1939
DOI: 10.1038/144327b0
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Electronic Conduction of Magnetite (Fe3O4) and its Transition Point at Low Temperatures

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Cited by 1,672 publications
(1,205 citation statements)
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“…At lower temperatures, the magnetic hystereses widen, an approximate doubling in coercive field being usually observed between 300 and 5 K ( Figure S2). Temperaturedependent magnetization data ( Figure S4) do not show any abrupt change indicative of a crystallographic phase transition (Verwey transition), 12 an observation consistent with a glassy structural state.…”
mentioning
confidence: 76%
“…At lower temperatures, the magnetic hystereses widen, an approximate doubling in coercive field being usually observed between 300 and 5 K ( Figure S2). Temperaturedependent magnetization data ( Figure S4) do not show any abrupt change indicative of a crystallographic phase transition (Verwey transition), 12 an observation consistent with a glassy structural state.…”
mentioning
confidence: 76%
“…The Verwey transition in magnetite, which is a first-order crystallographic phase transition, has been studied extensively since its discovery (Verwey, 1939) because of its enormous impact on the magnetic and other physical properties of the material (Walz, 2001). The Verwey transition is associated with an order-of-magnitude increase in magnetocrystalline anisotropy and a change in magnetic easy axis from cubic <111> to monoclinic [001] below ~120 K. Although numerous studies have suggested that magnetic domain walls in magnetite can interact with the ferroelastic twin walls that form at low temperature (e.g., Smirnov & Tarduno, 2002), no direct evidence for such interactions has previously been presented.…”
Section: Low-temperature Magnetic Propertiesmentioning
confidence: 99%
“…Magnetite also undergoes another Verwey transition at T V ~ 120 K, where the charge ordering between Fe 2+ and Fe 3+ has been observed below T V [14].…”
Section: Introductionmentioning
confidence: 99%