High-pressure structural behavior of α-Fe2O3 studied by single-crystal X-ray diffraction and synchrotron radiation up to 25 GPa

In situ X‑ray diffraction experiments were carried out at pressures up to 25 GPa on a synthetic hematite (α-Fe 2 O 3 ) crystal using synchrotron radiation in an angle-dispersive setup. Experiments were performed in diamond-anvil cells using neon as a pressure-transmitting medium. Single-crystal diff...

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Hauptverfasser: Schouwink, Pascal (VerfasserIn) , Dubrovinsky, Leonid (VerfasserIn) , Glazyrin, Konstantin (VerfasserIn) , Merlini, Marco (VerfasserIn) , Hanfland, Michael (VerfasserIn) , Pippinger, Thomas (VerfasserIn) , Miletich-Pawliczek, Ronald (VerfasserIn)
Dokumenttyp: Article (Journal)
Sprache:Englisch
Veröffentlicht: [2011]
In: American mineralogist
Year: 2011, Jahrgang: 96, Heft: 11/12, Pages: 1781-1786
ISSN:1945-3027
DOI:10.2138/am.2011.3775
Online-Zugang:Verlag, lizenzpflichtig, Volltext: https://doi.org/10.2138/am.2011.3775
Verlag, lizenzpflichtig, Volltext: https://www.degruyterbrill.com/document/doi/10.2138/am.2011.3775/html
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Verfasserangaben:Pascal Schouwink, Leonid Dubrovinsky, Konstantin Glazyrin, Marco Merlini, Michael Hanfland, Thomas Pippinger, Ronald Miletich

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520 |a In situ X‑ray diffraction experiments were carried out at pressures up to 25 GPa on a synthetic hematite (α-Fe 2 O 3 ) crystal using synchrotron radiation in an angle-dispersive setup. Experiments were performed in diamond-anvil cells using neon as a pressure-transmitting medium. Single-crystal diffraction data were collected from omega scans and structural refinements were carried out for 10 pressure points. Bulk and linear incompressibilities were obtained from least-squares fits of refined data to the Eulerian strain based Birch-Murnaghan equation of state. Finite strain analysis suggests a truncation at second order, yielding results of K 0 = 207(3), Ka 0 = 751(17), and K c0 = 492(8) for bulk and axial moduli, respectively. The a-axis is about 1.5 times stiffer than the c-axis. Compression of the main structural feature, the FeO 6 octahedra, is quite uniform, with just slight changes of distortion parameters at higher pressures. 
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