2021A&A...649A.113B


Query : 2021A&A...649A.113B

2021A&A...649A.113B - Astronomy and Astrophysics, volume 649A113 (2021/5-1)

Fragmentation and kinematics in high-mass star formation. CORE-extension targeting two very young high-mass star-forming regions.

BEUTHER H., GIESER C., SURI S., LINZ H., KLAASSEN P., SEMENOV D., WINTERS J.M., HENNING T., SOLER J.D., URQUHART J.S., SYED J., FENG S., MOLLER T., BELTRAN M.T., SANCHEZ-MONGE A., LONGMORE S.N., PETERS T., BALLESTEROS-PAREDES J., SCHILKE P., MOSCADELLI L., PALAU A., CESARONI R., LUMSDEN S., PUDRITZ R., WYROWSKI F., KUIPER R. and AHMADI A.

Abstract (from CDS):


Context. The formation of high-mass star-forming regions from their parental gas cloud and the subsequent fragmentation processes lie at the heart of star formation research.
Aims. We aim to study the dynamical and fragmentation properties at very early evolutionary stages of high-mass star formation.
Methods. Employing the NOrthern Extended Millimeter Array and the IRAM 30 m telescope, we observed two young high-mass star-forming regions, ISOSS22478 and ISOSS23053, in the 1.3 mm continuum and spectral line emission at a high angular resolution (∼0.8").
Results. We resolved 29 cores that are mostly located along filament-like structures. Depending on the temperature assumption, these cores follow a mass-size relation of approximately M ∝ r2.0±0.3, corresponding to constant mean column densities. However, with different temperature assumptions, a steeper mass-size relation up to M ∝ r3.0±0.2, which would be more likely to correspond to constant mean volume densities, cannot be ruled out. The correlation of the core masses with their nearest neighbor separations is consistent with thermal Jeans fragmentation. We found hardly any core separations at the spatial resolution limit, indicating that the data resolve the large-scale fragmentation well. Although the kinematics of the two regions appear very different at first sight - multiple velocity components along filaments in ISOSS22478 versus a steep velocity gradient of more than 50km/s/pc in ISOSS23053 - the findings can all be explained within the framework of a dynamical cloud collapse scenario.
Conclusions. While our data are consistent with a dynamical cloud collapse scenario and subsequent thermal Jeans fragmentation, the importance of additional environmental properties, such as the magnetization of the gas or external shocks triggering converging gas flows, is nonetheless not as well constrained and would require future investigation.

Abstract Copyright: ©

Journal keyword(s): stars: formation - ISM: clouds - ISM: kinematics and dynamics - stars: massive - stars: protostars

VizieR on-line data: <Available at CDS (J/A+A/649/A113): list.dat fits/*>

Nomenclature: Fig. 3, Table 2: [BGS2021] ISOSSHHMMm NN N=15+14.

