High-Pressure Synthesis of A-Site Ordered Double Perovskite CaMnTi2O6 and Ferroelectricity Driven by Coupling of A-Site Ordering and the Second-Order Jahn–Teller Effect
Abstract:We successfully synthesized a novel
ferroelectric A-site-ordered double perovskite CaMnTi2O6 under
high-pressure and investigated its structure, ferroelectric, magnetic
and dielectric properties, and high-temperature phase transition behavior.
Optical second harmonic generation signal, by frequency doubling 1064
nm radiation to 532 nm, was observed and its efficiency is about 9
times as much as that of SiO2 (α-quartz). This compound
possesses a tetragonal polar structure with space group P42
mc. P-E hysteresis… Show more
“…Based on crystal field stabilization arguments, Mn 2+ in the square-planar environment tends to restore the expected orbital degeneracy preferred by the symmetrically filled e g and t 2g orbitals by making its crystal field environment more regular by shortening second-nearestneighbor Mn-O bond distances. Such a shortening is evident in our low temperature refinements for Mn A , which have a nextnearest-neighbor distance of 2.4Å, very close to that reported in other systems with Mn A 2+ [31,32], and is well below the shortest second-nearest-neighbor distance of 2.65Å observed for any previously reported Mn A 3+ system. We hence assign a formal charge ordering of 1:2, Mn 2+ :Mn 3+ on the A -site.…”
Section: Charge Ordering and Improper Ferroelectric Couplingsupporting
It is of great interest to design and make materials in which ferroelectric polarization is coupled to other order parameters such as lattice, magnetic, and electronic instabilities. Such materials will be invaluable in next-generation data storage devices. Recently, remarkable progress has been made in understanding improper ferroelectric coupling mechanisms that arise from lattice and magnetic instabilities. However, although theoretically predicted, a compact lattice coupling between electronic and ferroelectric (polar) instabilities has yet to be realized. Here we report detailed crystallographic studies of a perovskite Hg A MnO 12 that is found to exhibit a polar ground state on account of such couplings that arise from charge and orbital ordering on both the A -and B-sites, which are themselves driven by a highly unusual Mn A -Mn B intersite charge transfer. The inherent coupling of polar, charge, orbital, and hence magnetic degrees of freedom make this a system of great fundamental interest, and demonstrating ferroelectric switching in this and a host of recently reported hybrid improper ferroelectrics remains a substantial challenge.
“…Based on crystal field stabilization arguments, Mn 2+ in the square-planar environment tends to restore the expected orbital degeneracy preferred by the symmetrically filled e g and t 2g orbitals by making its crystal field environment more regular by shortening second-nearestneighbor Mn-O bond distances. Such a shortening is evident in our low temperature refinements for Mn A , which have a nextnearest-neighbor distance of 2.4Å, very close to that reported in other systems with Mn A 2+ [31,32], and is well below the shortest second-nearest-neighbor distance of 2.65Å observed for any previously reported Mn A 3+ system. We hence assign a formal charge ordering of 1:2, Mn 2+ :Mn 3+ on the A -site.…”
Section: Charge Ordering and Improper Ferroelectric Couplingsupporting
It is of great interest to design and make materials in which ferroelectric polarization is coupled to other order parameters such as lattice, magnetic, and electronic instabilities. Such materials will be invaluable in next-generation data storage devices. Recently, remarkable progress has been made in understanding improper ferroelectric coupling mechanisms that arise from lattice and magnetic instabilities. However, although theoretically predicted, a compact lattice coupling between electronic and ferroelectric (polar) instabilities has yet to be realized. Here we report detailed crystallographic studies of a perovskite Hg A MnO 12 that is found to exhibit a polar ground state on account of such couplings that arise from charge and orbital ordering on both the A -and B-sites, which are themselves driven by a highly unusual Mn A -Mn B intersite charge transfer. The inherent coupling of polar, charge, orbital, and hence magnetic degrees of freedom make this a system of great fundamental interest, and demonstrating ferroelectric switching in this and a host of recently reported hybrid improper ferroelectrics remains a substantial challenge.
“…CaMnTi 2 O 6 was synthesized using pure ilmenite-type MnTiO 3 and CaTiO 3 sealed inside a platinum capsule at 7 GPa and 1700…”
Section: Methodsmentioning
confidence: 99%
“…• C in a multianvil press for 30 min following the work by Aimi et al [3]. The multianvil experiment was performed at GFZ Potsdam with a 18/11 assembly, which was calibrated at room temperature against the phase transitions in Bi metal [4,5].…”
Section: Methodsmentioning
confidence: 99%
“…Unfortunately, while most type-I multiferroics have a large spontaneous polarization, they do not show bulk ferroelectricity due to their large leakage and coercive field [2]. Recently, Aimi et al [3] have discovered that CaMnTi 2 O 6 is a multiferroic with a moderate spontaneous polarization of ∼24 μC/cm 2 and the first example of an oxide containing Mn 2+ allowing a polarization reversal at ambient temperature, thus leading to a novel class of type-I multiferroics.…”
Section: Introductionmentioning
confidence: 99%
“…However, in contrast to CaFeTi 2 O 6 , the square-planar Mn 2+ and the octahedrally coordinated Ti 4+ are shifted along the c axis in CaMnTi 2 O 6 . This breaks the center of inversion, lowering the symmetry from space group P 4 2 Aimi et al [3] have shown that with increasing temperature the off-centering of the square-planar coordinated Mn 2+ and of the Ti 4+ decreases. Concomitantly, the second-harmonicgeneration (SHG) signal decreases monotonically with temperature up to the Curie temperature T c = 630 K, where it becomes zero due to the ferroelectric (space group P 4 2 mc) to paraelectric (space group P 4 2 /nmc) phase transition.…”
The ferroelectric to paraelectric phase transition of multiferroic CaMnTi 2 O 6 has been investigated at high pressures and ambient temperature by second-harmonic generation (SHG), Raman spectroscopy, and powder and single-crystal x-ray diffraction. We have found that CaMnTi 2 O 6 undergoes a pressure-induced structural phase transition (P 4 2 mc → P 4 2 /nmc) at ∼7 GPa to the same paraelectric structure found at ambient pressure and T c = 630 K. The continuous linear decrease of the SHG intensity that disappears at 7 GPa and the existence of a Raman active mode at 244 cm −1 that first softens up to 7 GPa and then hardens with pressure are used to discuss the nature of the phase transition of CaMnTi 2 O 6 , for which a dT c /dP = −48 K/GPa has been found. Neither a volume contraction nor a change in the normalized pressure on the Eulerian strain is observed across the phase transition with all the unit-cell volume data following a second-order Birch-Murnaghan equation of state with a bulk modulus of B 0 = 182.95(2) GPa.
A huge number of compounds with chemical formula ABX
3
adopt the perovskite (Pv)‐type structure or its distorted derivatives. Studies on Pv‐type and related compounds synthesized under high pressures and high temperatures or stable under high pressure have been developed by large contributions of earth science as well as materials science and engineering. In the field of solid‐state chemistry, the stabilization of Pv‐phase by high pressure, the phase relation under various pressure‐temperature conditions, and the structure and properties of obtained metastable Pv phases have been elucidated. This chapter reviews syntheses of high‐pressure Pv in terms of synthetic methods, phase stability, structure, and chemical bonding. Synthetic methods of Pvs aided by pressure, from relative low gas pressure of ∼1 MPa to hydrostatic pressure in solid medium on the order of 10 GPa and the examples.
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