On the volatile enrichments and heavy element content in HD 189733b
O. Mousis, J.I. Lunine, J.-M. Petit, K. Zahnle, L. Biennier, S., Picaud, T.V. Johnson, J.B.A. Mitchell, V. Boudon, D. Cordier, M. Devel, R., Georges, C. Griffith, N. Iro, M.S. Marley, and U. Marboeuf

TL;DR
This paper models the volatile and heavy element content of HD 189733b, reconciling spectroscopic data with internal structure models, and suggests the presence of complex carbon molecules in its atmosphere.
Contribution
It introduces a formation and composition model for HD 189733b's envelope that aligns spectroscopic and structural data, highlighting the role of carbon molecules.
Findings
Range of volatile abundances consistent with heavy element estimates
Supersolar carbon and oxygen abundances fit spectral and structural data
Presence of polycyclic aromatic hydrocarbons may explain apparent abundance contradictions
Abstract
Favored theories of giant planet formation center around two main paradigms, namely the core accretion model and the gravitational instability model. These two formation scenarios support the hypothesis that the giant planet metallicities should be higher or equal to that of the parent star. Meanwhile, spectra of the transiting hot Jupiter HD189733b suggest that carbon and oxygen abundances range from depleted to enriched with respect to the star. Here, using a model describing the formation sequence and composition of planetesimals in the protoplanetary disk, we determine the range of volatile abundances in the envelope of HD189733b that is consistent with the 20--80 Earth-masses of heavy elements estimated to be present in the planet's envelope. We then compare the inferred carbon and oxygen abundances to those retrieved from spectroscopy and we find a range of supersolar values that…
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