2019A&A...631A..25J


Query : 2019A&A...631A..25J

2019A&A...631A..25J - Astronomy and Astrophysics, volume 631A25-25 (2019/11-1)

ALMA observations of water deuteration: a physical diagnostic of the formation of protostars.

JENSEN S.S., JORGENSEN J.K., KRISTENSEN L.E., FURUYA K., COUTENS A., VAN DISHOECK E.F., HARSONO D. and PERSSON M.V.

Abstract (from CDS):


Context. How water is delivered to planetary systems is a central question in astrochemistry. The deuterium fractionation of water can serve as a tracer for the chemical and physical evolution of water during star formation and can constrain the origin of water in Solar System bodies.
Aims. The aim is to determine the HDO/H2O ratio in the inner warm gas toward three low-mass Class 0 protostars selected to be in isolated cores, i.e., not associated with any cloud complexes. Previous sources for which the HDO/H2O ratio have been established were all part of larger star-forming complexes. Determining the HDO/H2O ratio toward three isolated protostars allows comparison of the water chemistry in isolated and clustered regions to determine the influence of local cloud environment.
Methods. We present ALMA Band 6 observations of the HDO 31,2-22,1 and 21,1-21,2 transitions at 225.897 GHz and 241.562 GHz along with the first ALMA Band 5 observations of the H218_2^{18}218O 31,3-22,0 transition at 203.407 GHz. The high angular resolution observations (0.3"-1.3") allow the study of the inner warm envelope gas. Model-independent estimates for the HDO/H2O ratios are obtained and compared with previous determinations of the HDO/H2O ratio in the warm gas toward low-mass protostars.
Results. We successfully detect the targeted water transitions toward the three sources with signal-to-noise ratio (S/N)>5. We determine the HDO/H2O ratio toward L483, B335 and BHR71-IRS1 to be (2.2±0.4)x10–3, (1.7±0.3)x10–3, and (1.8±0.4)x10–3, respectively, assuming Tex=124K. The degree of water deuteration of these isolated protostars are a factor of 2-4 higher relative to Class 0 protostars that are members of known nearby clustered star-forming regions.
Conclusions. The results indicate that the water deuterium fractionation is influenced by the local cloud environment. This effect can be explained by variations in either collapse timescales or temperatures, which depends on local cloud dynamics and could provide a new method to decipher the history of young stars.

Abstract Copyright: © ESO 2019

Journal keyword(s): astrochemistry - stars: formation - ISM: abundances - ISM: individual objects: L483 - ISM: individual objects: B335 - ISM: individual objects: BHR71-IRS1

Simbad objects: 23

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Number of rows : 23
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 [JCC87] IRAS 2A Y*O 03 28 55.55 +31 14 36.7           ~ 513 3
2 NGC 1333 OpC 03 29 09.2 +31 20 59           ~ 1575 1
3 [JCC87] IRAS 4A Y*O 03 29 10.49 +31 13 30.8           ~ 770 1
4 [JCC87] IRAS 4B Y*O 03 29 12.058 +31 13 02.05           ~ 625 0
5 QSO B0903-573 BLL 09 04 53.1791655231 -57 35 05.782508724           ~ 131 1
6 QSO B1104-445 Bla 11 07 08.69412105 -44 49 07.6183013   17.84 18.2 17.37   ~ 260 1
7 QSO B1145-676 Bla 11 47 33.39959532 -67 53 41.7696668   19.66   16.6   ~ 61 1
8 [B2001b] IRS 1 Y*O 12 01 36.53040 -65 08 51.9180           ~ 167 0
9 BHR 71 MoC 12 01 37 -65 08.8           ~ 163 0
10 NAME Coalsack Nebula DNe 12 31 19 -63 44.6           ~ 275 0
11 NAME Ophiuchus Molecular Cloud SFR 16 28 06 -24 32.5           ~ 3969 1
12 IRAS 16293-2422 cor 16 32 22.56 -24 28 31.8           ~ 1357 1
13 QSO B1741-038 Bla 17 43 58.85613537 -03 50 04.6167326     20.40 17.98   ~ 583 1
14 4C 09.57 BLL 17 51 32.81857326 +09 39 00.7284066   17.46 16.78 15.57   ~ 1007 1
15 IRAS 18148-0440 Y*O 18 17 29.94 -04 39 39.3           ~ 97 0
16 LDN 483 DNe 18 17 35 -04 39.8           ~ 359 0
17 NAME Aql Rift DNe 18 32 -01.0           ~ 355 1
18 LDN 663 DNe 19 36 55 +07 34.4           ~ 698 0
19 IRAS 19345+0727 cor 19 37 00.7 +07 34 08           ~ 96 0
20 PMN J1938+0448 Rad 19 38 30.66954887 +04 48 11.6142608           ~ 32 1
21 ICRF J195511.5+135816 Bla 19 55 11.57141632 +13 58 16.2406814       18.6   ~ 66 1
22 QSO B1958-179 Bla 20 00 57.09043927 -17 48 57.6726139   18.02 18.60 15.33   ~ 288 1
23 QSO B2023+336 BLL 20 25 10.84210426 +33 43 00.2143556           ~ 188 1

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