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• W2332564384 abstract "We report a Mossbauer spectroscopic study of cementite (Fe${}_{3}$C) in a diamond anvil cell up to 88 GPa. The hyperfine parameters reveal a two-stage loss of magnetism in Fe${}_{3}$C: a ferro-to-paramagnetic transition around 8--10 GPa and a spin transition at about 22 GPa. Full structural refinement based on single-crystal x-ray diffraction data collected at pressures up to $ensuremath{sim}$50 GPa reveals that there are no structural changes associated with the electronic transitions in Fe${}_{3}$C. Our Rapid Communication resolves the long-standing controversy regarding the nature of phase transitions in Fe${}_{3}$C at high pressures." @default.
• W2332564384 created "2016-06-24" @default.
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• W2332564384 date "2012-04-02" @default.
• W2332564384 modified "2023-10-06" @default.
• W2332564384 title "Structurally hidden magnetic transitions in Fe<mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML display=inline><mml:msub><mml:mrow /><mml:mn>3</mml:mn></mml:msub></mml:math>C at high pressures" @default.
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• W2332564384 doi "https://doi.org/10.1103/physrevb.85.140402" @default.
• W2332564384 hasPublicationYear "2012" @default.
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