Abstract
We performed synchrotron X-ray diffraction (XRD) and picosecond acoustic measurements on iron hydrides (FeHX) synthesized in laser-heated diamond anvil cells at pressures up to 100 GPa and 300 K. The obtained XRD data reveals that hcp FeH1.1, hcp FeH0.3, and fcc FeH1.0 were synthesized, and we determined the compressional wave velocities (VP) of the latter two phases. We discovered that the VP–density (ρ) relationships for fcc FeH1.0 changed between 8.7 and 9.2 g/cm3 (at about 60 GPa), which may be due to a magnetic transition. A comparison of the preliminary reference Earth model (PREM) with a Birch’s law extrapolation considering the temperature effect of our experimental VP–ρ results support the hypothesis of hydrogen presence in the Earth’s inner core.
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Acknowledgements
S. I. Kawaguchi helped experiments at SPring-8. The synchrotron XRD experiments were performed at the BL10XU of SPring-8 (Proposal No. 2019A0072, 2019B0072, 2020A0072, 2020B0072, and 2021A0072). This work was supported by JSPS KAKENHI (Grant No. 18J21664 and 19H00716). We would like to thank two anonymous reviewers for very helpful reviews.
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Wakamatsu, T., Ohta, K., Tagawa, S. et al. Compressional wave velocity for iron hydrides to 100 gigapascals via picosecond acoustics. Phys Chem Minerals 49, 17 (2022). https://doi.org/10.1007/s00269-022-01192-8
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DOI: https://doi.org/10.1007/s00269-022-01192-8