Evidence of superionic ice: news about the unusual magnetic fields of Uranus and Neptune

How conductive ice is formed at several thousand degrees and millions of times atmospheric pressure.


Not all ice is the same. The solid form of water comes in more than a dozen different - sometimes more, sometimes less crystalline - structures, depending on the conditions of pressure and temperature in the environment. Superionic ice is a special crystalline form, half solid, half liquid - and electrically conductive. Its existence has been predicted on the basis of various models and has already been observed on several occasions under - very extreme - laboratory conditions. However, the exact conditions at which superionic ices are stable remain controversial. A team of scientists led by Vitali Prakapenka from the University of Chicago, which also includes Sergey Lobanov from the German Research Center for Geosciences GFZ Potsdam, has now measured the structure and properties of two superionic ice phases (ice XVIII and ice XX). They brought water to extremely high pressures and temperatures in a laser-heated diamond anvil cell. At the same time, the samples were examined with regard to structure and electrical conductivity. The results were published today in the renowned journal Nature Physics. They provide another piece of the puzzle in the spectrum of the manifestations of water. And they may also help to explain the unusual magnetic fields of the planets Uranus and Neptune, which contain a lot of water.

Hot ice?

Ice is cold. At least type I ice from our freezer, snow or from a frozen lake. In planets or in laboratory high-pressure devices, there are different species of ice, type VII or VIII, for example, which exist at several hundred or thousand degrees Celsius. However, this is only because of very high pressures of several ten Gigapascal.

Pressure and temperature span the space for the so-called phase diagram of a substance: Depending on these two parameters, the various manifestations of water and the transitions between solid, gaseous, liquid and hybrid states are recorded here - as they are predicted theoretically or have already been proven in experiments.

Linking fundamental physics with geological questions

The higher the pressure and temperature, the more difficult such experiments are. And so the phase diagram of water - with ice as its solid phase - still has quite a few inaccuracies and inconsistencies in the extreme ranges. 

"Water is actually a relatively simple chemical compound consisting of one oxygen and two hydrogen atoms. Nevertheless, with its often unusual behaviour, it is still not fully understood. In the case of water, the fundamental physical and geoscientific interests come together because water plays an important role inside many planets. Not only in terms of the formation of life and landscapes, but - in the case of the gaseous planets Uranus and Neptune - also for the formation of their unusual planetary magnetic fields," says Sergey Lobanov, geophysicist at GFZ Potsdam.

Unique conditions in the lab

Sergey Lobanov is part of the team led by first author Vitali Prakapenka and Nicholas Holtgrewe, both from the University of Chicago, and Alexander Goncharov from the Carnegie Institution of Washington. They have now further characterized the phase diagram of water at its extremes. Using laser-heated diamond anvil cells - the size of a computer mouse - they have generated high pressures of up to 150 Gigapascal (about 1.5 million times atmospheric pressure) and temperatures of up to 6,500 Kelvin (about 6,227 degrees Celsius). In the sample chamber, which is only a few cubic millimetres in size, conditions then prevail that occur at the depth of several thousand kilometres inside Uranus or Neptune.

The scientists used X-ray diffraction to observe how the crystal structure changes under these conditions. They carried out these experiments using the extremely bright synchrotron X-rays at the Advanced Photon Source (APS) of the Argonne National Laboratory at the University of Chicago. A second series of experiments at the Earth and Planets Laboratory of the Carnegie Institution of Washington used optical spectroscopy to determine the electronic conductivity.

Structural changes in ice as it passes through phase space: formation of superionic ice

The researchers first produced ice VII or X from water at room temperature by increasing the pressure to several tens of Gigapascal (see the phase diagram). And then, at constant pressure, they increased the temperature by heating it with laser light. In the process, they observed how the crystalline ice structure changed: First, the oxygen and hydrogen atoms moved a little around their fixed positions. Then only the oxygen remained fixed and formed its own cubic crystal lattice. As the temperature rose, the hydrogen ionised, i.e. gave up its only electron to the oxygen lattice. Its atomic nucleus - a positively charged proton - then whizzed through this solid, making it electrically conductive. In this way, a hybrid of solid and liquid is created: superionic ice.

Its existence was predicted on the basis of various models and has already been observed on several occasions under laboratory conditions. The scientists have now been able to synthesize and identify two superionic ice phases - ice XVIII and ice XX –, and to delineate the pressure and temperature conditions of their stability. "Due to their distinct density and increased optical conductivity, we assign the observed structures to the theoretically predicted superionic ice phases," explains Lobanov.

Consequences for the explanation of the magnetic field of Uranus and Neptune

In particular, the phase transition to a conducting liquid has interesting consequences for the open questions surrounding the magnetic field of Uranus and Neptune, which presumably consist of more than sixty percent water. Their magnetic field is unusual in that it does not run quasi parallel and symmetrically to the axis of rotation - as it does on Earth - but is skewed and off-centre. Models of its formation therefore assume that it is not generated - as on Earth - by the motion of molten iron in the core, but by a conductive water-rich liquid in the outer third of Uranus or Neptune.

