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

Christophe Pinte, John D. Ilee, Jane Huang, Myriam Benisty, Stefano Facchini, Misato Fukagawa, Richard Teague, Jaehan Bae, Marcelo Barraza-Alfaro, Gianni Cataldi, Nicolás Cuello, Pietro Curone, Ian Czekala, Daniele Fasano, Mario Flock, Maria Galloway-Sprietsma, Himanshi Garg, Cassandra Hall, Iain Hammond, Caitlyn Hardiman, Thomas Hilder, Andrés F. Izquierdo, Kazuhiro Kanagawa, Geoffroy Lesur, Giuseppe Lodato, Cristiano Longarini, Ryan A. Loomis, Frédéric Masset, Francois Menard, Ryuta Orihara, Daniel J. Price, Giovanni Rosotti, Jochen Stadler, Hsi-Wei Yen, Gaylor Wafflard-Fernandez, David J. Wilner, Andrew J. Winter, Lisa Wölfer, Tomohiro C. Yoshida and Brianna Zawadzki
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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.
exoALMA。通道图揭示了复杂的12CO丰度分布和各种运动结构,并提供了嵌入式行星的证据
我们分析了exoALMA程序中磁盘的12CO J = 3-2数据立方体。13/15圆盘在单个通道中显示出各种各样的运动子结构:大规模的弧线或螺旋臂,局部速度扭结,和/或多个暗淡的弧线,在圆盘表面上看起来像丝状结构。我们在六个圆盘上发现了与行星尾迹一致的运动特征:AA Tau, SY Cha, J1842, J1615, LkCa 15和HD 143006。与流体动力学和辐射传输模拟的比较表明,行星的轨道半径在80到310 au之间,质量在1到5 MJup之间。额外的运动学子结构限制了我们对行星质量的严格限制。当倾角有利于分离上下表面时(接近45°,即在7/15个圆盘中),我们总是检测到垂直CO雪线,并发现12CO冻结在圆盘中层是部分的,与温暖分子层相比,损耗因子为≈10−3 -10−2。在这七个圆盘中,我们也系统地检测到CO在外部区域解吸的证据。
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