Abstract
Branded for its potential electronic ferroelectricity, charge-ordered has a layered Fe triangular framework, whose topology is a source of degeneracy, both at the charge and spin levels. Here we present an in-depth characterization of , the high-pressure polymorph of , using electron, x-ray, and neutron diffraction, combined with transport and magnetization measurements. We show that is characterized by a misfit-related monoclinic structure, accommodating a buckled triangular layer and two shifted adjacent rectangular planes belonging to a distorted rock salt–type layer. The release of the geometric frustration of the Fe magnetic lattice in the form leads to collinear antiferromagnetic ordering at . Possible coexistence of charge and magnetic orders in this material opens research pathways for the design of tunable multifunctional devices using high-pressure techniques.
- Received 15 October 2014
- Revised 10 March 2015
DOI:https://doi.org/10.1103/PhysRevB.91.214111
©2015 American Physical Society