2025A&A...703A.244T


Query : 2025A&A...703A.244T

2025A&A...703A.244T - Astronomy and Astrophysics, volume 703A244 (2025/11-1)

Anatomy of the Class I protostar L1489 IRS with NOEMA II. A disk replenished by a massive streamer.

TANIOUS M., LE GAL R., FAURE A., MARET S., LOPEZ-SEPULCRE A. and HILY-BLANT P.

Abstract (from CDS):

Context. Streamers are newly identified channels that transport mass from large, molecular-cloud scales down to small, protoplanetary-disk scales. To better understand their impact on planet formation, it is essential to study their physical and chemical properties.
Aims. In this framework, we aim to characterize the longest streamer identified in carbon chain emission within the Class I system L1489 IRS, connecting the nearby prestellar core L1489 to the young stellar object (YSO).
Methods. We observed multiple transitions of C2H, ortho-c-C3H2 and HC3N in L1489 IRS with NOEMA and IRAM-30m at 3 and 2 mm. Using a variety of radiative transfer methods, including a hyperfine structure (HFS) fitting, rotational diagrams, and proposing a new self-consistent Markov chain Monte Carlo approach combined with the non-LTE RADEX code, we derived the column densities and abundances of those molecules, as well as the H2 number density along the streamer. This enabled us to estimate its mass, infall rate, and its impact on the * system's mass.
Results. We found lower limits on the streamer mass of ≥(4.67-18.3) × 10–3M⊙ (i.e., ≥0.65-2.57 times the current disk mass) and an infallrate of ≥(1.94-7.57) × 10–7M⊙ yr–1, where the ranges correspond to the different molecular tracers. These values are consistent with those derived in similar Class I objects. This suggests that the disk could be fully replenished by streamer material. Given its mass, the streamer is likely at the origin of the external warped disk seen in this system, as predicted by numerical simulations. Moreover, the first investigations based on the C2H/c-C3H2 and HC3N/c-C3H2 abundance ratios suggest that the streamer chemistry may be inherited from the core. These results suggest, for the first time, that the chemical composition of a Class I object is affected by a streamer connecting a Class I YSO to its natal environment.
Conclusions. We demonstrate that the streamer in L1489 IRS has a significant impact on its disk. To better constrain how the streamer influences the disk's chemistry and determine whether its composition is inherited from the nearby core, further molecular surveys will be necessary toward the prestellar core, the streamer, and the YSO. Our findings reinforce the importance of characterizing the natal environment of protoplanetary disks both physically (e.g., structure formation) and chemically (e.g., material enrichment) to fully understand their evolution.

Abstract Copyright: © The Authors 2025

Journal keyword(s): astrochemistry - radiative transfer - protoplanetary disks - stars: low-mass - ISM: abundances - ISM: lines and bands

VizieR on-line data: <Available at CDS (J/A+A/703/A244): list.dat fits/*>

Simbad objects: 15

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Number of rows : 15
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 NGC 1275 Bla 03 19 48.1599902040 +41 30 42.108850836   13.10 12.48 11.09   ~ 4243 3
2 NAME Perseus Cloud SFR 03 35.0 +31 13           ~ 1553 0
3 6C 033321+320838 Bla 03 36 30.10760267 +32 18 29.3422162     17.50 16.6   ~ 688 1
4 QSO B0400+258 Bla 04 03 05.58608082 +26 00 01.5027775     18 19.00   ~ 220 1
5 Barnard 207 DNe 04 04.6 +26 20           ~ 9 0
6 IRAS 04016+2610 Y*O 04 04 43.07064 +26 18 56.3904           ~ 284 0
7 LDN 1489 DNe 04 04 47.5 +26 19 42           ~ 238 0
8 IRAS 04181+2655 mul 04 21 10.9 +27 02 06           ~ 55 0
9 EM* LkHA 101 Em* 04 30 14.4355820328 +35 16 23.983198932   17.91 15.71 13.33   F 376 1
10 LDN 1527 DNe 04 39 53 +25 45.0           ~ 689 0
11 NAME Taurus Complex SFR 04 41.0 +25 52           ~ 4971 0
12 V* SU Aur Or* 04 55 59.3866872552 +30 34 01.499608092   10.33 9.30 9.17   G2IIIne 628 0
13 NAME Orion Bright Bar reg 05 35 22.30 -05 24 33.0           ~ 1004 0
14 IRAS 16285-2355 Y*O 16 31 35.65752 -24 01 29.4708           ~ 178 0
15 IRAS 16544-1604 Y*O 16 57 19.626 -16 09 23.30           ~ 53 1

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