Abstract
Using nonresonant Fe x-ray emission spectroscopy, we reveal that Sr substitution into decouples the Fe moment from the volume collapse transition, yielding a collapsed-tetragonal, paramagnetic normal state out of which superconductivity develops. X-ray diffraction measurements implicate the -axis lattice parameter as the controlling criterion for the Fe moment, promoting a generic description for the appearance of pressure-induced superconductivity in the alkaline-earth-based 122 ferropnictides (A. The evolution of with pressure lends support to theories for superconductivity involving unconventional pairing mediated by magnetic fluctuations.
- Received 12 November 2013
- Revised 24 September 2014
DOI:https://doi.org/10.1103/PhysRevB.90.144506
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