2017
DOI: 10.1107/s2052520616017935
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Deformations of the α-Fe2O3 rhombohedral lattice across the Néel temperature

Abstract: High-resolution synchrotron radiation powder diffraction patterns of -Fe 2 O 3 measured between room temperature and 1100 K, i.e. above the Né el temperature T N = 950 K, have been analyzed. The integral breadths of the Bragg peaks show a hkl-dependent anisotropy, both below and above T N . This anisotropy can be quantitatively described by using a statistical peakbroadening model [Stephens (1999). J. Appl. Cryst. 32, 281]. Model calculations show that the rhombohedral -Fe 2 O 3 lattice is deformed and the def… Show more

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Cited by 10 publications
(6 citation statements)
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“…Therefore, the ZFC-FC relations plotted in Figure 7(c) present an irreversible process of magnetizing such a system, which can be treated as a bulk magnet. Nonetheless, it should be noted that a kink in the ZFC curve between 250 K and 260 K denotes the Morin transition usually observed in hematite at T∼260 K, [67,68] which confirms the presence of this phase in the annealed NFO sample. Figure 7(d) presents ZFC-FC curves for the annealed NFO@SiO 2 sample measured at 100 and 1000 Oe.…”
Section: Fc-zfc Magnetizationsupporting
confidence: 61%
“…Therefore, the ZFC-FC relations plotted in Figure 7(c) present an irreversible process of magnetizing such a system, which can be treated as a bulk magnet. Nonetheless, it should be noted that a kink in the ZFC curve between 250 K and 260 K denotes the Morin transition usually observed in hematite at T∼260 K, [67,68] which confirms the presence of this phase in the annealed NFO sample. Figure 7(d) presents ZFC-FC curves for the annealed NFO@SiO 2 sample measured at 100 and 1000 Oe.…”
Section: Fc-zfc Magnetizationsupporting
confidence: 61%
“…The further calcination at higher temperatures (500 • C) resulted in nearly pure hematite. Thus, the diffraction peaks were attributed to 96.9, 100, and 98.7% of the polycrystalline structure of hematite for the calcination times 2, 4, and 5 h, respectively (Figure 1b and Table 2) [46,51,56,62,64].…”
Section: Xrdmentioning
confidence: 98%
“…On the other hand, the increase in calcination temperature caused a pronounced change in the Fe x O y -NP type, which resulted in a greater proportion of hematite. For example, the diffraction peaks of GS-NPs calcined at 300 • C for 2, 4, and 5 h were attributed to 55.0, 57.1, and 86.6% of polycrystalline hematite, respectively (Table 2) [46,47,50,51,53,54], while the diffraction peaks of the GS-NPs calcined at 500 • C for 2, 4 and 5 h were assigned to 25.4, 91.3, and 62.4% of monoclinic, cubic, and trigonal with hexagonal axis hematite [46,47,[49][50][51][52][55][56][57][58][59][60].…”
Section: Xrdmentioning
confidence: 99%
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“…Additional peaks at 2θ values of 45.55 and 59.29° were assigned to monoclinic magnetite, corresponding to the crystallographic planes (030) and (049), respectively. The peaks at 21.08, 23.48, 39.33, 40.04, and 54.47° were attributed to monoclinic hematite, with the crystallographic planes (11-1), (20-2), (40-6), (021), and (512), respectively, and the space group C 1 2/c 1 (15) according to the JCPDS card number 00-210-8028 [ 67 ].…”
Section: Resultsmentioning
confidence: 99%