HAL (France)
open access
Shock compression of FeOOH and implications for iron-water interactions in super-earth magma oceans
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 models. Here, we study natural goethite (α-Fe
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