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 |
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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. |
doi_str_mv | 10.1021/ic401491y |
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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. Although the samples are potential multiferroics, the dielectric measurements do not show a ferroelectric response.</description><identifier>ISSN: 0020-1669</identifier><identifier>EISSN: 1520-510X</identifier><identifier>DOI: 10.1021/ic401491y</identifier><identifier>PMID: 24138134</identifier><language>eng</language><publisher>United States: American Chemical Society</publisher><ispartof>Inorganic chemistry, 2013-11, Vol.52 (21), p.12482-12491</ispartof><rights>Copyright © 2013 American Chemical Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://pubs.acs.org/doi/pdf/10.1021/ic401491y$$EPDF$$P50$$Gacs$$H</linktopdf><linktohtml>$$Uhttps://pubs.acs.org/doi/10.1021/ic401491y$$EHTML$$P50$$Gacs$$H</linktohtml><link.rule.ids>230,314,776,780,881,27053,27901,27902,56713,56763</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/24138134$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://www.osti.gov/biblio/1134185$$D View this record in Osti.gov$$Hfree_for_read</backlink></links><search><creatorcontrib>Retuerto, M.</creatorcontrib><creatorcontrib>Li, M. 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. Although the samples are potential multiferroics, the dielectric measurements do not show a ferroelectric response.</description><issn>0020-1669</issn><issn>1520-510X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNo9kdtKxDAQhoMouh4ufAEJgqBgNZOmTXrhhYonqK54QO9Cks5q3W6rTVfYO1_BV_RJjO7q1Qwz38zwz0_IOrA9YBz2SycYiAwmc6QHCWdRAuxxnvQYCzmkabZElr1_YYxlsUgXyRIXECuIRY8MrpvKtNTUBb00TzV2paO5mWCLBT38-vi8LTv87d40bkhvTdXRo1k56rfFL3dl8voUH_op3c5rehDmd-lVsUOvsW3e_TCgfpUsDEzlcW0WV8j96cnd8XmU988ujg_zyHCRdZEygFJJNHwQK6uktTIVFmIrEzlg3PJUxAwUciuFQcxMqkJBOWUhLaTL4hWyOd3b-K7U3oXb7tk1dY2u0xAUg0oCtD2FXtvmbYy-06PSO6wqU2Mz9hqEyLhUCYiAbszQsR1hoV_bcmTaif57YAC2poBxXr8047YO8jQw_WOM_jcm_gaIaHsR</recordid><startdate>20131104</startdate><enddate>20131104</enddate><creator>Retuerto, M.</creator><creator>Li, M. R.</creator><creator>Ignatov, A.</creator><creator>Croft, M.</creator><creator>Ramanujachary, K. V.</creator><creator>Chi, S.</creator><creator>Hodges, J. P.</creator><creator>Dachraoui, W.</creator><creator>Hadermann, J.</creator><creator>Tran, T. Thao</creator><creator>Halasyamani, P. Shiv</creator><creator>Grams, C. P.</creator><creator>Hemberger, J.</creator><creator>Greenblatt, M.</creator><general>American Chemical Society</general><scope>NPM</scope><scope>7X8</scope><scope>OTOTI</scope></search><sort><creationdate>20131104</creationdate><title>Polar and Magnetic Layered A‑Site and Rock Salt B‑Site-Ordered NaLnFeWO6 (Ln = La, Nd) Perovskites</title><author>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.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a249t-8a1e787ea2f38b87bb764b13b757f02b2643018e2b74aee9a684308c8b16d7c93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Retuerto, M.</creatorcontrib><creatorcontrib>Li, M. 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><collection>PubMed</collection><collection>MEDLINE - Academic</collection><collection>OSTI.GOV</collection><jtitle>Inorganic chemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Retuerto, M.</au><au>Li, M. R.</au><au>Ignatov, A.</au><au>Croft, M.</au><au>Ramanujachary, K. V.</au><au>Chi, S.</au><au>Hodges, J. P.</au><au>Dachraoui, W.</au><au>Hadermann, J.</au><au>Tran, T. Thao</au><au>Halasyamani, P. Shiv</au><au>Grams, C. P.</au><au>Hemberger, J.</au><au>Greenblatt, M.</au><aucorp>Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). High Flux Isotope Reactor (HFIR)</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Polar and Magnetic Layered A‑Site and Rock Salt B‑Site-Ordered NaLnFeWO6 (Ln = La, Nd) Perovskites</atitle><jtitle>Inorganic chemistry</jtitle><addtitle>Inorg. Chem</addtitle><date>2013-11-04</date><risdate>2013</risdate><volume>52</volume><issue>21</issue><spage>12482</spage><epage>12491</epage><pages>12482-12491</pages><issn>0020-1669</issn><eissn>1520-510X</eissn><abstract>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.</abstract><cop>United States</cop><pub>American Chemical Society</pub><pmid>24138134</pmid><doi>10.1021/ic401491y</doi><tpages>10</tpages></addata></record> |
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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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