MINDS: The very low-mass star and brown dwarf sample II. Probing disk settling, dust properties, and dust-gas interplay with JWST/MIRI
Hyerin Jang, Aditya M. Arabhavi, Till Kaeufer, Rens Waters, Inga Kamp, Thomas Henning, Alessio Caratti o Garatti, Ewine F. van Dishoeck, Giulia Perotti, Jayatee Kanwar, Manuel Güdel, Maria Morales-Calderón, Sierra L. Grant, Valentin Christiaens
TL;DR
This work analyzes JWST/MIRI observations of ten very low-mass star and brown dwarf disks to investigate dust settling, grain sizes, and crystallinity, and their connection to gas density in the inner disk. Using the DuCKLinG retrieval framework, the authors decompose mid-IR spectra into dust and gas components across a five-species dust suite and multiple grain sizes, revealing a progression from less-settled disks dominated by ~5 μm grains to more- and fully-settled disks with higher crystallinity and smaller-grain fractions, and weak silicate emission in the most evolved cases. They find an overall trend where gas column density, traced by hydrocarbon ratios such as $F_{^{13} m CCH_2}/F_{ m C_{2}H_{2}}$, increases as the dust opacity decreases, consistent with deeper optical-depth probing in settled disks, and they document a nuanced crystallinity pattern in which enstatite becomes prominent in inner regions while forsterite remains outer-disk dominated. The results point to evolutionary pathways involving dust settling, thermal processing, inner-disk clearing, or collisional cascades, and underscore the need for broader VLMS disk samples to link dust and gas appearance to planet-forming environments around VLMS and BD hosts.
Abstract
Disks around very low-mass stars (VLMS) provide environments for the formation of Earth-like planets. Mid-infrared observations have revealed that these disks exhibit weak silicate features and strong hydrocarbon emissions. This study characterizes the dust properties and geometrical structures of VLMS and brown dwarf (BD) disks, observed by the James Webb Space Telescope (JWST)/Mid-Infrared Instrument (MIRI), and connects these to gas column density and potential evolutionary stages. We analyze mid-infrared spectra of ten VLMS and BD disks as a part of the MIRI mid-Infrared Disk Survey (MINDS) program. Spectral slopes and silicate band strengths are compared with hydrocarbon emission line ratios, which probe the gas column density. Moreover, the Dust Continuum Kit with Line emission from Gas is used to quantify grain sizes, dust compositions, and crystallinity in the disk surface. The disks are classified into less, more, and fully settled geometries based on their mid-infrared spectral slopes and silicate band strengths. Less-settled disks show a relatively strong silicate band, high spectral slopes, and low crystallinity, and are dominated by 5 $μ$m-sized grains. More-settled disks have weaker silicate band, low spectral slope, enhanced crystallinity, and higher mass fractions of smaller grains. Fully-settled disks exhibit little or no silicate emission and negative spectral slopes. An overall trend of increasing gas column density with decreasing spectral slope suggests that more molecular gas is exposed when the dust opacity decreases due to dust settling. Our findings may reflect possible evolutionary pathways with dust settling and thermal processing or may point to inner-disk clearing or a collisional cascade. These results highlight the need for broader samples to understand the link between dust and gas appearance in regions where Earth-like planets form.
