2012
DOI: 10.1016/j.jmmm.2011.11.008
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Domain wall structure of weak ferromagnets according to Raman

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Cited by 12 publications
(4 citation statements)
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“…The band assigned at 1302 cm −1 is due to the vibration of magnetic Fe 3+ ions, which are in good agreement with the literature‐reported YFO samples. [ 6,25 ] Here the assigned Raman modes are well reliable with previous literature reported on YFO orthorhombic structure [ 7,32 ]…”
Section: Resultssupporting
confidence: 88%
See 1 more Smart Citation
“…The band assigned at 1302 cm −1 is due to the vibration of magnetic Fe 3+ ions, which are in good agreement with the literature‐reported YFO samples. [ 6,25 ] Here the assigned Raman modes are well reliable with previous literature reported on YFO orthorhombic structure [ 7,32 ]…”
Section: Resultssupporting
confidence: 88%
“…The band assigned at 1302 cm À1 is due to the vibration of magnetic Fe 3þ ions, which are in good agreement with the literature-reported YFO samples. [6,25] Here the assigned Raman modes are well reliable with previous literature reported on YFO orthorhombic structure [7,32] Figure 6 displays the XRD pattern of YFO powder samples with different crystallite sizes. These patterns confirm the existence of a single-phase nature without any impurity phases (pyrochlore phase).…”
Section: Resultssupporting
confidence: 87%
“…Apart from these bands, the vibration of magnetic Fe 3+ ion was also observed at ∼1300 cm −1 , and this band is good agreement with earlier reported of YFO sample. 8,9,40,41 Figure 4 shows the room temperature magnetization hysteresis (M-H) loops of YFO, YFO125, YFO25 and YFO50 with an applied field up to 1.5 T. The magnetic characteristics, such as coercivity (H c ), magnetization (M s ), and remnant magnetization (M r ), have been determined separately for each sample using the appropriate M-H loop. The M-H hysteresis data from −0.1 kOe to + 0.1 kOe was inserted in their respective graphs for clear visibility of Mr and Hc points.…”
Section: Resultsmentioning
confidence: 99%
“…The peaks at 217, 610, and 1062 cm −1 can be attributed to Fe 2 O 3 , whereas the peaks at 276 and 326 cm −1 can be explained by the octahedral oxygen environment of the magnetic ions of Fe 3+ . 23,27) The peak at 1346 cm −1 , which was equally close to both cubic YIG and YFeO 3 (Fe 2 O 3 ), can be assigned to impurities. The present Raman spectra differed from those for amorphous garnets.…”
Section: Single-crystal Samplesmentioning
confidence: 99%