Host: Japan Association of Mineralogical Sciences
We previously demonstrated that quasielastic neutron scattering is uniquely effective for analyzing atomic-scale hydrogen transport processes in crystalline hydrous minerals. We recently started to apply it for analyzing hydrogen transport in hydrated amorphous silicate of nanoscale particles. From the results at T≦300 K where crystallization does not occur, we identified two types of transport processes, which have implication for water storage mechanism in this potential career of water into early Earth.