Sequestration of noble gases in giant planet interiors
arXiv:1003.5940 · doi:10.1103/PhysRevLett.104.121101
Abstract
The Galileo probe showed that Jupiter's atmosphere is severely depleted in neon compared to protosolar values. We show, via ab initio simulations of the partitioning of neon between hydrogen and helium phases, that the observed depletion can be explained by the sequestration of neon into helium-rich droplets within the postulated hydrogen-helium immiscibility layer of the planet's interior. We also demonstrate that this mechanism will not affect argon, explaining the observed lack of depletion of this gas. This provides strong indirect evidence for hydrogen-helium immiscibility in Jupiter.
References in corpus (1)
Cited by in corpus (44)
- Comparing Jupiter interior structure models to Juno gravity measurements and the role of a dilute core
- The Uniform Electron Gas at Warm Dense Matter Conditions
- New models of Jupiter in the context of Juno and Galileo
- Rocky core solubility in Jupiter and giant exoplanets
- Self-Consistent Model Atmospheres and the Cooling of the Solar System's Giant Planets
- Superionic to superionic phase change in water: consequences for the interiors of Uranus and Neptune
- Excess C/O and C/H in outer protoplanetary disk gas
- A Preliminary Jupiter Model
- Modelling the He I triplet absorption at 10830 Angstroms in the atmosphere of HD 209458 b
- The Challenge of Forming a Fuzzy Core in Jupiter
- Saturn layered structure and homogeneous evolution models with different EOSs
- Thermal density functional theory: Time-dependent linear response and approximate functionals from the fluctuation-dissipation theorem
- Understanding Jupiter's Interior
- Deep Atmosphere Composition, Structure, Origin, and Exploration, with Particular Focus on Critical in situ Science at the Icy Giants
- Giant Planets
- An Exploration of Double Diffusive Convection in Jupiter as a Result of Hydrogen-Helium Phase Separation
- Zonal Flow Magnetic Field Interaction in the Semi-Conducting Region of Giant Planets
- Models of Saturn's Interior Constructed with Accelerated Concentric Maclaurin Spheroid Method
- High-temperature miscibility of iron and rock during terrestrial planet formation
- Evidence for a Dichotomy in the Interior Structures of Jupiter and Saturn from Helium Phase Separation
- Scientific rationale of Saturn's in situ exploration
- Measuring Jupiter's water abundance by Juno: the link between interior and formation models
- Modelling the He I triplet absorption at 10830 Angstroms in the atmospheres of HD 189733 b and GJ 3470 b
- Jupiter's formation in the vicinity of the amorphous ice snowline
- X-ray scattering as a probe for warm dense mixtures and high-pressure miscibility
- Path integral Monte Carlo simulations of dense carbon-hydrogen plasmas
- Evolution of Jupiter and Saturn with helium rain
- The Fundamental Connections Between the Solar System and Exoplanetary Science
- Characterisation of the upper atmospheres of HAT-P-32 b, WASP-69 b, GJ 1214 b, and WASP-76 b through their He I triplet absorption
- High Pressure Phase Diagram of Beryllium from \emph{Ab Initio} Free Energy Calculations
- The properties of heavy elements in giant planet envelopes
- Ab Initio Investigation of a Possible Liquid-Liquid Phase Transition in MgSiO3 at Megabar Pressures
- Quantum Langevin molecular dynamics determination of the solar-interior equation of state
- The deep composition of Uranus and Neptune from in situ exploration and thermochemical modeling
- Relation of Gravity, Winds, and the Moment of Inertia of Jupiter and Saturn
- The Properties of G-modes in Layered Semi-Convection
- Benchmarking the ab initio hydrogen equations of state for the interior structure of Jupiter
- H-HO demixing in Uranus and Neptune: Adiabatic structure models
- Internal Structure of Giant and Icy Planets: Importance of Heavy Elements and Mixing
- Study of Jupiter's Interior with Quadratic Monte Carlo Simulations
- On the meaning of the dynamo radius in giant planets with stable layers
- Quantum kinetic theory of light-matter interactions in degenerate plasmas
- Ab initio Simulations of Superionic H2O, H2O2, and H9O4 Compounds
- Interpreting the atmospheric composition of exoplanets: sensitivity to planet formation assumptions