Polar and Magnetic Layered A‑Site and Rock Salt B‑Site-Ordered NaLnFeWO6 (Ln = La, Nd) Perovskites

We have expanded the double perovskite family of materials with the unusual combination of layered order in the A sublattice and rock salt order over the B sublattice to compounds NaLaFeWO6 and NaNdFeWO6. The materials have been synthesized and studied by powder X-ray diffraction, neutron diffractio...

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Veröffentlicht in:Inorganic chemistry 2013-11, Vol.52 (21), p.12482-12491
Hauptverfasser: Retuerto, M., Li, M. R., Ignatov, A., Croft, M., Ramanujachary, K. V., Chi, S., Hodges, J. P., Dachraoui, W., Hadermann, J., Tran, T. Thao, Halasyamani, P. Shiv, Grams, C. P., Hemberger, J., Greenblatt, M.
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container_end_page 12491
container_issue 21
container_start_page 12482
container_title Inorganic chemistry
container_volume 52
creator Retuerto, M.
Li, M. R.
Ignatov, A.
Croft, M.
Ramanujachary, K. V.
Chi, S.
Hodges, J. P.
Dachraoui, W.
Hadermann, J.
Tran, T. Thao
Halasyamani, P. Shiv
Grams, C. P.
Hemberger, J.
Greenblatt, M.
description We have expanded the double perovskite family of materials with the unusual combination of layered order in the A sublattice and rock salt order over the B sublattice to compounds NaLaFeWO6 and NaNdFeWO6. The materials have been synthesized and studied by powder X-ray diffraction, neutron diffraction, electron diffraction, magnetic measurements, X-ray absorption spectroscopy, dielectric measurements, and second harmonic generation. At room temperature, the crystal structures of both compounds can be defined in the noncentrosymmetric monoclinic P21 space group resulting from the combination of ordering both in the A and B sublattices, the distortion of the cell due to tilting of the octahedra, and the displacement of certain cations. The magnetic studies show that both compounds are ordered antiferromagnetically below T N ≈ 25 K for NaLaFeWO6 and at ∼21 K for NaNdFeWO6. The magnetic structure of NaNdFeWO6 has been solved with a propagation vector k = (1/2 0 1/2) as an antiferromagnetic arrangement of Fe and Nd moments. Although the samples are potential multiferroics, the dielectric measurements do not show a ferroelectric response.
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R. ; Ignatov, A. ; Croft, M. ; Ramanujachary, K. V. ; Chi, S. ; Hodges, J. P. ; Dachraoui, W. ; Hadermann, J. ; Tran, T. Thao ; Halasyamani, P. Shiv ; Grams, C. P. ; Hemberger, J. ; Greenblatt, M.</creator><creatorcontrib>Retuerto, M. ; Li, M. R. ; Ignatov, A. ; Croft, M. ; Ramanujachary, K. V. ; Chi, S. ; Hodges, J. P. ; Dachraoui, W. ; Hadermann, J. ; Tran, T. Thao ; Halasyamani, P. Shiv ; Grams, C. P. ; Hemberger, J. ; Greenblatt, M. ; Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). High Flux Isotope Reactor (HFIR)</creatorcontrib><description>We have expanded the double perovskite family of materials with the unusual combination of layered order in the A sublattice and rock salt order over the B sublattice to compounds NaLaFeWO6 and NaNdFeWO6. The materials have been synthesized and studied by powder X-ray diffraction, neutron diffraction, electron diffraction, magnetic measurements, X-ray absorption spectroscopy, dielectric measurements, and second harmonic generation. At room temperature, the crystal structures of both compounds can be defined in the noncentrosymmetric monoclinic P21 space group resulting from the combination of ordering both in the A and B sublattices, the distortion of the cell due to tilting of the octahedra, and the displacement of certain cations. The magnetic studies show that both compounds are ordered antiferromagnetically below T N ≈ 25 K for NaLaFeWO6 and at ∼21 K for NaNdFeWO6. The magnetic structure of NaNdFeWO6 has been solved with a propagation vector k = (1/2 0 1/2) as an antiferromagnetic arrangement of Fe and Nd moments. 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R.</creatorcontrib><creatorcontrib>Ignatov, A.</creatorcontrib><creatorcontrib>Croft, M.</creatorcontrib><creatorcontrib>Ramanujachary, K. V.</creatorcontrib><creatorcontrib>Chi, S.</creatorcontrib><creatorcontrib>Hodges, J. P.</creatorcontrib><creatorcontrib>Dachraoui, W.</creatorcontrib><creatorcontrib>Hadermann, J.</creatorcontrib><creatorcontrib>Tran, T. Thao</creatorcontrib><creatorcontrib>Halasyamani, P. Shiv</creatorcontrib><creatorcontrib>Grams, C. P.</creatorcontrib><creatorcontrib>Hemberger, J.</creatorcontrib><creatorcontrib>Greenblatt, M.</creatorcontrib><creatorcontrib>Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). High Flux Isotope Reactor (HFIR)</creatorcontrib><title>Polar and Magnetic Layered A‑Site and Rock Salt B‑Site-Ordered NaLnFeWO6 (Ln = La, Nd) Perovskites</title><title>Inorganic chemistry</title><addtitle>Inorg. Chem</addtitle><description>We have expanded the double perovskite family of materials with the unusual combination of layered order in the A sublattice and rock salt order over the B sublattice to compounds NaLaFeWO6 and NaNdFeWO6. The materials have been synthesized and studied by powder X-ray diffraction, neutron diffraction, electron diffraction, magnetic measurements, X-ray absorption spectroscopy, dielectric measurements, and second harmonic generation. At room temperature, the crystal structures of both compounds can be defined in the noncentrosymmetric monoclinic P21 space group resulting from the combination of ordering both in the A and B sublattices, the distortion of the cell due to tilting of the octahedra, and the displacement of certain cations. The magnetic studies show that both compounds are ordered antiferromagnetically below T N ≈ 25 K for NaLaFeWO6 and at ∼21 K for NaNdFeWO6. The magnetic structure of NaNdFeWO6 has been solved with a propagation vector k = (1/2 0 1/2) as an antiferromagnetic arrangement of Fe and Nd moments. 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title Polar and Magnetic Layered A‑Site and Rock Salt B‑Site-Ordered NaLnFeWO6 (Ln = La, Nd) Perovskites
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