%AChoban, Caleb%AKereš, Dušan%AHopkins, Philip%ASandstrom, Karin%AHayward, Christopher%AFaucher-Giguère, Claude-André%BJournal Name: Monthly Notices of the Royal Astronomical Society; Journal Volume: 514; Journal Issue: 3; Related Information: CHORUS Timestamp: 2023-06-09 10:11:21 %D2022%IOxford University Press %JJournal Name: Monthly Notices of the Royal Astronomical Society; Journal Volume: 514; Journal Issue: 3; Related Information: CHORUS Timestamp: 2023-06-09 10:11:21 %K %MOSTI ID: 10368501 %PMedium: X %TThe galactic dust-up: modelling dust evolution in FIRE %XABSTRACT

Recent strides have been made developing dust evolution models for galaxy formation simulations but these approaches vary in their assumptions and degree of complexity. Here, we introduce and compare two separate dust evolution models (labelled ‘Elemental’ and ‘Species’), based on recent approaches, incorporated into the gizmo code and coupled with fire-2 stellar feedback and interstellar medium physics. Both models account for turbulent dust diffusion, stellar production of dust, dust growth via gas-dust accretion, and dust destruction from time-resolved supernovae, thermal sputtering in hot gas, and astration. The ‘Elemental’ model tracks the evolution of generalized dust species and utilizes a simple, ‘tunable’ dust growth routine, while the ‘Species’ model tracks the evolution of specific dust species with set chemical compositions and incorporates a physically motivated, two-phase dust growth routine. We test and compare these models in an idealized Milky Way-mass galaxy and find that while both produce reasonable galaxy-integrated dust-to-metals (D/Z) ratios and predict gas-dust accretion as the main dust growth mechanism, a chemically motivated model is needed to reproduce the observed scaling relation between individual element depletions and D/Z with column density and local gas density. We also find the inclusion of theoretical metallic iron and O-bearing dust species are needed in the case of specific dust species in order to match observations of O and Fe depletions, and the integration of a sub-resolution dense molecular gas/CO scheme is needed to both match observed C depletions and ensure carbonaceous dust is not overproduced in dense environments.

%0Journal Article