1998
DOI: 10.1006/jssc.1997.7737
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Raman Spectra and Vibrational Analysis of BaFe12O19Hexagonal Ferrite

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Cited by 346 publications
(154 citation statements)
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“…As for magnetite and nickel ferrite, the structure would correspond to an inverse spinel, having half of the Fe 3C ions in the tetrahedral sites. 19 concluded that the A1g band in the 670-720 cm 1 spectral range of the inverse spinels may be assigned to a vibrational mode of FeO 4 tetrahedra, in good agreement with other authors. 20,21 This band, indeed, seems to occur irrespective of the chemical nature of the bivalent cation.…”
Section: Analysis Of the 5 Nm Thick Fe 3 O 4 Filmsupporting
confidence: 77%
“…As for magnetite and nickel ferrite, the structure would correspond to an inverse spinel, having half of the Fe 3C ions in the tetrahedral sites. 19 concluded that the A1g band in the 670-720 cm 1 spectral range of the inverse spinels may be assigned to a vibrational mode of FeO 4 tetrahedra, in good agreement with other authors. 20,21 This band, indeed, seems to occur irrespective of the chemical nature of the bivalent cation.…”
Section: Analysis Of the 5 Nm Thick Fe 3 O 4 Filmsupporting
confidence: 77%
“…According to the literature, both Raman modes at 612 and 682 cm -1 are reflecting the local lattice effect in the tetrahedral sublattice, while the peak at 468 cm -1 is probing the local lattice effect in the octahedral sublattice. 39,40 The same Raman bands mentioned above as well as additional bands at 222 cm -1 and 286 cm -1 can be seen in samples ZC31/4 to ZC11/8; these additional bands can be assigned to α-Fe 2 O 3 , which has very intense bands at these positions, shown in the Figure 3 for convenience. The Raman data thus confirm the observed significant difference between sample ZC13/8 and samples ZC31/4 to ZC11/8 by Mossbauer spectroscopy, i.e.…”
Section: 2 Phase Composition and Crystal Structure Of Ternary MIXsupporting
confidence: 66%
“…Wide peaks at around 190, 350, 500 and 700 cm -1 are characteristic for maghemite (circles), while narrow peaks at 225, 247, 299, 412, 498 and 613 cm -1 belong to hematite (diamonds). Popup and a evanescent narrow peak at 690 cm -1 may be assigned to a bipyramidal FeO 5 [12]. The presence of maghemite is not surprising since fine powdered magnetite easily undergoes oxidation, which may be induced by laser radiation during the measurement or due to calcination of potassium doped materials [13].…”
Section: Resultsmentioning
confidence: 99%