We analyze the 12CO J = 3-2 data cubes of the disks in the exoALMA program. 13/15 disks reveal a variety of kinematic substructures in individual channels: large-scale arcs or spiral arms, localized velocity kinks, and/or multiple faints arcs that appear like filamentary structures on the disk surface. We find kinematic signatures that are consistent with planet wakes in six disks: AA Tau, SY Cha, J1842, J1615, LkCa 15, and HD 143006. Comparison with hydrodynamical and radiative transfer simulations suggests planets with orbital radii between 80 and 310 au and masses between 1 and 5 MJup. Additional kinematic substructures limit our ability to place tight constraints on the planet masses. When the inclination is favorable to separate the upper and lower surfaces (near 45°, i.e., in 7/15 disks), we always detect the vertical CO snowline and find that the 12CO freeze-out is partial in the disk midplane, with a depletion factor of ≈10−3 -10−2 compared to the warm molecular layer. In these same seven disks, we also systematically detect evidence of CO desorption in the outer regions.

exoALMA. X. Channel Maps Reveal Complex 12CO Abundance Distributions and a Variety of Kinematic Structures with Evidence for Embedded Planets / C. Pinte, J.D. Ilee, J. Huang, M. Benisty, S. Facchini, M. Fukagawa, R. Teague, J. Bae, M. Barraza-Alfaro, G. Cataldi, N. Cuello, P. Curone, I. Czekala, D. Fasano, M. Flock, M. Galloway-Sprietsma, H. Garg, C. Hall, I. Hammond, C. Hardiman, T. Hilder, A.F. Izquierdo, K. Kanagawa, G. Lesur, G. Lodato, C. Longarini, R.A. Loomis, F. Masset, F. Menard, R. Orihara, D.J. Price, G. Rosotti, J. Stadler, H.-. Yen, G. Wafflard-Fernandez, D.J. Wilner, A.J. Winter, L. Wolfer, T.C. Yoshida, B. Zawadzki. - In: THE ASTROPHYSICAL JOURNAL LETTERS. - ISSN 2041-8205. - 984:1(2025 May 01), pp. L15.1-L15.13. [10.3847/2041-8213/adc433]

exoALMA. X. Channel Maps Reveal Complex 12CO Abundance Distributions and a Variety of Kinematic Structures with Evidence for Embedded Planets

S. Facchini;P. Curone;G. Lodato;C. Longarini;G. Rosotti;
2025

Abstract

We analyze the 12CO J = 3-2 data cubes of the disks in the exoALMA program. 13/15 disks reveal a variety of kinematic substructures in individual channels: large-scale arcs or spiral arms, localized velocity kinks, and/or multiple faints arcs that appear like filamentary structures on the disk surface. We find kinematic signatures that are consistent with planet wakes in six disks: AA Tau, SY Cha, J1842, J1615, LkCa 15, and HD 143006. Comparison with hydrodynamical and radiative transfer simulations suggests planets with orbital radii between 80 and 310 au and masses between 1 and 5 MJup. Additional kinematic substructures limit our ability to place tight constraints on the planet masses. When the inclination is favorable to separate the upper and lower surfaces (near 45°, i.e., in 7/15 disks), we always detect the vertical CO snowline and find that the 12CO freeze-out is partial in the disk midplane, with a depletion factor of ≈10−3 -10−2 compared to the warm molecular layer. In these same seven disks, we also systematically detect evidence of CO desorption in the outer regions.
Settore PHYS-05/A - Astrofisica, cosmologia e scienza dello spazio
   Unveiling the infancy of planetary systems (UNVEIL)
   UNVEIL
   EUROPEAN COMMISSION
   101076613

   Probing the Origin of Planetary Systems (POPS)
   POPS
   MINISTERO DELL'UNIVERSITA' E DELLA RICERCA
   2022YP5ACE_001

   Rebuilding the foundations of planet formation: proto-planetary disc evolution (DiscEvol)
   DiscEvol
   EUROPEAN COMMISSION
   101039651

   From non-ideal magnetohydrodynamics to the structure and evolution of protoplanetary discs
   MHDiscs
   European Commission
   Horizon 2020 Framework Programme
   815559

   Establishing a global observational view of the early stages of planet formation and evolution
   PROTOPLANETS
   European Commission
   Horizon 2020 Framework Programme
   101002188

   A new window into planet formation: disc kinematics
   FONDAZIONE CARIPLO
   ID Progetto 2022-1217
1-mag-2025
28-apr-2025
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/1163738
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