2023
DOI: 10.3847/1538-4357/aca614
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Breaking Degeneracies in Formation Histories by Measuring Refractory Content in Gas Giants

Abstract: Relating planet formation to atmospheric composition has been a long-standing goal of the planetary science community. So far, most modeling studies have focused on predicting the enrichment of heavy elements and the C/O ratio in giant planet atmospheres. Although this framework provides useful constraints on the potential formation locations of gas giant exoplanets, carbon and oxygen measurements alone are not enough to determine where a given gas giant planet originated. Here, we show that characterizing the… Show more

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Cited by 19 publications
(15 citation statements)
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“…High-C/O, high-metallicity atmospheres require formation and/or substantial accretion in an environment that is enriched in both carbon and solids. Such conditions are consistent with models that incorporate pebble drift (Booth et al 2017), formation near CO or CO 2 snow lines (Öberg et al 2011), or with pollution by C-rich grains interior to the H 2 O snow line (Chachan et al 2023).…”
Section: Implications For Planet Formationsupporting
confidence: 85%
“…High-C/O, high-metallicity atmospheres require formation and/or substantial accretion in an environment that is enriched in both carbon and solids. Such conditions are consistent with models that incorporate pebble drift (Booth et al 2017), formation near CO or CO 2 snow lines (Öberg et al 2011), or with pollution by C-rich grains interior to the H 2 O snow line (Chachan et al 2023).…”
Section: Implications For Planet Formationsupporting
confidence: 85%
“…The atmospheric abundance of refractory species such as Fe is a particularly important quantity as it is an indicator of the rock composition accreted during the planet's formation (Lothringer et al 2021). Chachan et al (2023) further demonstrate how measuring the abundances of refractory species, specifically Fe, can break degeneracies that exist when trying to determine the formation location of an exoplanet when using only volatile species, such as C-and O-rich species. In the future, our results of measured refractory abundances can be combined with abundances of volatiles from near-infrared observations, to constrain how the population of ultrahot Jupiters formed and evolved, as was recently done with dayside spectra (Kasper et al 2023).…”
Section: Fementioning
confidence: 80%
“…Abundance constraints for the refractory species are of particular importance as they are expected to be accreted onto the planet as solids given their high sublimation temperatures, and hence provide a measure of the accreted rock during formation (Lothringer et al 2021;Knierim et al 2022;Chachan et al 2023). Future work can combine these optical observations with those in the infrared such as JWST and ground-based observatories such as IGRINS/Gemini-S and CRIRES+/VLT, which can constrain volatile species.…”
Section: Discussionmentioning
confidence: 99%
“…While the initial formation locations of hot Jupiters may be obfuscated by postdisk dynamical sculpting, compositional tracers of their birthplaces may remain undisturbed. Chemical signatures of the gas giants' initial locations, such as the carbon-to-oxygen ratio (C/O; Öberg et al 2011) or siliconbased tracers of refractory content (Chachan et al 2023), may remain detectable and can potentially be used to distinguish the initial locations of Jovian planet formation in the future (e.g., Line et al 2021;Reggiani et al 2022).…”
Section: On Hot Jupiters' Initial Formation Locationsmentioning
confidence: 99%