Chemical evolution of protoplanetary disks - the effects of viscous accretion, turbulent mixing and disk winds
Dominikus Heinzeller (1, 3), Hideko Nomura (1), Catherine Walsh (2), and Tom J. Millar (2) ((1) Department of Astronomy, Graduate School of, Science, Kyoto University, Japan (2) Astrophysics Research Centre, School of, Mathematics, Physics, Queen's University Belfast

TL;DR
This study models the chemical evolution of protoplanetary disks considering viscous accretion, turbulent mixing, and disk winds, revealing their significant impact on molecular abundances and emission spectra, and comparing results with observations.
Contribution
It introduces a comprehensive chemical model incorporating viscous accretion, turbulent mixing, and disk winds, and analyzes their effects on disk chemistry and observable spectra.
Findings
H2 formation on warm grains increases H2O and OH in disk surface.
Radial accretion strongly influences midplane molecular abundances.
Turbulent mixing enhances certain molecules and improves spectral agreement.
Abstract
We calculate the chemical evolution of protoplanetary disks considering radial viscous accretion, vertical turbulent mixing and vertical disk winds. We study the effects on the disk chemical structure when different models for the formation of molecular hydrogen on dust grains are adopted. Our gas-phase chemistry is extracted from the UMIST Database for Astrochemistry (Rate06) to which we have added detailed gas-grain interactions. We use our chemical model results to generate synthetic near- and mid-infrared LTE line emission spectra and compare these with recent Spitzer observations. Our results show that if H2 formation on warm grains is taken into consideration, the H2O and OH abundances in the disk surface increase significantly. We find the radial accretion flow strongly influences the molecular abundances, with those in the cold midplane layers particularly affected. On the other…
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