Abstract
We have carefully investigated the transition pathway of iron under quasihydrostatic pressures. For this purpose, combined measurements of extended x-ray absorption fine structure (EXAFS) and x-ray magnetic circular dichroism at the Fe edge were performed using a helium pressure-transmitting medium. Collapse of the ferromagnetism simultaneously occurs with the structural transition, which is in contrast to the scenario that the transition is driven by the pressure-induced instability of the ferromagnetism in phase of iron. We conclude that shear stress is important to initiate the transition. Our model to fit the EXAFS profile demonstrates that the local atomic arrangement in phase is slightly distorted due to unfinished shuffle motion, whereas shear motion finishes at the beginning of the transition.
- Received 31 March 2014
- Revised 23 June 2014
DOI:https://doi.org/10.1103/PhysRevB.90.014422
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