2021 Volume 116 Issue 6 Pages 309-313
The Earth’s core is believed to contain some light elements because it is 10% less dense than pure Fe under the corresponding pressure and temperature conditions. Hydrogen, a promising candidate among light elements, has phase relations and physical properties that have been investigated mainly for the Fe–H system. This study specifically examined an Fe–Si–H system using in–situ neutron diffraction experiments to investigate the site occupancy of deuterium of hcp–Fe0.95Si0.05 hydride at 14.7 GPa and 800 K. To date, this pressure condition is the highest for neutron diffraction experiments conducted at high pressure and high temperature, where crystal structure analysis has been conducted. Results of Rietveld refinement indicate hcp–Fe0.95Si0.05 hydride as having deuterium (D) occupancy of 0.24(2) exclusively at the interstitial octahedral site in the hcp lattice. The effect on the site occupancy of D by addition of 2.6 wt% Si into Fe (Fe0.95Si0.05) was negligible compared to results obtained from an earlier study of an Fe–D system (Machida et al., 2019).
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists
