A new equation of state for dense hydrogen-helium mixtures II: taking into account hydrogen-helium interactions
arXiv:2107.04434 · doi:10.3847/1538-4357/abfc48
Abstract
In a recent paper (Chabrier et al. 2019), we have derived a new equation of state (EOS) for dense hydrogen/helium mixtures which covers the temperature-density domain from solar-type stars to brown dwarfs and gaseous planets. This EOS is based on the so-called additive volume law and thus does not take into account the interactions between the hydrogen and helium species. In the present paper, we go beyond these calculations by taking into account H/He interactions, derived from quantum molecular dynamics simulations. These interactions, which eventually lead to H/He phase separation, become important at low temperature and high density, in the domain of brown dwarfs and giant planets. The tables of this new EOS are made publicly available.
To be published in The Astrophysical Journal
References in corpus (5)
- New evolutionary models for pre-main sequence and main sequence low-mass stars down to the hydrogen-burning limit
- Hydrogen-Helium Mixtures in the Interiors of Giant Planets
- New models of Jupiter in the context of Juno and Galileo
- A new equation of state for dense hydrogen-helium mixtures
- Jupiter internal structure: the effect of different equations of state
Cited by in corpus (37)
- SWIFT: A modern highly-parallel gravity and smoothed particle hydrodynamics solver for astrophysical and cosmological applications
- Impact of a new H/He equation of state on the evolution of massive brown dwarfs. New determination of the hydrogen burning limit
- Jupiter's interior from Juno: Equation-of-state uncertainties and dilute core extent
- Accounting for non-ideal mixing effects in the hydrogen-helium equation of state
- TOI-5005 b: A super-Neptune in the savanna near the ridge
- Towards a new era in giant exoplanet characterisation
- Convective Mixing in Gas Giant Planets with Primordial Composition Gradients
- GASTLI: An open-source coupled interior-atmosphere model to unveil gas giant composition
- Revising the Giant Planet Mass-Metallicity Relation: Deciphering the Formation Sequence of Giant Planets
- Jupiter and jovian (exo)-planets in Palatini gravity
- Shallowness of circulation in hot Jupiters -- Advancing the Ohmic dissipation model
- H-HO demixing in Uranus and Neptune: Adiabatic structure models
- The effect of cloudy atmospheres on the thermal evolution of warm giant planets from an interior modelling perspective
- Diversity of low-mass planet atmospheres in the C-H-O-N-S-Cl system with interior dissolution, nonideality, and condensation: Application to TRAPPIST-1e and sub-Neptunes
- Unraveling the origin of giant exoplanets: Observational implications of convective mixing
- Cooling process of substellar objects in scalar-tensor gravity
- REMIX SPH -- improving mixing in smoothed particle hydrodynamics simulations using a generalised, material-independent approach
- Three Warm Jupiters orbiting TOI-6628, TOI-3837, TOI-5027 and one sub-Saturn orbiting TOI-2328
- Breaking degeneracies in exoplanetary parameters through self-consistent atmosphere-interior modelling
- The Sonora Substellar Atmosphere Models VI. Red Diamondback: Extending Diamondback with SPHINX for Brown Dwarf Early Evolution
- On the origin of Jupiter's fuzzy core: constraints from N-body, impact and evolution simulations
- The Evolution of Jupiter and Saturn as a function of the Parameter R
- Investigating the eccentricity distribution of transiting, long-period giant planets
- Further constraints on Jupiter's primordial structure
- TOI-3288 b and TOI-4666 b: two gas giants transiting low-mass stars characterised by NIRPS
- Detection and characterisation of a 106-day transiting Jupiter : TOI-2449 b / NGTS-36 b
- Near-infrared spectroscopic characterisation of Gaia ultra-cool dwarf candidates; Spectral types and peculiarities
- Probing Superheavy Dark Matter with Exoplanets
- No dilute core produced in simulations of giant impacts on to Jupiter
- An Energy Perspective of Core Erosion in Gas Giant Planets
- A Validated Low-to-Intermediate Mass Planetary Interior Structure Model and New Mass-Radius Relations
- The Evolution and Internal Structure of Neptunes and Sub-Neptunes: The importance of thermal conductivity in non-convective regions
- Ohmic dissipation during the formation of super-Earth
- Icy or rocky? Convective or stable? New interior models of Uranus and Neptune
- Resizing the giants: How modelling adiabatic interiors impacts predicted planetary radii
- Rapid and Predictive Planet Population Synthesis Model (RAPPS) I. Upgraded model and resulting synthetic populations
- A Denser Hydrogen Inferred from First-Principles Simulations Challenges Jupiter's Interior Models