Insights on the Formation Conditions of Uranus and Neptune from their Deep Elemental Compositions

TL;DR

This paper models the formation conditions of Uranus and Neptune by analyzing their deep elemental compositions, focusing on volatile species and their implications for planetary formation scenarios.

Contribution

It introduces a protoplanetary disk model to predict the bulk volatile compositions of Uranus and Neptune, considering different solid accretion scenarios and their impact on elemental abundances.

Findings

Case 1 predicts argon depletion and enrichments of other volatiles.

Case 2 predicts significant enrichments for all species, including argon.

Both cases align with observed sulfur-to-nitrogen ratios.

Abstract

This study, placed in the context of the preparation for the Uranus Orbiter Probe mission, aims to predict the bulk volatile compositions of Uranus and Neptune. Using a protoplanetary disk model, it examines the evolution of trace species through vapor and solid transport as dust and pebbles. Due to the high carbon abundance found in their envelopes, the two planets are postulated to have formed at the carbon monoxide iceline within the protosolar nebula. The time evolution of the abundances of the major volatile species at the location of the CO iceline is then calculated to derive the abundance ratios of the corresponding key elements, including the heavy noble gases, in the feeding zones of Uranus and Neptune. Supersolar metallicity in their envelopes likely results from accreting solids in these zones. Two types of solids are considered: pure condensates (Case 1) and a mixture of pure condensates and clathrates (Case 2). The model, calibrated to observed carbon enrichments, predicts deep compositions. In Case 1, argon is deeply depleted, while nitrogen, oxygen, krypton, phosphorus, sulfur, and xenon are significantly enriched relative to their protosolar abundances in the two planets. Case 2 predicts significant enrichments for all species, including argon, relative to their protosolar abundances. Consequently, Case 1 predicts near-zero Ar/Kr or Ar/Xe ratios, while Case 2 suggests these ratios are 0.1 and 0.5-1 times their protosolar ratios. Both cases predict a bulk sulfur-to-nitrogen ratio consistent with atmospheric measurements.