2012
DOI: 10.1016/j.talanta.2012.03.001
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A new method for the identification and quantification of magnetite–maghemite mixture using conventional X-ray diffraction technique

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Cited by 312 publications
(158 citation statements)
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“…This selected sample presents the best yield of functionalization. Crystallographic peaks and Miller indices found in the sample, which are reported in literature (Kim et al, 2012), were 21.4 ° (111), 35.2 ° (220), 41.6 ° (311), 50.7 ° (400) 63.2 ° (422), 67.5 ° (511) and 74.4 ° (440). These data are related to the cubic crystal system Fd-3m (227) space group that represents the characteristics of the unit cell of magnetite spinel, showing that the nanoparticles synthesized in this study are Fe3O4.…”
Section: Functionalization Methods and Biocatalyst Selectionsupporting
confidence: 74%
“…This selected sample presents the best yield of functionalization. Crystallographic peaks and Miller indices found in the sample, which are reported in literature (Kim et al, 2012), were 21.4 ° (111), 35.2 ° (220), 41.6 ° (311), 50.7 ° (400) 63.2 ° (422), 67.5 ° (511) and 74.4 ° (440). These data are related to the cubic crystal system Fd-3m (227) space group that represents the characteristics of the unit cell of magnetite spinel, showing that the nanoparticles synthesized in this study are Fe3O4.…”
Section: Functionalization Methods and Biocatalyst Selectionsupporting
confidence: 74%
“…An indirect indication can be obtained from the shape of the high-angle peaks (5 1 1) and (4 4 0). It has been shown by Kim et al [47] that these peaks are doublets in case of mixture of magnetite (Fe 3 O 4 ) and maghemite ( -Fe 2 O 3 ) phases; for example, the maximum of the (5 1 1) mixture, the intensity of each of these peaks varies, depending on the concentration of the corresponding oxide. The experimental data of each of the (5 1 1) and (4 0 0) peaks in Figure 5 were successfully fitted with a single symmetric peak with maximum at 57.3 ∘ and 62.8 ∘ , respectively, which is an indirect indication for formation of -Fe 2 O 3 attached to the CNF during the synthesis.…”
Section: Resultsmentioning
confidence: 99%
“…79196) with a lattice parameter of 8.349 Å. As it was mentioned in previous studies on identification and quantification of magnetite-maghemite mixture using conventional X-ray diffraction technique carried out by W. Kim et al [29], the magnetite and maghemite phases are difficult to differentiate when they coexist because they are very close. The lattice parameter calculated from the pattern play an important role in the establishment the magnetite or maghemite phase.…”
Section: Discussionmentioning
confidence: 99%