The Roasting Marshmallows Program with IGRINS on Gemini South V: Atmosphere of MASCARA-1b is Enriched in Refractory Elements
arXiv:2606.07497 · doi:10.3847/1538-3881/ae77f1
Abstract
Ultra-hot Jupiters (UHJs; K) enable simultaneous detection of volatile (ice-forming) and refractory (rock-forming) species in planetary atmospheres, providing a powerful diagnostic of planet formation and atmospheric processing. We present a comprehensive high-resolution cross-correlation spectroscopy (HRCCS) analysis of the UHJ MASCARA-1b ( K) using the IGRINS and IGRINS-2 spectrographs. We detect robust (SNR4) signals from HO, CO, OH, Fe I, Mg I, Ca I, and Ti I, marking the most complete atmospheric inventory of MASCARA-1b to date. Using a chemically consistent atmospheric inference framework, we constrain elemental abundances to a typical precision of 0.2 dex, retrieving a solar atmospheric metallicity ([M/H] solar), a C/O ratio (C/O ) consistent with solar value (C/O 0.59), an enhanced refractory abundance ([R/H] solar; stellar), and a moderately super-solar refractory-to-volatile ratio ([R/V] solar). Comparison with formation models suggests that MASCARA-1b most likely accreted material between the soot-HO or HO-CO snowlines (at 68 confidence). We additionally find stellar values for atmospheric Ti/Mg and Ca/Mg ratios (at 68 confidence). The Mg/Fe is also found to be consistent with stellar value at 95 confidence. Therefore, we do not find strong indication of nightside cold trapping in MASCARA-1b. As homogeneous refractory-to-volatile measurements expand across the UHJ population, particularly with upcoming Extremely Large Telescopes, these diagnostics will enable statistically robust tests of emerging trends in giant planet formation and atmospheric evolution.
20 pages, 12 figures, accepted for publication in AJ