Rocky planets are common around other stars, but their atmospheric properties remain
largely unconstrained. Thanks to a wealth of recent planet discoveries and upcoming …

Pressure profoundly alters all states of matter. The symbiotic development of ultrahigh-
pressure diamond anvil cells, to compress samples to sustainable multi-megabar pressures; …

In order to test accretion simulations as well as planetary differentiation scenarios, we have
integrated a multistage core–mantle differentiation model with N-body accretion simulations …

The distributions of major and minor elements in Earth's core and mantle were primarily
established by high pressure, high temperature metal–silicate partitioning during core …

This work investigated the ignition and combustion process of single micron-sized iron
particles in the hot gas flow of burned methane-oxygen-nitrogen mixture. The particle …

The high-pressure melting curve of FeO controls key aspects of Earth's deep interior and the
evolution of rocky planets more broadly. However, existing melting studies on wüstite were …

The mantles of both Earth and Mars are more oxidized than would be expected based on
low pressure equilibration of molten silicate and alloy during their magma ocean stages …

Hexagonal close-packed iron (hcp-Fe) is a main component of Earth's inner core. The
difference in density between hcp-Fe and the inner core in the Preliminary Reference Earth …

The discovery of an extraordinary number of extrasolar planets, characterized by an
unexpected variety of sizes, masses and orbits, challenges our understanding of the …

FeO is a crucial component of the Earth's core, and its thermodynamic properties are
essential to developing more accurate core models. It is also a notorious correlated insulator …