Understanding dense hydrogen at planetary conditions

Understanding dense hydrogen at planetary conditions


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ABSTRACT Materials at high pressures and temperatures are of great interest for planetary science and astrophysics, warm dense-matter physics and inertial confinement fusion research.


Planetary structure models rely on an understanding of the behaviour of elements and their mixtures under conditions that do not exist on Earth; at the same time, planets serve as natural


laboratories for studying materials at extreme conditions. The topic of dense hydrogen is timely given the recent accurate measurements of the gravitational fields of Jupiter and Saturn, the


current and upcoming progress in shock experiments, and the advances in numerical simulations of materials at high pressure. In this Review we discuss the connection between modelling


planetary interiors and the high-pressure physics of hydrogen and helium. We summarize key experiments and theoretical approaches for determining the equation of state and phase diagram of


hydrogen and helium. We relate this to current knowledge of the internal structures of Jupiter and Saturn, and discuss the importance of high-pressure physics to their characterization. KEY


POINTS * Modelling planetary interiors relies on a profound knowledge of the behaviour of materials at high pressures and temperatures. For the gas giant planets, these materials are


hydrogen and helium. * Progress in high-pressure experiments using diamond anvil cells and shock waves is critical for understanding hydrogen under extreme conditions and for calibrating


theoretical models * Simulations of hydrogen at high pressure are essential to understand fundamental physical problems such as its rich phase diagram; assist the experimental realization


and interpretation of new materials; and predict its behaviour for parameters at which experiments cannot be performed. * Jupiter and Saturn are expected to have complex interiors in which


hydrogen metallizes and helium separates from hydrogen. The full understanding of these processes is still a major challenge in high-pressure physics. * Although the structure and evolution


of gas giant planets are dominated by hydrogen and helium, the planets contain other, heavier elements and can have complex interiors that include composition gradients and inhomogeneous


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EXTRASOLAR PLANETS Article Open access 27 April 2022 IMPLICATIONS OF THE IRON OXIDE PHASE TRANSITION ON THE INTERIORS OF ROCKY EXOPLANETS Article 11 February 2021 REFERENCES * McMahon, J.


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authors thank the anonymous referees for comments that helped to improve the manuscript. The authors also acknowledge support from W. Nellis, F. Soubrian, S. Sorella, D. Stevenson, N.


Nettelmann, J. J. Fortney, Y. Miguel, S. Müller, C. Valletta and A. Cumming. R.H. acknowledges support from the Swiss National Science Foundation (SNSF grant 200020_188460) and thanks the


members of the Juno science team for discussions. R.R. acknowledges support by the Deutsche Forschungsgemeinschaft via the projects FOR 2440 and SPP 1992. AUTHOR INFORMATION AUTHORS AND


AFFILIATIONS * Institute for Computational Science, Center for Theoretical Astrophysics and Cosmology, University of Zurich, Zurich, Switzerland Ravit Helled * IBM Quantum, IBM Research —


Zurich, Rüschlikon, Switzerland Guglielmo Mazzola * Institut für Physik, Universität Rostock, Rostock, Germany Ronald Redmer Authors * Ravit Helled View author publications You can also


search for this author inPubMed Google Scholar * Guglielmo Mazzola View author publications You can also search for this author inPubMed Google Scholar * Ronald Redmer View author


publications You can also search for this author inPubMed Google Scholar CONTRIBUTIONS All authors contributed to all aspects of this article. CORRESPONDING AUTHOR Correspondence to Ravit


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Redmer, R. Understanding dense hydrogen at planetary conditions. _Nat Rev Phys_ 2, 562–574 (2020). https://doi.org/10.1038/s42254-020-0223-3 Download citation * Accepted: 20 July 2020 *


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