Excess C/O and C/H in outer protoplanetary disk gas
Karin I. Oberg, Edwin A. Bergin

TL;DR
This paper shows that pebble drift in protoplanetary disks can lead to enhanced C/O and C/H ratios in the gas, affecting the composition of forming gas giants and explaining some of Jupiter's observed abundances.
Contribution
It introduces a toy model demonstrating that pebble drift causes CO enrichment between snowlines, altering gas compositions relevant to planet formation.
Findings
CO is enhanced between water and CO snowlines due to pebble drift.
Supersolar C/O and C/H ratios can occur in gas giant formation zones.
Pebble drift influences nitrogen and noble gas abundances, explaining Jupiter's peculiarities.
Abstract
The compositions of nascent planets depend on the compositions of their birth disks. In particular, the elemental compositions of Gas Giant gaseous envelopes depend on the elemental composition of the disk gas from which the envelope is accreted. Previous models demonstrated that sequential freeze-out of O and C-bearing volatiles in disks will result in an supersolar C/O ratios and subsolar C/H ratios in the gas between water and CO snowlines. This result does not take into account, however, the expected grain growth and radial drift of pebbles in disks, and the accompanying re-distribution of volatiles from the outer to the inner disk. Using a toy model we demonstrate that when drift is considered, CO is enhanced between the water and CO snowline, resulting in both supersolar C/O and C/H ratios in the disk gas in the Gas Giant formation zone. This result appears robust to the details…
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