Protoplanetary Disk Structure With Grain Evolution: the ANDES Model
V. Akimkin, S. Zhukovska, D. Wiebe, D. Semenov, Ya. Pavlyuchenkov, A., Vasyunin, T. Birnstiel, Th. Henning

TL;DR
This paper introduces ANDES, a comprehensive protoplanetary disk model that integrates dust grain evolution and molecular chemistry, revealing how dust processes influence disk temperature, chemistry, and molecular distributions.
Contribution
The novel aspect is the first-time inclusion of grain evolution and time-dependent chemistry in a self-consistent protoplanetary disk model.
Findings
Dust growth and sedimentation raise temperatures in the inner disk and lower them in the outer disk.
Dust evolution shifts the molecular layer closer to the midplane due to increased transparency.
Molecular abundances like CO2, H2O, and HCN are enhanced with dust evolution.
Abstract
We present a self-consistent model of a protoplanetary disk: 'ANDES' ('AccretioN disk with Dust Evolution and Sedimentation'). ANDES is based on a flexible and extendable modular structure that includes 1) a 1+1D frequency-dependent continuum radiative transfer module, 2) a module to calculate the chemical evolution using an extended gas-grain network with UV/X-ray-driven processes surface reactions, 3) a module to calculate the gas thermal energy balance, and 4) a 1+1D module that simulates dust grain evolution. For the first time, grain evolution and time-dependent molecular chemistry are included in a protoplanetary disk model. We find that grain growth and sedimentation of large grains to the disk midplane lead to a dust-depleted atmosphere. Consequently, dust and gas temperatures become higher in the inner disk (R < 50 AU) and lower in the outer disk (R > 50 AU), in comparison with…
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