOH as a reference species, we obtain a [O]/[CHOH] abundance ratio lower than , depending on the assumed , a three to four times lower abundance than the [O]/[CHOH] ratio of found in comet 67P/C-G. Such a low O abundance could be explained by the lower temperature of the dense cloud precursor of IRAS16293 with respect to the one at the origin of our Solar System that prevented an efficient formation of O in interstellar ices.
arXiv comment12 pages, 3 figures, accepted for publication in Astronomy & Astrophysics
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