Magnetic properties of Sr0.5Ba0.5HoxFe12-xO19 (x ? 0.10) nanohexaferrites

dc.authorid0000-0002-7453-0210
dc.authorid0000-0002-3367-2263
dc.authorid0000-0003-1651-3591
dc.authorid0000-0003-3105-0425
dc.authorid0000-0002-3102-7201
dc.contributor.authorCaliskan, S.
dc.contributor.authorAlmessiere, M. A.
dc.contributor.authorBaykal, A.
dc.contributor.authorSlimani, Y.
dc.contributor.authorGüngüneş, H.
dc.contributor.authorKorkmaz, A. Demir
dc.contributor.authorUl-Hamid, A.
dc.date.accessioned2025-05-10T19:54:23Z
dc.date.issued2023
dc.departmentİstanbul Medeniyet Üniversitesi
dc.description.abstractThe Ho3+ ion-substituted SrBa nanohexaferrites, Sr0.5Ba0.5Fe12-xHoxO19 (x & LE; 0.1) (Ho & RARR; SrBa NHFs), were fabricated via ultrasonic-assisted sol-gel route. The hexagonal structure and plate-like morphology were confirmed by X-ray powder pattern (XRD), transmittance electron microscope (TEM), scanning electron microscope (SEM), and high-resolution transmittance electron microscope (HR-TEM). It has been found out that the crystallite size (D-XRD) was within 45-74 nm range. Both elemental mapping and energy-dispersive X-ray spectroscopy (EDX) analyses provided the purity and expected chemical composition of the products. Using the M-H hysteresis loops (at 300 and 10 K), magnetic properties of Ho & RARR; SrBa NHFs are analyzed. Upon a sudden fall at x = 0.02, as soon as Ho ions are added, the magnetization is improved with the Ho substitution and prominently enhanced with decreasing temperature. However, the coercivity H-c is decreased with the Ho substitution. The Ho-doped samples represent a magnetically soft material at both high and low temperatures, which is also confirmed through M-T measurements. Their squareness ratio is found to be less than 0.5, suggesting the generation of multi-magnetic domains. The unsubstituted HFs and the samples with x = 0.02 and 0.06 show usual M-T variations with typical field-cooling (FC) and zero-field-cooling (ZFC) branches. However, the other samples (with x = 0.04, 0.08, and 0.10) exhibit unusual behavior with anomalies in their M-T plots. From Fe-57 Mossbauer spectroscopy data, the variation in line width, isomer shift, quadrupole splitting, and hyperfine magnetic field values on Ho3+ substitution have been determined. Mossbauer spectra show that Ho3+ ions located at generally octahedral 12 k site. The s-electron density of around Fe3+ ions has not influenced doped content.
dc.identifier.doi10.1007/s00339-023-06881-x
dc.identifier.issn0947-8396
dc.identifier.issn1432-0630
dc.identifier.issue9
dc.identifier.scopus2-s2.0-85168310499
dc.identifier.scopusqualityQ2
dc.identifier.urihttps://doi.org/10.1007/s00339-023-06881-x
dc.identifier.urihttps://hdl.handle.net/20.500.14730/13035
dc.identifier.volume129
dc.identifier.wosWOS:001048598800002
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSpringer Heidelberg
dc.relation.ispartofApplied Physics A-Materials Science & Processing
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WOS_20250302
dc.subjectHexaferrites
dc.subjectMagnetic features
dc.subjectZFC
dc.subjectFC magnetization
dc.subjectUltrasonic-assisted sol-gel approach synthesis
dc.subjectMossbauer study
dc.titleMagnetic properties of Sr0.5Ba0.5HoxFe12-xO19 (x ? 0.10) nanohexaferrites
dc.typeArticle

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