MINDS: The very low-mass star and brown dwarf sample

Context . Disks around very low-mass stars (VLMSs) provide environments for the formation of Earth-like planets. Mid-infrared observations have revealed that these disks often exhibit weak silicate features and prominent hydrocarbon emissions. Aims . This study aims to characterize 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). We investigate how these properties relate to gas column density and potential evolutionary stages. Methods . We analyzed mid-infrared spectra of ten VLMSs and BD disks from the JWST/MIRI observations as part of the MIRI mid-Infrared Disk Survey (MINDS) program. Spectral slopes and silicate band strengths were measured and compared with hydrocarbon emission line ratios, which probe the gas column density. Moreover, the Dust Continuum Kit with Line emission from Gas (DuCKLinG) was used to quantify grain sizes, dust compositions, and crystallinity on the disk surface. Results . 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 µm-sized grains. More settled disks have weaker silicate bands, low spectral slopes, enhanced crystallinity, and higher mass fractions of smaller grains (<5 µm). 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 with increasing dust settling. Conclusions . Our findings indicate that our sample shows dust processing signatures of grain growth and crystallization. These characteristics may reflect possible evolutionary pathways with disk turbulence, dust settling, and thermal processing or may alternatively 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.

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Journal
Astronomy and Astrophysics
Published
2025-09-27
DOI
https://doi.org/10.1051/0004-6361/202556193
Primary Topic
Astronomy and Astrophysical Research
Type
article
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article

MINDS: The very low-mass star and brown dwarf sample

Hyerin Jang, M. Guêdel, J. S. Kanwar, A. Caratti o Garatti et al.
Astronomy and Astrophysics
Astronomy and Astrophysical Research
article

MINDS: The very low-mass star and brown dwarf sample

Hyerin Jang, M. Guêdel, J. S. Kanwar, A. Caratti o Garatti, Aditya M. Arabhavi, Rens Waters, E. F. van Dishoeck, Valentin Christiaens, M. Morales‐Calderón, I. Kamp, Sierra L. Grant, Giulia Perotti, Thomas Henning, Till Kaeufer
article en

Abstract

Context . Disks around very low-mass stars (VLMSs) provide environments for the formation of Earth-like planets. Mid-infrared observations have revealed that these disks often exhibit weak silicate features and prominent hydrocarbon emissions. Aims . This study aims to characterize 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). We investigate how these properties relate to gas column density and potential evolutionary stages. Methods . We analyzed mid-infrared spectra of ten VLMSs and BD disks from the JWST/MIRI observations as part of the MIRI mid-Infrared Disk Survey (MINDS) program. Spectral slopes and silicate band strengths were measured and compared with hydrocarbon emission line ratios, which probe the gas column density. Moreover, the Dust Continuum Kit with Line emission from Gas (DuCKLinG) was used to quantify grain sizes, dust compositions, and crystallinity on the disk surface. Results . 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 µm-sized grains. More settled disks have weaker silicate bands, low spectral slopes, enhanced crystallinity, and higher mass fractions of smaller grains (<5 µm). 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 with increasing dust settling. Conclusions . Our findings indicate that our sample shows dust processing signatures of grain growth and crystallization. These characteristics may reflect possible evolutionary pathways with disk turbulence, dust settling, and thermal processing or may alternatively 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.

Astronomy and AstrophysicsVol. 703
Leiden University (NL), University of Copenhagen (DK), University of Vienna (AT), Radboud University Nijmegen (NL), Max Planck Society (DE), University of Liège (BE), University of Groningen (NL), Carnegie Institution for Science (US), University of Exeter (GB), University of Michigan (US), Institute of Particle Physics (CA), Max Planck Institute for Astronomy (DE), Institute of Astronomy (RU), Centro de Astrobiología (ES), Astronomical Institute of the Slovak Academy of Sciences (SK), Space Research Organisation Netherlands (NL), National Institute for Astrophysics (IT), KU Leuven (BE)
Openalex Percentile: Top 71%
Astronomy and Astrophysical Research
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