The magnetic structure of polar $G$-type charge and orbital ordered Hg-quadruple manganite perovskites
Ben R. M. Tragheim, Fabio Orlandi, En-Pei Liu, Wei-Tin Chen, Mark S. Senn
TL;DR
The paper solves the magnetic ground state of Hg0.7Na0.3Mn3Mn4O12, a Hg-based quadruple manganite with a unique G-type charge and orbital order, using powder neutron diffraction and symmetry analysis. It identifies two antiferromagnetic transitions at approximately 80 K and 60 K, with A'-site Mn showing G-type AFM order in the a-c plane and B-site Mn exhibiting an 'up–up–down–down' AFM order along b accompanied by canting; the magnetic structure is best described by a P2' symmetry with propagation vectors k1=(1,1,1) and k2=(0,0.5,0). The authors discuss symmetry-allowed couplings to secondary lattice distortions (including Zener-polaron-like modes) and propose that while these couplings may fine-tune the ground state, they are unlikely the primary driving force; instead, an improper polarization-related invariant could help stabilize the commensurate B-site order. The results emphasize the distinct magnetic behavior of Hg-based quadruple manganites compared to their Ca/Sr/Cd/Pb counterparts, highlighting the rich interplay of charge, orbital, lattice, and spin degrees of freedom in these materials.
Abstract
The magnetic structure of the novel Hg$_{0.7}$Na$_{0.3}$Mn$_3$Mn$_4$O$_{12}$, a quadruple manganite perovskite that exhibits a unique $G$-type charge and orbital ordered state distinct to other $A^{2+}$Mn$_3$Mn$_4$O$_{12}$ equivalents ($A$ $=$ Ca, Sr, Cd, Pb), has been solved using powder neutron diffraction and symmetry-motivated analysis. A $G$-type-like antiferromagnetic (AFM) ordering of Mn on the $A'$ sites and a `up--up--down--down' AFM moment configuration of Mn spins on the $B$ sites is found to occur. The mechanism for the onset and stabilization of $B$ site `up--up--down--down' AFM order is explored in terms of coupling between structural and magnetic distortions. The results presented here provide evidence of the exotic charge, orbital, electronic and magnetic orderings that quadruple manganite perovskites demonstrate, and further highlighting the distinct chemistry that Hg$^{2+}$ plays in stabilizing novel states compared to other divalent $A$-site cation equivalents.
