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Kohdai Yamamoto

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Articles

Structural evolution of iron oxides melts at Earth’s outer-core pressures

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By Céline Crépisson, Patrick G. Heighway, Thomas Stevens, Adrien Descamps, David McGonegle, Alexis Amouretti, Michal Andrzejewski, Sam Azadi, Erik Brambrink, Carolina Camarda, David Chin, Ana Dutra, Hauke Höppner, Zuzana Konopkova, Motoaki Nakatsutsumi, Norimasa Ozaki, Danae N. Polsin, Jan-Patrick Schwinkendorf, Georgiy Shoulga, Cornelius Strohm, Minxue Tang, Harry Taylor, Monika Toncian, Yizhen Wang, Jin Yao, Gianluca Gregori, Justin S. Wark, Karen Appel, Marion Harmand, Sam M. Vinko, Mila Fitzgerald, Domenic Peake, Karim K. Alaa El-Din, Kohdai Yamamoto, Phani S. Karamched
| Nature Verified
Abstract Oxygen and other light elements comprise up to 5 wt% of the Earth’s outer-core, and may significantly influence its physical properties and the operation of the geodynamo. Here we report in situ X-ray diffraction measurements of Fe, Fe + 4.5 FeO (atomic proportion), and Fe2O3 melts at 177-440 GPa, achieved using laser-driven shock compression at an x-ray free-electron laser.
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