Are NH and CO ice present on Miranda?
arXiv:2309.04844 · doi:10.3847/PSJ/acf834
Abstract
Published near-infrared spectra of the four largest classical Uranian satellites display the presence of discrete deposits of CO ice, along with subtle absorption features around 2.2 m. The two innermost satellites, Miranda and Ariel, also possess surfaces heavily modified by past endogenic activity. Previous observations of the smallest satellite, Miranda, have not detected the presence of CO ice, and a report of an absorption feature at 2.2 m has not been confirmed. An absorption feature at 2.2 m could result from exposed or emplaced NH- or NH-bearing species, which have a limited lifetime on Miranda's surface, and therefore may imply that Miranda's internal activity was relatively recent. In this work, we analyzed near-infrared spectra of Miranda to determine whether CO ice and the 2.2-m feature are present. We measured the band area and depth of the CO ice triplet (1.966, 2.012, and 2.070 m), a weak 2.13-m band attributed to CO ice mixed with HO ice, and the 2.2-m band. We confirmed a prior detection of a 2.2-m band on Miranda, but we found no evidence for CO ice, either as discrete deposits or mixed with HO ice. We compared a high signal-to-noise spectrum of Miranda to synthetic and laboratory spectra of various candidate compounds to shed light on what species may be responsible for the 2.2-m band. We conclude that the 2.2-m absorption is best matched by a combination of NH ice with NH-hydrates or NH-HO mixtures. NH-bearing salts like NHCl are also promising candidates that warrant further investigation.
29 pages, 10 figures. Accepted for publication in Planetary Science Journal
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