Carbon-rich planet formation in a solar composition disk

Abstract

The C--to--O ratio is a crucial determinant of the chemical properties of planets. The recent observation of WASP 12b, a giant planet with a C/O value larger than that estimated for its host star, poses a conundrum for understanding the origin of this elemental ratio in any given planetary system. In this paper, we propose a mechanism for enhancing the value of C/O in the disk through the transport and distribution of volatiles. We construct a model that computes the abundances of major C and O bearing volatiles under the influence of gas drag, sublimation, vapor diffusion, condensation and coagulation in a multi--iceline 1+1D protoplanetary disk. We find a gradual depletion in water and carbon monoxide vapors inside the water's iceline with carbon monoxide depleting slower than water. This effect increases the gaseous C/O and decreases the C/H ratio in this region to values similar to those found in WASP 12b's day side atmosphere. Giant planets whose envelopes were accreted inside the water's iceline should then display C/O values larger than those of their parent stars, making them members of the class of so-called ``carbon-rich planets''.

8 pages, 4 figures, accepted for publication ApJ

References in corpus (5)

• Gas- and dust evolution in protoplanetary disks
• A chemical model for the atmosphere of hot Jupiters
• Evolution of Migrating Planets Undergoing Gas Accretion
• Turbulent diffusion in protoplanetary discs: the effect of an imposed magnetic field
• Extrasolar Carbon Planets

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