Yayın: Structure and magnetic properties of (La1-x Fe x)Fe O3(x=0, 0.25, 0.50) perovskite
| dc.contributor.author | Ünlu, C. Gökhan | |
| dc.contributor.author | Kaynar, M. Burak | |
| dc.contributor.author | Şimşek, Telem | |
| dc.contributor.author | Tekgül, Atakan | |
| dc.contributor.author | Kalkan, Bora | |
| dc.contributor.author | Özcan, Sadan | |
| dc.contributor.buuauthor | Tekgül, Atakan | |
| dc.contributor.department | Fen Edebiyat Fakültesi | |
| dc.contributor.department | Fizik Bölümü | |
| dc.contributor.orcid | 0000-0001-6737-3838 | |
| dc.contributor.researcherid | P-2124-2016 | |
| dc.date.accessioned | 2024-07-26T10:26:20Z | |
| dc.date.available | 2024-07-26T10:26:20Z | |
| dc.date.issued | 2019-05-05 | |
| dc.description.abstract | The effect of Fe doping of a LaFeO3 orthoferrite nanostructure was investigated, and the structural and magnetic properties of the resulting material were studied. The pure (La1-xFex)FeO3 (x= 0, 0.25, 0.50) nanocrystals with a minimal amount of impurities (<= 6%) were successfully produced by the sol-gel technique using La(NO2)(3) and Fe(NO2 )center dot 34H(2)O as starting materials. The phase impurities and crystalline structures were characterized through multiphase Rietveld refinement of x-ray diffraction data. The results showed that the average crystallite size of synthesized powders is similar to 18 nm. Lanthanum ions have a valence state of La3+ in the (La1-xFex)FeO3, meanwhile inducing the states of mixed character of Fe3+ and Fe4+ in Fe ions, as confirmed by X-ray photoelectron spectroscopy. Magnetometry measurements provided evidence that all the samples, including the parent LaFeO3, are weak ferromagnets; this finding is explained by distortions in the orthoferrite structure, which disturb the ideal antiferromagnetic coupling between Fe(3+ )ions. Fe substitution for La ions in the parent LaFeO3 structure leads to a significant increase in the saturation magnetization from 5.4 to 10.2 Am(2 )kg(-1), indicating that the double-exchange interaction occurs between Fe3+ and Fe4+ ions. | |
| dc.identifier.doi | 10.1016/j.jallcom.2019.01.047 | |
| dc.identifier.endpage | 1204 | |
| dc.identifier.issn | 0925-8388 | |
| dc.identifier.scopus | 2-s2.0-85060231715 | |
| dc.identifier.startpage | 1198 | |
| dc.identifier.uri | https://doi.org/10.1016/j.jallcom.2019.01.047 | |
| dc.identifier.uri | https://www.sciencedirect.com/science/article/pii/S0925838819300532 | |
| dc.identifier.uri | https://hdl.handle.net/11452/43473 | |
| dc.identifier.volume | 784 | |
| dc.identifier.wos | 000459796400122 | |
| dc.indexed.wos | WOS.SCI | |
| dc.language.iso | en | |
| dc.publisher | Elsevier | |
| dc.relation.journal | Journal of Alloys and Compounds | |
| dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi | |
| dc.rights | info:eu-repo/semantics/closedAccess | |
| dc.subject | Lafeo3 | |
| dc.subject | Nanoparticles | |
| dc.subject | Fe | |
| dc.subject | La | |
| dc.subject | Perovskite | |
| dc.subject | Nanoparticle | |
| dc.subject | Sol-gel | |
| dc.subject | Orthoferrites | |
| dc.subject | Science & technology | |
| dc.subject | Physical sciences | |
| dc.subject | Technology | |
| dc.subject | Chemistry, physical | |
| dc.subject | Materials science, multidisciplinary | |
| dc.subject | Metallurgy & metallurgical engineering | |
| dc.subject | Chemistry | |
| dc.subject | Materials science | |
| dc.title | Structure and magnetic properties of (La1-x Fe x)Fe O3(x=0, 0.25, 0.50) perovskite | |
| dc.type | Article | |
| dspace.entity.type | Publication | |
| local.contributor.department | Fen Edebiyat Fakültesi/Fizik Bölümü | |
| local.indexed.at | WOS | |
| local.indexed.at | Scopus |
