2008
DOI: 10.1016/j.jmmm.2008.02.034
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Application of FORC distributions to the study of magnetic interactions in ferrites of composition

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Cited by 22 publications
(11 citation statements)
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“…In a work by other authors [12], where Ba hexaferrite with La-Co substitution is studied, a stoichiomet- ric sample with La-Co substitution is compared to one with La excess (which implies an iron deficiency). They observe a very high coercivity of 6700 Oe for the iron-deficient sample and explain this considering that La excess both raises the anisotropy field and decouples the particles.…”
Section: Resultsmentioning
confidence: 99%
“…In a work by other authors [12], where Ba hexaferrite with La-Co substitution is studied, a stoichiomet- ric sample with La-Co substitution is compared to one with La excess (which implies an iron deficiency). They observe a very high coercivity of 6700 Oe for the iron-deficient sample and explain this considering that La excess both raises the anisotropy field and decouples the particles.…”
Section: Resultsmentioning
confidence: 99%
“…In a work by other authors [12], where Ba hexaferrite with La-Co substitution is studied, a stoichiometric sample with La-Co substitution is compared to one with La excess (which implies an iron deficiency). They observe a very high coercivity of 84.20 A/m for the iron-deficient sample and explain this considering that La excess both raises the anisotropy field and decouples particles.…”
Section: Article In Pressmentioning
confidence: 99%
“…In M-type hexaferrites, the 24 iron atoms of a unit cell occupy five different crystallographic sites: three octahedral sites, crystallographically known as 2a, 12k and 4f2, one tetrahedral site (4f1) and one bipyramidal site (2b). In the magnetically ordered state in BaFe 12 O 19 or SrFe 12 O 19 , the 12k, 2a and 2b sites have their spins aligned parallel to each other and to the crystallographic c-axis, whereas those of 4f2 and 4f1 point in the opposite direction.…”
Section: Introductionmentioning
confidence: 99%
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“…In these studies, the magnetic properties of ferrites were changed by substituting Fe 3 + with other cations. The magnetic properties of ferrites can also be changed by substituting Ba 2 + (or Sr 2 + ) with La 3 + (or Pr 3 + , Gd 3 + ), [17][18][19][20], which alters the Fe 3 + -O-Fe 3 + super-exchange interaction, or along with lanthanide-doping, substituting Fe 3 + with ions such as Zn 2 + [21-23] Sn 4 + , Mn 2 + [24], and Co 2 + [25][26][27]. Mn 2 + was adopted as a dopant because it has the same number of unpaired electrons as Fe 3 + and would therefore provide a useful comparison to our previous work [16].…”
Section: Introductionmentioning
confidence: 99%