Detection of a 2.85 micrometer Feature on 5 Spinel-rich Asteroids from JWST
Ground-based observations of `Barbarian' L-type asteroids at 1 to 2.5-\(\mu\)m indicate that their near-infrared spectra are dominated by the mineral spinel, which has been attributed to a high abundance of calcium-aluminum inclusions (CAIs) -- the first solids to condense out of the protoplane...
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Published in | arXiv.org |
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Main Authors | , , , , |
Format | Paper Journal Article |
Language | English |
Published |
Ithaca
Cornell University Library, arXiv.org
20.05.2024
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Subjects | |
Online Access | Get full text |
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Summary: | Ground-based observations of `Barbarian' L-type asteroids at 1 to 2.5-\(\mu\)m indicate that their near-infrared spectra are dominated by the mineral spinel, which has been attributed to a high abundance of calcium-aluminum inclusions (CAIs) -- the first solids to condense out of the protoplanetary disk during the formation of the Solar System. However, the spectral properties of these asteroids from 2.5 to 5-\(\mu\)m, a wavelength region that covers signatures of hydrated minerals, water, and organics, have not yet been explored. Here, we present 2 to 5-\(\mu\)m reflectance spectra of five spinel-rich asteroids obtained with the NIRSpec instrument on the James Webb Space Telescope. All five targets exhibit a \(\sim\) 2.85-\(\mu\)m absorption feature with a band depth of 3-6\(\%\) that appears correlated in strength with that of the 2-\(\mu\)m spinel absorption feature. The shape and position of the 2.85-\(\mu\)m feature are not a good match to the 2.7-\(\mu\)m feature commonly seen in carbonaceous CM meteorites or C-type asteroids. The closest spectral matches are to the Moon and Vesta, suggesting commonalities in aqueous alteration across silicate bodies, infall of hydrated material, and/or space weathering by solar wind H implantation. Lab spectra of CO/CV chondrites, CAIs, as well as the minerals cronstedtite and spinel, also show a similar feature, providing clues into the origin of the 2.85-\(\mu\)m feature. |
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ISSN: | 2331-8422 |
DOI: | 10.48550/arxiv.2405.12281 |