arXiv · 1602.06721
Local Structure and Spin Transition in Fe2O3 Hematite at High-Pressure
Abstract
The pressure evolution of the local structure of Fe2O3 hematite has been determined for the first time by extended x-ray absorption fine structure up to 79 GPa. The comparison to the different high-pressure forms proposed in the literature suggests that the orthorhombic structure with space group Aba2 is the most probable. The crossover from Fe high-spin to low-spin states with pressure increase has been monitored from the pre-edge region of the Fe K-edge absorption spectra. The "simultaneous" comparison with the local structural changes allows us to definitively conclude that it is the electronic transition that drives the structural transition and not viceversa.
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Andrea Sanson, Innokenty Kantor, Valerio Cerantola, Tetsuo Irifune, Alberto Carnera, Sakura Pascarelli. 2016-02-22. Local Structure and Spin Transition in Fe2O3 Hematite at High-Pressure. https://doi.org/10.1103/physrevb.94.014112
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