Shock-driven amorphization and melting in Fe2O3

Céline Crépisson; Alexis Amouretti; Marion Harmand; Chrystèle Sanloup; Patrick Heighway; Sam Azadi; David McGonegle; Thomas Campbell; Juan Pintor; David Alexander Chin; Ethan Smith; Linda Hansen; Alessandro Forte; Thomas Gawne; Hae Ja Lee; Bob Nagler; Yuanfeng Shi; Guillaume Fiquet; François Guyot; Mikako Makita; Alessandra Benuzzi-Mounaix; Tommaso Vinci; Kohei Miyanishi; Norimasa Ozaki; Tatiana Pikuz; Hirotaka Nakamura; Keiichi Sueda; Toshinori Yabuuchi; Makina Yabashi; Justin S. Wark; Danae N. Polsin; Sam M. Vinko

doi:10.1103/PhysRevB.111.024209

Shock-driven amorphization and melting in Fe2O3

Céline Crépisson
, Alexis Amouretti
, Marion Harmand
, Chrystèle Sanloup
, Patrick Heighway
, Sam Azadi
, David McGonegle
, Thomas Campbell
, Juan Pintor
, David Alexander Chin
, Ethan Smith
, Linda Hansen
, Alessandro Forte
, Thomas Gawne
, Hae Ja Lee
, Bob Nagler
, Yuanfeng Shi
, Guillaume Fiquet
, François Guyot
, Mikako Makita

Alessandra Benuzzi-Mounaix, Tommaso Vinci, Kohei Miyanishi, Norimasa Ozaki, Tatiana Pikuz, Hirotaka Nakamura, Keiichi Sueda, Toshinori Yabuuchi, Makina Yabashi, Justin S. Wark, Danae N. Polsin, Sam M. Vinko

Résultats de recherche: Contribution à un journal › Article › Revue par des pairs

Résumé

We present measurements on Fe2O3 amorphization and melt under laser-driven shock compression up to 209(10) GPa via time-resolved in situ 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 Fe2O3 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-Fe2O3. The extracted structure factor and pair distribution function of this release phase resemble those reported for Fe2O3 melt at ambient pressure.

langue originale	Anglais
Numéro d'article	024209
journal	Physical Review B
Volume	111
Numéro de publication	2
Les DOIs	https://doi.org/10.1103/PhysRevB.111.024209
état	Publié - 1 janv. 2025
Modification externe	Oui

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10.1103/PhysRevB.111.024209

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Crépisson, C., Amouretti, A., Harmand, M., Sanloup, C., Heighway, P., Azadi, S., McGonegle, D., Campbell, T., Pintor, J., Chin, D. A., Smith, E., Hansen, L., Forte, A., Gawne, T., Lee, H. J., Nagler, B., Shi, Y., Fiquet, G., Guyot, F., ... Vinko, S. M. (2025). Shock-driven amorphization and melting in Fe2O3. Physical Review B, 111(2), Article 024209. https://doi.org/10.1103/PhysRevB.111.024209

@article{3b436976d3a4435bb13522f6f578315a,

title = "Shock-driven amorphization and melting in Fe2O3",

abstract = "We present measurements on Fe2O3 amorphization and melt under laser-driven shock compression up to 209(10) GPa via time-resolved in situ 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 Fe2O3 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-Fe2O3. The extracted structure factor and pair distribution function of this release phase resemble those reported for Fe2O3 melt at ambient pressure.",

author = "C{\'e}line Cr{\'e}pisson and Alexis Amouretti and Marion Harmand and Chryst{\`e}le Sanloup and Patrick Heighway and Sam Azadi and David McGonegle and Thomas Campbell and Juan Pintor and Chin, \{David Alexander\} and Ethan Smith and Linda Hansen and Alessandro Forte and Thomas Gawne and Lee, \{Hae Ja\} and Bob Nagler and Yuanfeng Shi and Guillaume Fiquet and Fran{\c c}ois Guyot and Mikako Makita and Alessandra Benuzzi-Mounaix and Tommaso Vinci and Kohei Miyanishi and Norimasa Ozaki and Tatiana Pikuz and Hirotaka Nakamura and Keiichi Sueda and Toshinori Yabuuchi and Makina Yabashi and Wark, \{Justin S.\} and Polsin, \{Danae N.\} and Vinko, \{Sam M.\}",

