Understanding the stability and properties of hydrous minerals, possibly contributing to hydrogen transport to the lower mantle is crucial as key properties of the constituents of Earth’s mantle, e.g., melting temperatures, rheology, electrical conductivity and atomic diffusivity can be strongly affected by the presence of even small amounts of hydrogen.
Hydrides synthesised at extreme conditions show furthermore promising functionalities for hydrogen storage and room-T superconductivity. However, a reliable analysis of hydrogen-bearing phases at extreme conditions purely from experiment is often not possible and even in combination with computations it is not straightforward to unambiguously refine structures or understand properties.
Therefore, I am working with a broad range of collaborators on finding new techniques and new synergies between experiment and theory, especially the combination of high-pressure NMR with density-functional-theory-based calculations, in order to improve our understanding of phase stability, properties and functionalities of these phases.