Abstract
We present the discovery and refinement by neutron powder diffraction of a new magnetic phase in the quadruple perovskite phase diagram, which is the incommensurate analogue of the well-known pseudo-CE phase of the simple perovskite manganites. We demonstrate that incommensurate magnetic order arises in quadruple perovskites due to the exchange interactions between and sites. Furthermore, by constructing a simple mean field Heisenberg exchange model that generically describes both simple and quadruple perovskite systems, we show that this new magnetic phase unifies a picture of the interplay between charge, magnetic, and orbital ordering across a wide range of compounds.
- Received 1 March 2018
- Revised 28 March 2018
DOI:https://doi.org/10.1103/PhysRevLett.120.257202
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