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  Structure and magnetic properties of a new anion-deficient perovskite Pb2Ba2BiFe4ScO13 with crystallographic shear structure

Batuk, M., Tyablikov, O. A., Tsirlin, A. A., Kazakov, S. M., Rozova, M. G., Pokholok, K. V., et al. (2013). Structure and magnetic properties of a new anion-deficient perovskite Pb2Ba2BiFe4ScO13 with crystallographic shear structure. Materials Research Bulletin, 48(9), 3459-3465. doi:10.1016/j.materresbull.2013.05.028.

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Batuk, M., Author
Tyablikov, O. A., Author
Tsirlin, A. A.1, Author           
Kazakov, S. M., Author
Rozova, M. G., Author
Pokholok, K. V., Author
Filimonov, D. S., Author
Antipov, E. V., Author
Abakumov, A. M.2, Author           
Hadermann, J.2, Author           
Affiliations:
1Chemical Metal Science, Max Planck Institute for Chemical Physics of Solids, Max Planck Society, ou_1863405              
2Max Planck Institute for Chemical Physics of Solids, Max Planck Society, ou_1863404              

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 Abstract: Pb2Ba2BiFe4ScO13, a new n = 5 member of the oxygen-deficient perovskite-based A(n)B(n)O(3n-2) homologous series, was synthesized using a solid-state method. The crystal structure of Pb2Ba2BiFe4ScO13 was investigated by a combination of synchrotron X-ray powder diffraction, electron diffraction, high-angle annular dark-field scanning transmission electron microscopy and Mossbauer spectroscopy. At 900 K, it crystallizes in the Ammm space group with the unit cell parameters a = 5.8459(1) angstrom, b = 4.0426(1) angstrom, and c=27.3435(1) angstrom. In the Pb2Ba2BiFe4ScO13 structure, quasi-two-dimensional perovskite blocks are periodically interleaved with 1/2[1 1 0] ((1) over bar 0 1)(p) crystallographic shear (CS) planes. At the CS planes, the corner-sharing FeO6 octahedra are transformed into chains of edge-sharing FeO5 distorted tetragonal pyramids. B-positions of the perovskite blocks between the CS planes are jointly occupied by Fe3+ and Sc3+. The chains of the FeO5 pyramids and (Fe,Sc)O-6 octahedra delimit six-sided tunnels that are occupied by double columns of cations with a lone electron pair (Pb2+). The remaining A-cations (Bi3+, Ba2+) occupy positions in the perovskite block. According to the magnetic susceptibility measurements, Pb2Ba2BiFe4ScO13 is antiferromagnetically ordered below T-N approximate to 350 K. (C) 2013 Elsevier Ltd. All rights reserved.

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Language(s): eng - English
 Dates: 2013-09-17
 Publication Status: Issued
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 Identifiers: eDoc: 670431
ISI: 000322354000076
DOI: 10.1016/j.materresbull.2013.05.028
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Title: Materials Research Bulletin
Source Genre: Journal
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Pages: - Volume / Issue: 48 (9) Sequence Number: - Start / End Page: 3459 - 3465 Identifier: ISSN: 0025-5408