JWST Reveals Carbon-rich Chemistry in a Transitional Disk
M. Volz, C. C. Espaillat, C. V. Pittman, S. L. Grant, T. Thanathibodee, M. McClure, B. Tabone, N. Calvet, F. M. Walter
TL;DR
JWST-MIRI MRS observations reveal a carbon-rich transitional disk around RX J1615.3-3255, with strong emissions from H2O, HCN, C2H2, 12CO2, 13CO2, OH, and 13C12CH2, in stark contrast to GM Aur, which shows primarily H2O and OH. LTE slab modeling yields a CO2/H2O column density ratio of about 2.15 in J1615, indicating enhanced carbon-bearing gas, and detects a hot water reservoir near the star in J1615 that GM Aur lacks. The two disks share similar stellar properties, yet differ in accretion rate and inner-disk dust processing; J1615 has larger, more crystalline grains and lower accretion, conditions that may shield carbon-bearing species and favor their observability. The results expand the catalog of carbon-rich protoplanetary environments and suggest that a combination of accretion-driven UV fields and inner-disk dust evolution shapes the MIR carbon chemistry in transitional disks. This work highlights the chemical diversity of planet-forming regions and motivates broader JWST surveys to understand the prevalence and origins of carbon-rich gas in disks around solar-mass stars.
Abstract
We present JWST-MIRI Medium Resolution Spectrometer (MRS) observations of the Classical T Tauri stars GM Aur and RX J1615.3-3255 (J1615), both hosting transitional disks. Despite their similar stellar and disk properties, the two systems differ strikingly in their carbon-bearing molecular emission. Using local thermodynamic equilibrium (LTE) slab models to analyze spectral lines within the 13.6-17.7 micron wavelength range, we find that J1615 exhibits strong emission from H2O, HCN, C2H2, 12CO2, 13CO2, OH, and 13C12CH2, whereas GM Aur shows only H2O and OH. We measure the accretion rates of both objects using contemporaneous optical spectra and find that J1615's accretion rate is lower than that of GM Aur. We constrain the properties of the dust in both disks using SED modeling and find elevated amounts of crystalline silicates and larger dust grains in the disk of J1615. The enhanced carbon emission in J1615 may result from a combination of lower accretion rate and larger and more processed dust grains in the inner disk, conditions that together may allow carbon-rich gas to persist and be detected. These results expand the sample of protoplanetary disks around solar-mass stars with strong CO2 and C2H2 emission and identify J1615 as a carbon-rich transitional disk, providing new insights into the chemical diversity of planet-forming environments.
