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Research PaperResearchia:202606.08043

The Roasting Marshmallows Program with IGRINS on Gemini South V: Atmosphere of MASCARA-1b is Enriched in Refractory Elements

Krishna Kanumalla

Abstract

Ultra-hot Jupiters (UHJs; $T_{\rm eq} \gtrsim 2000$ 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 ($T_{\rm eq} \approx 2600$ K) using the IGRINS and IGRINS-2 spectrographs. We detect robust (SNR$>$4) signals from H$_2$O, CO, OH, F...

Submitted: June 8, 2026Subjects: Astrophysics; Space Science

Description / Details

Ultra-hot Jupiters (UHJs; Teq≳2000T_{\rm eq} \gtrsim 2000 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 (Teqβ‰ˆ2600T_{\rm eq} \approx 2600 K) using the IGRINS and IGRINS-2 spectrographs. We detect robust (SNR>>4) signals from H2_2O, 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 β‰ˆ\approx0.2 dex, retrieving a solar atmospheric metallicity ([M/H]βŠ™_\odot =0.07βˆ’0.13+0.17= 0.07^{+0.17}_{-0.13} β‰ˆ1.2Γ—\approx 1.2\times solar), a C/O ratio (C/O =0.65βˆ’0.08+0.08= 0.65^{+0.08}_{-0.08}) consistent with solar value (C/O == 0.59), an enhanced refractory abundance ([R/H]βŠ™_\odot =0.40βˆ’0.17+0.23β‰ˆ2.5Γ—= 0.40^{+0.23}_{-0.17} \approx 2.5\times solar; β‰ˆ3.8Γ—\approx 3.8\times stellar), and a moderately super-solar refractory-to-volatile ratio ([R/V]βŠ™_\odot =0.36βˆ’0.09+0.11= 0.36^{+0.11}_{-0.09} β‰ˆ2.3Γ—\approx 2.3\times solar). Comparison with formation models suggests that MASCARA-1b most likely accreted material between the soot-H2_2O or H2_2O-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.


Source: arXiv:2606.07497v1 - http://arxiv.org/abs/2606.07497v1 PDF: https://arxiv.org/pdf/2606.07497v1 Original Link: http://arxiv.org/abs/2606.07497v1

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Date:
Jun 8, 2026
Topic:
Space Science
Area:
Astrophysics
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The Roasting Marshmallows Program with IGRINS on Gemini South V: Atmosphere of MASCARA-1b is Enriched in Refractory Elements | Researchia