Resolved gas temperatures and <sup>12</sup>C/<sup>13</sup>C ratios in SVS13A from ALMA Observations of CH<sub>3</sub>CN and CH<sub>3</sub><sup>13</sup>CN
Context. Multiple systems are common in field stars and the frequency is found to be higher in early evolutionary stages. Thus, the study of young multiple systems during the embedded stages is key to a comprehensive understanding of star formation. In particular, the way material accretes from the large-scale envelope into the inner region and how this flow interacts with the system physically and chemically has not been well characterized observationally to date. Aims. We aim to provide a snapshot of the forming protobinary system SVS13A, consisting of VLA4A and VLA4B. This includes a clear picture of its kinematic structures, physical conditions, and chemical properties. Methods. We conducted ALMA observations toward SVS13A targeting CH 3 CN and CH 3 13 CN J=12-11 K-ladder line emission with a high spatial resolution of ∼30 astronomical units (au) at a spectral resolution of ∼0.08 km s −1 . Results. We used local thermal equilibrium (LTE) radiative transfer models to fit the spectral features of the line emission. We found the two-layer LTE radiative model that includes dust absorption is essential to interpreting the CH 3 CN and CH 3 13 CN line emission. We identified two major and four small kinematic components and derived their physical and chemical properties. Conclusions. We identified a possible infalling signature toward the bursting secondary source VLA4A, which may be fed by an infalling streamer from the large-scale envelope. The mechanical heating in the binary system, as well as the infalling shocked gas, are likely to play a role in the thermal structure of the protobinary system. By accumulating mass from the streamer, it is plausible that the system experienced a gravitationally unstable phase before the accretion outburst. Finally, the derived CH 3 CN/CH 3 13 CN ratio is lower than the canonical ratio in the ISM and varies between VLA4A and VLA4B.
Authors
- Dominique Segura-Cox (ORCID: https://orcid.org/0000-0003-3172-6763)
- M. T. Valdivia-Mena (ORCID: https://orcid.org/0000-0002-0347-3837)
- J. E. Pineda (ORCID: https://orcid.org/0000-0002-3972-1978)
- C. Gieser (ORCID: https://orcid.org/0000-0002-8120-1765)
- Valerio Lattanzi (ORCID: https://orcid.org/0000-0001-9819-1658)
- A. Lopez-Sepulcre
- R. Neri (ORCID: https://orcid.org/0000-0002-7176-4046)
- A. Laura Busch
- Timothy H. Hsieh (ORCID: https://orcid.org/0000-0002-5507-5697)
- María José Maureira (ORCID: https://orcid.org/0000-0002-7026-8163)
- S. Spezzano
- Yuxin Lin (ORCID: https://orcid.org/0000-0001-9299-5479)
- P. Caselli (ORCID: https://orcid.org/0000-0003-1481-7911)
- Y.-R. Chou
Institutions
- Centre National de la Recherche Scientifique (FR)
- Institute of Astronomy and Astrophysics, Academia Sinica (TW)
- European Southern Observatory (DE)
- Taiwan Comprehensive University System (TW)
- Max Planck Institute for Extraterrestrial Physics (DE)
- Institut de Radioastronomie Millimétrique (FR)
- University of Rochester (US)
- Université Grenoble Alpes (FR)
Publication Details
- Journal
- Astronomy and Astrophysics
- Published
- 2025-03-07
- DOI
- https://doi.org/10.1051/0004-6361/202453273
- Citations
- 6
- Primary Topic
- Atmospheric Ozone and Climate
- Type
- article
- Field-Weighted Citation Impact
- 7.80
Funders
- National Science Foundation
- National Radio Astronomy Observatory
- Korea Astronomy and Space Science Institute
- Max-Planck-Gesellschaft
- National Astronomical Observatory of Japan
- National Science and Technology Council
- National Institutes of Natural Sciences