The compositions of the HR 8799 planets reflect accretion of both solids and metal-enriched gas
arXiv:2602.09422 · doi:10.3847/1538-4357/ae448f
Abstract
With four giant planets (, $T_\rm{eff}\sim900-1200$ K) orbiting between 15-70 au, HR 8799 provides an unparalleled testbed for studying giant planet formation and probing compositional trends across the protoplanetary disk. We present new JWST/NIRSpec IFU observations (m, ) that now include the spectrum of HR 8799 b, and higher S/N spectra for HR 8799 c, d, and e compared to that in Ruffio & Xuan et al. We detect CO, CH, HO, HS, CO, and for planet b, NH. We combine the NIRSpec spectra with m photometry to perform atmospheric retrievals that account for disequilibrium chemistry and clouds, and allow C/H, O/H, N/H, and S/H to scale independently. While the four planets are similarly enriched in carbon and oxygen, with C/H and O/H between stellar, we observe a tentative trend of increasing S/H - a tracer of refractory solids - from stellar with increasing orbital distance. From HR 8799 b's NH abundance, we estimate stellar, suggesting the outer planet accreted significant amounts of N-rich gas. Overall, the elemental abundance patterns we observe are consistent with a picture where planet b formed between the CO snowline and the more-distant N snowline, while the inner planets accreted stellar CO-enriched disk gas within the CO snowline. The excess volatile mass from pebble drift and evaporation implies an integrated pebble flux of . The increase in the planets' S/H with orbital distance implies more solid accretion further out, which is quantitatively compatible with expectations from both pebble and planetesimal accretion ( Minimum Mass Solar Nebula) paradigms.
Published in ApJ. The planet spectra are available in Zenodo at https://doi.org/10.5281/zenodo.19355669
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