The Dyn-Atmo Survey: High-contrast Imaging Spectroscopy of the Substellar Companion HD 13724 B with the JWST NIRSpec IFU
Kielan K. W. Hoch, Alex Madurowicz, Evert Nasedkin, Emily Rickman, Daniella C. Bardalez Gagliuffi, James Mang, Caroline V. Morley, Christopher A. Theissen, William O. Balmer, Brendan P. Bowler, Emily Calamari, Henry Dennen, Jacqueline K. Faherty, Kyle Franson, Mark R. Giovinazzi, Lisseth Gonzales Quevedo, Elena Manjavacas, Piper Lentz, Klara Matuszewska, Ashley Messier, Marshall Perrin, Laurent Pueyo, Jean-Baptiste Ruffio, Kimberly Ward-Duong, Jerry W. Xuan
Abstract
We present the first spectral analysis from the JWST Cycle 3 GO Program #6362, the Dyn-Atmo Survey of dynamical-atmospheric benchmarks, characterizing the atmospheres of directly-imaged companions with dynamical masses and measured orbits. This program has obtained moderate-resolution spectra (R2700, 3-5μm) using the NIRSpec/G395H IFU. We observe the T4-dwarf companion, HD 13724 B, companion to a G-type star at a projected angular separation of 0''2. Updated orbital monitoring constrains the mass to 38.30.6~MJup, which we use as a Gaussian prior when inferring the atmospheric state. We fit the continuum-subtracted spectrum using the BT-SETTL, Sonora Diamondback, Sonora Flame Skimmer, and NEWERA-PHOENIX self-consistent model grids, together with petitRADTRANS atmospheric retrievals. We adopt bulk parameter values of Teff=1150195 K, g=5.10.3 dex, [M/H]=0.40.4, 10(Kzz)=6.33-2.22+2.59, and C/O=0.500.13 using a bayesian average across model grids. We find degeneracies in the models between surface gravity, metallicity, and Kzz for Sonora Diamondback and Flame Skimmer. The Flame Skimmer and NEWERA-PHOENIX vertical mixing strengths are incompatible, with Flame Skimmer finding a systematically lower value. The retrievals favor an atmosphere in chemical equilibrium, with enhanced metallicity and a solar C/O ratio, but with no detection of disequilibrium chemistry, and no detection of trace gases other than CH4, CO2, 12CO and H2O. Ultimately, we identify critical challenges in forward modeling continuum-subtracted G395H spectra in the low signal-to-noise regime. We find that including independent dynamical mass measurements better constrains atmospheric parameters, but degeneracies between self-consistent model parameters limit accurate atmospheric parameter inferences.
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