Simbad objects: 46

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Number of rows : 46
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 QSO B0016+73 Bla 00 19 45.78637230 +73 27 30.0176020     19.00 18.26   ~ 313 1
2 NGC 253 SyG 00 47 33.134 -25 17 19.68   8.03   6.94 8.1 ~ 3588 2
3 NAME f-Shaped Filament in Orion Cld 05 35.0 -05 30           ~ 133 0
4 NAME OMC-1 MoC 05 35 14 -05 22.4           ~ 1249 2
5 M 42 HII 05 35 16.8 -05 23 15           ~ 4411 0
6 EGO G011.92-0.61 of? 18 13 58.1 -18 54 17           ~ 54 0
7 NAME Serpens South Cluster Cl* 18 30 03.00 -02 01 58.2           ~ 148 0
8 NAME IRDC 18310-4 cor 18 33 39.42 -08 21 10.4           ~ 20 0
9 CORNISH G029.9559-00.0168 Y*O 18 46 04.18 -02 39 21.3           ~ 385 0
10 AGAL G030.818-00.056 cor 18 47 47.0 -01 54 28           ~ 186 0
11 MSXDC G035.39-00.33 MoC 18 57 09.0 +02 07 46           ~ 132 0
12 SNR G035.2-01.8 SNR 19 01.6 +01 14           ~ 158 0
13 EM* MWC 349 ** 20 32 45.499080 +40 39 36.74124   15.88 13.15 12.13   Bep 837 0
14 ICRF J222318.0+624933 Bz? 22 23 18.09663229 +62 49 33.8051074           ~ 25 1
15 [BGS2021] ISOSS22478 10 cor 22 47 45.65 +63 56 27.1           ~ 2 0
16 [BGS2021] ISOSS22478 4 cor 22 47 46.42 +63 56 49.8           ~ 2 0
17 [BGS2021] ISOSS22478 3 cor 22 47 46.56 +63 56 49.1           ~ 2 0
18 [BGS2021] ISOSS22478 5 cor 22 47 48.15 +63 56 44.3           ~ 2 0
19 [BGS2021] ISOSS22478 11 cor 22 47 49.40 +63 56 52.1           ~ 2 0
20 [BGS2021] ISOSS22478 15 cor 22 47 49.87 +63 56 45.8           ~ 2 0
21 [BGS2021] ISOSS22478 13 cor 22 47 50.02 +63 56 45.0           ~ 2 0
22 [BGS2021] ISOSS22478 6 cor 22 47 50.39 +63 56 57.1           ~ 2 0
23 [BGS2021] ISOSS22478 9 cor 22 47 50.43 +63 56 46.6           ~ 2 0
24 [BGS2021] ISOSS22478 7 cor 22 47 50.67 +63 57 00.6           ~ 2 0
25 [BGS2021] ISOSS22478 8 cor 22 47 50.88 +63 56 41.2           ~ 2 0
26 [BGS2021] ISOSS22478 1 cor 22 47 51.08 +63 56 43.7           ~ 2 0
27 [BGS2021] ISOSS22478 14 cor 22 47 51.19 +63 57 00.3           ~ 2 0
28 [BGS2021] ISOSS22478 12 cor 22 47 51.22 +63 56 38.4           ~ 2 0
29 [BGS2021] ISOSS22478 2 cor 22 47 52.68 +63 56 34.6           ~ 2 0
30 IRAS 22460+6341 IR 22 47 54.1 +63 57 11           ~ 9 0
31 3C 454.3 Bla 22 53 57.7480438728 +16 08 53.561508864   16.57 16.10 15.22   ~ 3004 2
32 [BGS2021] ISOSS23053 12 cor 23 05 19.82 +59 54 02.6           ~ 2 0
33 [BGS2021] ISOSS23053 4 cor 23 05 19.99 +59 53 55.2           ~ 2 0
34 [BGS2021] ISOSS23053 8 cor 23 05 20.34 +59 53 43.2           ~ 2 0
35 [BGS2021] ISOSS23053 10 cor 23 05 20.74 +59 53 52.1           ~ 2 0
36 [BGS2021] ISOSS23053 11 cor 23 05 21.38 +59 53 53.0           ~ 2 0
37 [BGS2021] ISOSS23053 1 cor 23 05 21.62 +59 53 43.2           ~ 2 0
38 [BGS2021] ISOSS23053 5 cor 23 05 21.84 +59 53 46.1           ~ 2 0
39 [BGS2021] ISOSS23053 9 cor 23 05 22.41 +59 53 46.2           ~ 2 0
40 IRAS 23032+5937 HII 23 05 23.1 +59 53 53           ~ 40 0
41 [BGS2021] ISOSS23053 3 cor 23 05 23.15 +59 53 54.9           ~ 2 0
42 [BGS2021] ISOSS23053 2 cor 23 05 23.54 +59 53 54.7           ~ 2 0
43 [BGS2021] ISOSS23053 13 cor 23 05 23.78 +59 53 51.7           ~ 2 0
44 [BGS2021] ISOSS23053 6 cor 23 05 23.79 +59 54 01.0           ~ 2 0
45 [BGS2021] ISOSS23053 14 cor 23 05 24.42 +59 54 01.7           ~ 2 0
46 [BGS2021] ISOSS23053 7 cor 23 05 24.57 +59 53 59.4           ~ 2 0

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