note = "Publisher Copyright: {\textcopyright} 2025 authors. Published by the American Physical Society. Published by the American Physical Society under the terms of the {"}https://creativecommons.org/licenses/by/4.0/{"}Creative Commons Attribution 4.0 International license. Further distribution of this work must maintain attribution to the author(s) and the published article's title, journal citation, and DOI.",

year = "2025",

month = jan,

day = "1",

doi = "10.1103/PhysRevB.111.024209",

language = "English",

volume = "111",

journal = "Physical Review B",

issn = "2469-9950",

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}

Crépisson, C, Amouretti, A, Harmand, M, Sanloup, C, Heighway, P, Azadi, S, McGonegle, D, Campbell, T, Pintor, J, Chin, DA, Smith, E, Hansen, L, Forte, A, Gawne, T, Lee, HJ, Nagler, B, Shi, Y, Fiquet, G, Guyot, F, Makita, M, Benuzzi-Mounaix, A, Vinci, T, Miyanishi, K, Ozaki, N, Pikuz, T, Nakamura, H, Sueda, K, Yabuuchi, T, Yabashi, M, Wark, JS, Polsin, DN & Vinko, SM 2025, 'Shock-driven amorphization and melting in Fe2O3', Physical Review B, VOL. 111, Numéro 2, 024209. https://doi.org/10.1103/PhysRevB.111.024209

TY - JOUR

T1 - Shock-driven amorphization and melting in Fe2O3

AU - Crépisson, Céline

AU - Amouretti, Alexis

AU - Harmand, Marion

AU - Sanloup, Chrystèle

AU - Heighway, Patrick

AU - Azadi, Sam

AU - McGonegle, David

AU - Campbell, Thomas

AU - Pintor, Juan

AU - Chin, David Alexander

AU - Smith, Ethan

AU - Hansen, Linda

AU - Forte, Alessandro

AU - Gawne, Thomas

AU - Lee, Hae Ja

AU - Nagler, Bob

AU - Shi, Yuanfeng

AU - Fiquet, Guillaume

AU - Guyot, François

AU - Makita, Mikako

AU - Benuzzi-Mounaix, Alessandra

AU - Vinci, Tommaso

AU - Miyanishi, Kohei

AU - Ozaki, Norimasa

AU - Pikuz, Tatiana

AU - Nakamura, Hirotaka

AU - Sueda, Keiichi

AU - Yabuuchi, Toshinori

AU - Yabashi, Makina

AU - Wark, Justin S.

AU - Polsin, Danae N.

AU - Vinko, Sam M.

N1 - Publisher Copyright: © 2025 authors. Published by the American Physical Society. Published by the American Physical Society under the terms of the "https://creativecommons.org/licenses/by/4.0/"Creative Commons Attribution 4.0 International license. Further distribution of this work must maintain attribution to the author(s) and the published article's title, journal citation, and DOI.

PY - 2025/1/1

Y1 - 2025/1/1

N2 - We present measurements on Fe2O3 amorphization and melt under laser-driven shock compression up to 209(10) GPa via time-resolved in situ 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 Fe2O3 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-Fe2O3. The extracted structure factor and pair distribution function of this release phase resemble those reported for Fe2O3 melt at ambient pressure.

AB - We present measurements on Fe2O3 amorphization and melt under laser-driven shock compression up to 209(10) GPa via time-resolved in situ 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 Fe2O3 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-Fe2O3. The extracted structure factor and pair distribution function of this release phase resemble those reported for Fe2O3 melt at ambient pressure.

UR - https://www.scopus.com/pages/publications/85216929324

U2 - 10.1103/PhysRevB.111.024209

DO - 10.1103/PhysRevB.111.024209

M3 - Article

AN - SCOPUS:85216929324

SN - 2469-9950

VL - 111

JO - Physical Review B

JF - Physical Review B

IS - 2

M1 - 024209

ER -

Shock-driven amorphization and melting in Fe2O3

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