Measuring the D/H Ratios of Exoplanets and Brown Dwarfs
Caroline V. Morley, Andrew J. Skemer, Brittany E. Miles, Michael R., Line, Eric D. Lopez, Matteo Brogi, Richard S. Freedman, Mark S. Marley

TL;DR
This paper investigates the detectability of deuterium to hydrogen ratios in exoplanets and brown dwarfs using mid-infrared spectra, highlighting the potential of JWST for measuring these ratios to inform planetary formation and evolution.
Contribution
It provides simulations of spectra for giant exoplanets and brown dwarfs to assess the observability of D/H ratios, emphasizing the advantages of CH3D detection and guiding future telescope observations.
Findings
CH3D features are more detectable than HDO in spectra.
Protosolar D/H ratios can be measured in nearby cool brown dwarfs with JWST.
Young Jupiter-mass planets are promising targets for D/H ratio detection.
Abstract
The relative abundance of deuterium and hydrogen is a potent tracer of planet formation and evolution. Jupiter and Saturn have protosolar atmospheric D/H ratios, a relic of substantial gas accretion from the nebula, while the atmospheres of Neptune and Uranus are enhanced in D by accretion of ices into their envelopes. For terrestrial planets, D/H ratios are used to determine the mechanisms of volatile delivery and subsequent atmosphere loss over the lifetime of the planet. Planets and brown dwarfs more massive than 13 M_J quickly fuse their initial D reservoir. Here, we simulate spectra for giant exoplanets and brown dwarfs (2 M_Neptune to ~10 M_Jupiter) from Teff=200--1800 K including both CH3D and HDO to determine the observability of these dominant deuterium isotopologues in mid-infrared thermal emission spectra. Colder objects have stronger molecular features in their spectra, due…
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