2017
DOI: 10.1016/j.jcrysgro.2017.05.034
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Growth of YbFe2O4 single crystals exhibiting long-range charge order via the optical floating zone method

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Cited by 9 publications
(14 citation statements)
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“…[9,11,13,14] The ferrimagnetic transition due to the ordering of the Fe 2+ and Fe 3+ moments occurs around 240 K in this family. Similarly, the Fe 2+ -Fe 3+ charge-ordered state has been reported in LuFe 2 O 4 [15,16,17] and in YbFe 2 O 4 [18,19,20]. Such charge ordering is believed to break the space-inversion symmetry, leading to macroscopic ferroelectric polarization.…”
Section: Introductionmentioning
confidence: 65%
“…[9,11,13,14] The ferrimagnetic transition due to the ordering of the Fe 2+ and Fe 3+ moments occurs around 240 K in this family. Similarly, the Fe 2+ -Fe 3+ charge-ordered state has been reported in LuFe 2 O 4 [15,16,17] and in YbFe 2 O 4 [18,19,20]. Such charge ordering is believed to break the space-inversion symmetry, leading to macroscopic ferroelectric polarization.…”
Section: Introductionmentioning
confidence: 65%
“…At low temperature, the spins of Yb 3+ ions could play a significant role in the magnetic state of the system. In particular, the interactions of the Yb 3+ (4f 13 ) spins with the Fe spins could lead to a complicated spin structure at low temperatures. We interpret that the reversal of the moment below 65 K is due to the emergence of the spins of Yb 3+ ions.…”
Section: Resultsmentioning
confidence: 99%
“…It is possible that the observed temperature dependence of the M-H hysteresis loops below 65 K could be attributed to a spin-glass state due to the competition between ferromagnetic and antiferromagnetic interactions of Yb and Fe sub-lattices. There have been reports of a spin-glass state in YbFO below 80 K. 10,12,13 The one caveat is that the highest magnetic field was 8 T, which was not sufficient to drive the full saturation of magnetization in the sample and thus, the coercive field (H * c ) value at each temperature (Fig. 2(d)) does not represent its true value and its temperature dependence only represents a qualitative feature.…”
Section: Resultsmentioning
confidence: 99%
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“…In particular, LuFe 2 O 4 was considered a clear example of ferroelectricity from charge ordering (CO) of Fe 2+ and Fe 3+ in the Fe-O bilayers [1], though recently this was contradicted [2,3,4,5]. Rare earth substitutions tune the relevant interactions within the Fe-O bilayers [6] resulting in a similar CO for R = Yb, which has almost the same ion size as Lu [7,8] but a dramatically different CO for the larger Y [9,10]. Another way to tune the CO is to focus on the interactions between different bilayers.…”
Section: Introductionmentioning
confidence: 99%