journal article·2011-01-25

Antiferroelectric (Pb,Bi)1−xFe1+xO3−y Perovskites Modulated by Crystallographic Shear Planes

Artem M. Abakumov, Dmitry Batuk, Joke Hadermann, Marina G. Rozova, Denis V. Sheptyakov, Alexander A. Tsirlin, Daniel Niermann, Florian Waschkowski, Joachim Hemberger, Gustaaf Van Tendeloo, Evgeny V. Antipov

Chemistry of Materials· Volume 23· Issue 2
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Abstract

We demonstrate for the first time a possibility to vary the anion content in perovskites over a wide range through a long-range-ordered arrangement of crystallographic shear (CS) planes. Anion-deficient perovskites (Pb,Bi) 1− x Fe 1+ x O 3− y with incommensurately modulated structures were prepared as single phases in the compositional range from Pb 0.857 Bi 0.094 Fe 1.049 O 2.572 to Pb 0.409 Bi 0.567 Fe 1.025 O 2.796 . Using a combination of electron diffraction and high-resolution scanning transmission electron microscopy, we constructed a superspace model describing a periodic arrangement of the CS planes. The model was verified by refinement of the Pb 0.64 Bi 0.32 Fe 1.04 O 2.675 crystal structure from neutron powder diffraction data ((3 + 1)D S.G. X 2 /m (α0γ), X = [1/2,1/2,1/2,1/2], a = 3.9082(1) Å, b = 3.90333(8) Å, c = 4.0900(1) Å, β = 91.936(2)°, q = 0.05013(4) a * + 0.09170(3) c * at T = 700 K, R P = 0.036, R wP = 0.048). The (Pb,Bi) 1− x Fe 1+ x O 3− y structures consist of perovskite blocks separated by CS planes confined to nearly the (509) p perovskite plane. Along the CS planes, the perovskite blocks are shifted with respect to each other over the 1/2[110] p vector that transforms the corner-sharing connectivity of the FeO 6 octahedra in the perovskite framework to an edge-sharing connectivity of the FeO 5 pyramids at the CS plane, thus reducing the oxygen content. Variation of the chemical composition in the (Pb,Bi) 1− x Fe 1+ x O 3− y series occurs mainly because of a changing thickness of the perovskite block between the interfaces, that can be expressed through the components of the q vector as Pb 6γ+2α Bi 1−7γ−α Fe 1+γ−α O 3−3γ−α . The Pb, Bi, and Fe atoms are subjected to strong displacements occurring in antiparallel directions on both sides of the perovskite blocks, resulting in an antiferroelectric-type structure. This is corroborated by the temperature-, frequency-, and field-dependent complex permittivity measurements. Pb 0.64 Bi 0.32 Fe 1.04 O 2.675 demonstrates a remarkably high resistivity >0.1 T Ω cm at room temperature and orders antiferromagnetically below T N = 608(10) K.
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Research context

OpenAlex topics: Multiferroics and related materials · Ferroelectric and Piezoelectric Materials · Dielectric properties of ceramics

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

Affiliations

Electron Microscopy for Materials Research (EMAT), University of Antwerp, Groenenborgerlaan 171, B-2020, Antwerp, Belgium

Department of Chemistry, Moscow State University, 119991 Moscow, Russia

Laboratory for Neutron Scattering, ETH Zurich and Paul Scherrer Institut (PSI), CH-5232 Villigen, Switzerland

Max Planck Institute for Chemical Physics of Solids, Nöthnitzer Strasse 40, 01187 Dresden, Germany

Institute of Physics II, University of Cologne, Zülpicher Strasse 77, 50937 Cologne, Germany

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