Magnetic investigations for studying planetary interiors
Most of the magnetic methods used for investigating planetary interiors are based on the reasonable hypothesis that the mechanism for the origin of the field is an Earth-like hydromagnetic dynamo: in this case the planet has an electrically conducting ...
A. De Santis, M. Chiappini
doaj +4 more sources
Fluid Dynamics Experiments for Planetary Interiors [PDF]
AbstractUnderstanding fluid flows in planetary cores and subsurface oceans, as well as their signatures in available observational data (gravity, magnetism, rotation, etc.), is a tremendous interdisciplinary challenge. In particular, it requires understanding the fundamental fluid dynamics involving turbulence and rotation at typical scales well beyond
Le Bars, Michael +6 more
openaire +5 more sources
Magnesium oxide-water compounds at megabar pressure and implications on planetary interiors [PDF]
Magnesium Oxide and water are abundant in the interior of planets. Here, the authors predict three new MgO-H2O compounds: Mg2O3H2, MgO3H4 and MgO4H6, and they exhibit superionic behavior in planetary interior conditions.
Shuning Pan +9 more
doaj +2 more sources
Hydrogen-helium immiscibility boundary in gas-giant planetary interiors from machine-learning molecular dynamics [PDF]
The location of the hydrogen-helium (H/He) immiscibility boundary controls whether and where helium rain occurs in giant planets, yet it remains uncertain because high-pressure experiments are challenging and ab initio simulations are limited in system ...
Xiaoyu Wang +2 more
doaj +2 more sources
Seven decades of exploring planetary interiors with rotating convection experiments [PDF]
The interiors of all the planets in the solar system consist of layers, most of which are made out of fluids. When these layers are subject to superadiabatic temperature or compositional gradients, turbulent convection takes place that transports heat ...
Pothérat, Alban, Horn, Susanne
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Shock compression of FeOOH and implications for iron-water interactions in super-earth magma oceans [PDF]
Iron(Fe)-water reactions in a magma ocean can influence water storage and density of planets. These reactions can form Fe-O-H phases, whose density, melting, and electronic properties at planetary interior conditions are important for informing planetary
Yanyao Zhang +21 more
doaj +2 more sources
Prediction of thermally driven quasi-1D superionic states in carbon hydride under giant planetary conditions [PDF]
Planetary interiors experience high-pressure-high temperature conditions that give rise to unconventional states of matter, reshaping our understanding of planetary dynamics and the generation of magnetic fields.
Cong Liu, R. E. Cohen, Jian Sun
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Numerical modelling of liquid metal transport in partially molten H5 ordinary chondrite [PDF]
An equation-based model of liquid metal segregation in Fe-bearing chondrite meteorites is presented. Textural data from natural samples provide the input conditions.
Lansdown, G. +2 more
core +7 more sources
The discovered exoplanet population spans a wide range in planetary bulk properties, from large gas giants to low-mass sub-Neptunes and rocky planets.
Nettelmann, Nadine, Valencia, Diana
core +1 more source
Fluids and melts in planetary interiors: From crust to core–mantle boundaries [PDF]
International audienceAqueous fluids and melts (silicate, carbonate/carbonatites or metallic melts) are major vectors of massand heat transfer in planetary interiors and play an important role in a variety of geochemical andgeodynamical processes that ...
Sanchez-Valle, Carmen +4 more
core +1 more source

