The composition of hot Jupiter atmospheres assembled within chemically evolved protoplanetary discs
arXiv:2009.09444 · doi:10.1093/mnras/staa2944
Abstract
The radial-dependent positions of snowlines of abundant oxygen- and carbon-bearing molecules in protoplanetary discs will result in systematic radial variations in the C/O ratios in the gas and ice. This variation is proposed as a tracer of the formation location of gas-giant planets. However, disc chemistry can affect the C/O ratios in the gas and ice, thus potentially erasing the chemical fingerprint of snowlines in gas-giant atmospheres. We calculate the molecular composition of hot Jupiter atmospheres using elemental abundances extracted from a chemical kinetics model of a disc midplane where we have varied the initial abundances and ionization rates. The models predict a wider diversity of possible atmospheres than those predicted using elemental ratios from snowlines only. As found in previous work, as the C/O ratio exceeds the solar value, the mixing ratio of CH increases in the lower atmosphere, and those of CH and HCN increase mainly in the upper atmosphere. The mixing ratio of HO correspondingly decreases. We find that hot Jupiters with C/O can only form between the CO and CH snowlines. Moreover, they can only form in a disc which has fully inherited interstellar abundances, and where negligible chemistry has occurred. Hence, carbon-rich planets are likely rare, unless efficient transport of hydrocarbon-rich ices via pebble drift to within the CH snowline is a common phenomenon. We predict combinations of C/O ratios and elemental abundances that can constrain gas-giant planet formation locations relative to snowline positions, and that can provide insight into the disc chemical history.
arXiv comment18 pages, 7 figures, and 2 tables are contained in this paper. It was accepted for publication in MNRAS on September 18th, 2020
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