"In the phase diagram, we can draw the pressure and temperature in the interiors of Uranus and Neptune. Here, the pressure can roughly be taken as a measure of the depth inside. Based on the refined phase boundaries we have measured, we see that about the upper third of both planets is liquid, but deeper interiors contain solid superionic ices. This confirms the predictions about the origin of the observed magnetic field", Lobanov sums up.


The geophysicist emphasises that further investigations to better clarify the inner structure and the magnetic field of the two gas planets will be carried out at the GFZ. Here, in addition to the diamond anvil cells already in use, there is both the corresponding high-pressure laboratory and the highly sensitive spectroscopic measuring equipment. Lobanov set up the latter as part of his funding as head of the Helmholtz Young Investigators Group CLEAR to investigate the phenomena of the deep Earth with unconventional ultra-fast time-resolved spectroscopy techniques.

Funding: The work of Sergey Lobanov was supported within the Helmholtz Young Investigators Program CLEAR (VH-NG-1325).

Original study: Prakapenka, V.B., Holtgrewe, N., Lobanov, S.S., and Goncharov, A. 2021. Strucutre and properties of two superionic ice phases. Nature Physics. DOI: 10.1038/s41567-021-01351-8

Scientific contact:

Dr. Sergey S. Lobanov
Junior Group Leader
Chemistry and Physics of Earth Materials
Helmholtz Centre Potsdam
GFZ German Research Centre for Geosciences
14473 Potsdam
Phone: +49 331 288-28607
Email: sergey.lobanov@gfz-potsdam.de

Media contact:

Dr. Uta Deffke
Public and Media Relations
Helmholtz Centre Potsdam
GFZ German Research Centre for Geosciences
14473 Potsdam
Phone: +49 331 288-1049
Email: uta.deffke@gfz-potsdam.de

Additional News

DEUQUA Logo mit Mammut und Friedenstaube

DEUQUA 2022 Tagung am GFZ

PAW Logo

Postdoc Appreciation Week Germany

Building, photo taken in winter, Isaac Newton Institute

Simons Scholarship for Dr Monika Korte

Die Verteilung der seismischen Stationen auf einer Karte der Region.

How deeply does Eifel volcanism sleep?

Geomagnetic Field. Space with stars, Earth with animation around

GFZ film among the finalists of the Earth Futures Festival 2022

Earth's radiation belt: High-energy particles modelled around the Earth. The particles are ring-shaped

A new population of particles in the Earth’s radiation belts

[Translate to English:] Die teilnehmenden GFZ Mitarbeiter als Gruppenfoto

2nd proWissen run in Potsdam with successful participation by GFZ employees

The group on the first day of work.

New faces at the GFZ - start of the training year 2022/2023

Forest vs no forest on two sides of a road

Agriculture drives more than 90% of tropical deforestation

Group photo: people on the roof terrace of a house

2nd International Symposium of International Association of Geodesy’s Commission 4…

[Translate to English:] Foto eines Bergs mit darüber gelegter Skizze des geologischen Profils.

How thick should clay be as a host rock for a repository?

White dots of different thicknesses in a hexagonal pattern on a black ground.

Synthesis of hexagonal SiGe semiconductor using high pressure and temperature

Landslide on a slope directly adjacent to a settlement with small houses.

Landslides increasingly threaten the world's urban poor cities

Different coloured liquids mix in an aquarium. A child watches.

Catching up after Corona: "GEOtogether" brings joy for pupils in collaborative…

A woman and a man stand on a stage holding a picture with a coloured map of Türkiye..

Four decades of joint Turkish-German earthquake research

Egon Althaus sitting around a table with colleagues outside on a project

We mourn the death of Egon Althaus (1933-2022)

A dry dam near Capetown, South Africa.

The challenge of unprecedented floods and droughts in risk management

Drawing of a fictional historical submersible.

Eleven short research stays with GFZ participation funded

Drilling platform on Lake Junin with several people on it

Tropical glaciers followed the rhythm of the ice sheet expansion in the northern…

Schematic representation of the VECTOR project: A large arrow with different levels - from the earth's surface to underground.

Improving the exploration efficiency in Europe

Hoby Razafindrakoto

Project from Dr. Razafindrakoto to create a seismological lab in Madagascar wins ARISE…

3D digital Earth at night

Open-Earth-Monitor getting started

The dam of the Steinbach Dam in the Eifel region, cut by flooding but not destroyed.

Flood risk management after the Eifel flood in July 2021

Group picture of the Cermak7 Conference in front of the Museum Barberini in Potsdam

International heat flow conference and workshop in Potsdam

Castor platform in the ocean. The sea is still.

Filling geological gas reservoirs: Causal research in the most important event of induced…

People sit on chairs in a circle in a room.

GFZ PhD Days

Jeffrey Perez in front of the Logo of the meeting

Two GFZ Researchers participate in the 71st Lindau Nobel Laureate Meeting

Young woman standing with certificate in hand in a hall in front of the lettering EAGE

Best Paper Award for Evgeniia Martuganova

Four persons are holding a large golden key, standing in front of a house

Housing for visiting scientists


Favoring curiosity-driven research of the solid earth

back to top of main content