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Dryad

Carbon dioxide and amorphous water ices in the debris disk around β Pictoris

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Abstract

The star β Pictoris is orbited by a dusty debris disk, within which planet formation is occurring. The disk extends far from the star such that molecules in the outer disk should freeze. We observed the β Pictoris disk in the near-infrared using the James Webb Space Telescope. The spectrum shows features due to amorphous water ice (<7% crystallinity), and carbon dioxide ice in both the 12CO2 and 13CO2 isotopologues. We infer that the CO2 ice is intimately mixed with the water ice, at a ratio of 1:10. This implies that the ices formed in cold conditions, likely in the interstellar medium during a phase of amorphous H2O- dominated formation. Frequent collisions within the debris disk are required to explain the observed uniform distribution of icy dust grains.