Shock-driven amorphization and melting in Fe2O3
We present measurements on Fe<sub>2</sub>O<sub>3</sub> amorphization and melt under laser-driven shock compression up to 209(10) GPa via time-resolved <em>in situ</em> x-ray diffraction. At 122(3) GPa, a diffuse signal is observed indicating the presence of a nonc...
Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
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Format: | Journal article |
Language: | English |
Published: |
American Physical Society
2025
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Summary: | We present measurements on Fe<sub>2</sub>O<sub>3</sub> amorphization and melt under laser-driven shock compression up to 209(10) GPa via time-resolved <em>in situ</em> x-ray diffraction. At 122(3) GPa, a diffuse signal is observed indicating the presence of a noncrystalline phase. Structure factors have been extracted up to 182(6) GPa showing the presence of two well-defined peaks. A rapid change in the intensity ratio of the two peaks is identified between 145(12) and 151(12) GPa, indicative of a phase change. The noncrystalline diffuse scattering is consistent with shock amorphization of Fe<sub>2</sub>O<sub>3</sub> between 122(3) and 145(12) GPa, followed by an amorphous-to-liquid transition above 151(12) GPa. Upon release, a noncrystalline phase is observed alongside crystalline α-Fe<sub>2</sub>O<sub>3</sub>. The extracted structure factor and pair distribution function of this release phase resemble those reported for Fe<sub>2</sub>O<sub>3</sub> melt at ambient pressure. |
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