Exploring DCO as a tracer of thermal inversion in the disk around the Herbig Ae star HD163296
arXiv:1806.02950 · doi:10.1051/0004-6361/201731745
Abstract
We aim to reproduce the DCO emission in the disk around HD163296 using a simple 2D chemical model for the formation of DCO through the cold deuteration channel and a parametric treatment of the warm deuteration channel. We use data from ALMA in band 6 to obtain a resolved spectral imaging data cube of the DCO =3--2 line in HD163296 with a synthesized beam of 0."53 0."42. We adopt a physical structure of the disk from the literature that reproduces the spectral energy distribution. We then apply a simplified chemical network for the formation of DCO that uses the physical structure of the disk as parameters along with a CO abundance profile, a constant HD abundance and a constant ionization rate. Finally, from the resulting DCO abundances, we calculate the non-LTE emission using the 3D radiative transfer code LIME. The observed DCO emission is reproduced by a model with cold deuteration producing abundances up to . Warm deuteration, at a constant abundance of , becomes fully effective below 32 K and tapers off at higher temperatures, reproducing the lack of DCO inside 90 AU. Throughout the DCO emitting zone a CO abundance of is found, with 99\% of it frozen out below 19 K. At radii where both cold and warm deuteration are active, warm deuteration contributes up to 20\% of DCO, consistent with detailed chemical models. The decrease of DCO at large radii is attributed to a temperature inversion at 250 AU, which raises temperatures above values where cold deuteration operates. Increased photodesorption may also limit the radial extent of DCO. The corresponding return of the DCO layer to the midplane, together with a radially increasing ionization fraction, reproduces the local DCO emission maximum at 260 AU.
arXiv comment9 pages, 5 figures, accepted 7th July 2018
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