Characterising the molecular line emission in the asymmetric Oph-IRS 48 dust trap: Temperatures, timescales, and sub-thermal excitation

Milou Temmink; Alice S. Booth; Margot Leemker; Nienke van der Marel; Ewine F. van Dishoeck; Lucy Evans; Luke Keyte; Charles J. Law; Shota Notsu; Karin Öberg; Catherine Walsh

paper

Characterising the molecular line emission in the asymmetric Oph-IRS 48 dust trap: Temperatures, timescales, and sub-thermal excitation

arXiv:2411.12418

Abstract

The ongoing physical and chemical processes in planet-forming disks set the stage for planet formation. The asymmetric disk around the young star Oph-IRS 48 has one of the most well-characterised chemical inventories, showing molecular emission from a wide variety of species at the dust trap. One of the explanations for the asymmetric structure is dust trapping by a perturbation-induced vortex. We aim to constrain the excitation properties of the molecular species SO $_{2}$ , CH $_{3}$ OH, and H $_{2}$ CO. We further characterise the extent of the molecular emission, through the determination of important physical and chemical timescales at the location of the dust trap. We also investigate whether the potential vortex can influence the observable temperature structure of the gas. Through a pixel-by-pixel rotational diagram analysis, we create rotational temperature and column density maps for SO $_{2}$ and CH $_{3}$ OH, while temperature maps for H $_{2}$ CO are created using line ratios. We find temperatures of $T \sim$ 55 K and $T \sim$ 125 K for SO $_{2}$ and CH $_{3}$ OH, respectively, while the line ratios point towards temperatures of T $\sim$ 150-300 K for H $_{2}$ CO. The rotational diagram of CH $_{3}$ OH is dominated by scatter and subsequent non-LTE RADEX calculations suggest that both CH $_{3}$ OH and H $_{2}$ CO must be sub-thermally excited. The temperatures suggest that SO $_{2}$ comes from a layer deep in the disk, while CH $_{3}$ OH and H $_{2}$ CO originate from a higher layer. While a potential radial gradient is seen in the temperature map of SO $_{2}$ , we do not find any hints of a vortex influencing the temperature structure. The determined turbulent mixing timescale is not able to explain the emitting heights of the molecules, but the photodissociation timescales are able to explain the wider azimuthal extents of SO $_{2}$ and H $_{2}$ CO compared to CH $_{3}$ OH, where a secondary, gas-phase formation reservoir is required for H $_{2}$ CO.

Accepted for publication in Astronomy and Astrophysics