Jupiter's interior from Juno: Equation-of-state uncertainties and dilute core extent
Author
Howard, S.Guillot, T.
Bazot, M.
Miguel, Y.
Stevenson, D.J.
Galanti, E.
Kaspi, Y.
Hubbard, W.B.
Militzer, B.
Helled, R.
Nettelmann, N.
Idini, B.
Bolton, S.
Affiliation
Lunar and Planetary Laboratory, University of ArizonaIssue Date
2023-03-28Keywords
Equation of statePlanets and satellites: composition
Planets and satellites: gaseous planets
Planets and satellites: individual: Jupiter
Planets and satellites: interiors
Metadata
Show full item recordPublisher
EDP SciencesCitation
A&A 672, A33 (2023)Journal
Astronomy and AstrophysicsRights
© The Authors 2023. Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Context. The Juno mission has provided measurements of Jupiter's gravity field with an outstanding level of accuracy, leading to better constraints on the interior of the planet. Improving our knowledge of the internal structure of Jupiter is key to understanding its formation and evolution but is also important in the framework of exoplanet exploration. Aims. In this study, we investigated the differences between the state-of-the-art equations of state and their impact on the properties of interior models. Accounting for uncertainty on the hydrogen and helium equation of state, we assessed the span of the interior features of Jupiter. Methods. We carried out an extensive exploration of the parameter space and studied a wide range of interior models using Markov chain Monte Carlo simulations. To consider the uncertainty on the equation of state, we allowed for modifications of the equation of state in our calculations. Results. Our models harbour a dilute core and indicate that Jupiter's internal entropy is higher than what is usually assumed from the Galileo probe measurements. We obtain solutions with extended dilute cores, but contrary to other recent interior models of Jupiter, we also obtain models with small dilute cores. The dilute cores in such solutions extend to ∼20% of Jupiter's mass, leading to better agreement with formation-evolution models. Conclusions. We conclude that the equations of state used in Jupiter models have a crucial effect on the inferred structure and composition. Further explorations of the behaviour of hydrogen-helium mixtures at the pressure and temperature conditions in Jupiter will help to constrain the interior of the planet, and therefore its origin. © 2023 The Authors.Note
Open access articleISSN
0004-6361Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.1051/0004-6361/202245625
Scopus Count
Collections
Except where otherwise noted, this item's license is described as © The Authors 2023. Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License.

