2013
DOI: 10.1051/0004-6361/201322400
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Deuterated water in the solar-type protostars NGC 1333 IRAS 4A and IRAS 4B

Abstract: Context. The measure of the water deuterium fractionation is a relevant tool for understanding mechanisms of water formation and evolution from the prestellar phase to the formation of planets and comets. Aims. The aim of this paper is to study deuterated water in the solar-type protostars NGC 1333 IRAS 4A and IRAS 4B, to compare their HDO abundance distributions with other star-forming regions, and to constrain their HDO/H 2 O abundance ratios. Methods. Using the Herschel/HIFI instrument as well as ground-bas… Show more

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Cited by 43 publications
(38 citation statements)
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“…The transitions could originate in slightly different regions depending on the source structure. Coutens et al (2013) used Herschel and several groundbased single dish telescopes to observe lines of HDO toward IRAS 4A and IRAS 4B. From 1D radiative transfer models and using the H 18 2 O column density by Persson et al (2012), they estimated HDO/H 2 O ratios in the inner warm regions of IRAS 4A (4.0−30.0 × 10 −4 ) and IRAS 4B (1.0−37.0 ± 10 −4 ).…”
Section: Resultsmentioning
confidence: 99%
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“…The transitions could originate in slightly different regions depending on the source structure. Coutens et al (2013) used Herschel and several groundbased single dish telescopes to observe lines of HDO toward IRAS 4A and IRAS 4B. From 1D radiative transfer models and using the H 18 2 O column density by Persson et al (2012), they estimated HDO/H 2 O ratios in the inner warm regions of IRAS 4A (4.0−30.0 × 10 −4 ) and IRAS 4B (1.0−37.0 ± 10 −4 ).…”
Section: Resultsmentioning
confidence: 99%
“…Using SMA data of the HDO 3 1,2 −2 2,1 transition at 225 GHz, the above mentioned HDO/H 2 O limit of <6.4 × 10 −4 was found toward NGC 1333-IRAS 4B (Jørgensen & van Dishoeck 2010b). Coutens et al (2013) obtained values of 4−30 × 10 −4 for IRAS 4A and 1−37 × 10 −4 for IRAS 4B using new Herschel data combined with the H 18 2 O column densities found by Persson et al (2012) based on interferometric data. Taquet et al (2013) derived the warm HDO/H 2 O ratios for IRAS 2A and IRAS 4A using the determinations of the H 18 2 O column density from Persson et al (2012) and lower spatial-and spectral-resolution interferometric observations targeting the HDO 4 2,2 −4 2,3 transition (143.7 GHz, E u = 316.2 K) together with single dish (Liu et al 2011) observations of HDO.…”
Section: Introductionmentioning
confidence: 85%
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“…After the formation of water and deuterated water in the ice mantles in the star formation scenario, the environment undergoes gravitational collapse and the local density increases, leading to the formation of a protostar. The surrounding medium then heats up and releases the icy mantles into the gas phase, leading to a significant HDO abundance in the gas phase (Coutens et al 2012(Coutens et al , 2013b. Based on the non-LTE modeling of the five observed NH 3 transitions, we characterize the region of the filament that gives rise to the 70 km s −1 feature as having T kin = 30 K and n(H 2 ) = 5 × 10 5 cm −3 .…”
Section: Discussionmentioning
confidence: 99%
“…Previous studies used step-or drop-abundance profiles for water vapour (Herpin et al 2012;Coutens et al 2012Coutens et al , 2013. These profiles are characterised by distinct regions of constant abundance.…”
Section: Simplified Water Network (Swan)mentioning
confidence: 99%