Nature Geoscience, Published online: 09 June 2026; doi:10.1038/s41561-026-02001-5 Iron hydride in the Earth’s inner core may exist in a superionic state, according to high-pressure and high-temperature experiments at relevant conditions. Accompanying slow diffusion suggests that the inner core could retain hydrogen on geologic timescales.
Experimental indications of superionic behaviour in iron hydride under Earth’s core conditions
Kenji Ohta
