We present spatially resolved Atacama Large Millimeter/submillimeter Array (ALMA) observations of the water line at 183 GHz in the disk around the Herbig star HD 100546. The water vapor emission peaks at the inner edge of the warm dust cavity, located ∼15 au from the central star. We attribute this to thermal desorption at the water snow line, shifted outward at the dust cavity wall directly heated by the intense radiation. This represents the first spatially resolved image of the water snow line using ALMA observations of the main water isotopologue in a protoplanetary disk. The water emission morphology peaking inside the first dust ring is consistent with previous ALMA detections of oxygen-bearing complex organic molecules in the disk, including thermally desorbed methanol. These findings signal that warm cavities of transition disks provide ideal targets to directly reconstruct the spatial distribution of water vapor and the snow line location with ALMA and directly connect water vapor emission to ice desorption of complex organic species.

Water Vapor Emission at the Warm Cavity Wall of the HD 100546 Disk as Revealed by ALMA / L. Rampinelli, S. Facchini, M. Leemker, A. Isella, P. Curone, M. Benisty, E. Humphreys, L. Testi. - In: THE ASTROPHYSICAL JOURNAL LETTERS. - ISSN 2041-8205. - 996:1(2026 Jan), pp. L17.1-L17.10. [10.3847/2041-8213/ae2868]

Water Vapor Emission at the Warm Cavity Wall of the HD 100546 Disk as Revealed by ALMA

L. Rampinelli
Primo
;
S. Facchini
Secondo
;
M. Leemker;A. Isella;P. Curone;
2026

Abstract

We present spatially resolved Atacama Large Millimeter/submillimeter Array (ALMA) observations of the water line at 183 GHz in the disk around the Herbig star HD 100546. The water vapor emission peaks at the inner edge of the warm dust cavity, located ∼15 au from the central star. We attribute this to thermal desorption at the water snow line, shifted outward at the dust cavity wall directly heated by the intense radiation. This represents the first spatially resolved image of the water snow line using ALMA observations of the main water isotopologue in a protoplanetary disk. The water emission morphology peaking inside the first dust ring is consistent with previous ALMA detections of oxygen-bearing complex organic molecules in the disk, including thermally desorbed methanol. These findings signal that warm cavities of transition disks provide ideal targets to directly reconstruct the spatial distribution of water vapor and the snow line location with ALMA and directly connect water vapor emission to ice desorption of complex organic species.
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
gen-2026
30-dic-2025
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/1208338
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