2019
DOI: 10.1016/j.solidstatesciences.2019.105932
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Solventless synthesis and characterization of α-Fe, γ-Fe, magnetite and hematite using iron(III)citrate

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Cited by 7 publications
(9 citation statements)
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“…On the other hand, in case of FA2, the sextet S1 can be assigned to iron in magnetite, whereas the sextet S2 represents iron in hematite phase [16,18,41]. The population ratio of these two sites is ~ 2:3.…”
Section: Mössbauer Studymentioning
confidence: 99%
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“…On the other hand, in case of FA2, the sextet S1 can be assigned to iron in magnetite, whereas the sextet S2 represents iron in hematite phase [16,18,41]. The population ratio of these two sites is ~ 2:3.…”
Section: Mössbauer Studymentioning
confidence: 99%
“…In magnetite at ~ 123 K, a charge-ordering transition (Verwey transition) occurs when an ordering of Fe 3+ and Fe 2+ ions within the octahedral sites occurs and a drop in magnetization at the transition temperature is the signature of magnetite [13,14]. On the other hand, at ~ 263 K, hematite exhibits a weak ferromagnetic to antiferromagnetic transition (Morin transition) owing to rearrangement of spins to antiparallel fashion along the rhombohedral (111) axis from a canted spin arrangement with respect to the basal (111) plane [15][16][17]. These magnetic phases of iron oxide along with subphases are very accurately detected by the application of Mӧssbauer spectroscopy [16,18].…”
Section: Introductionmentioning
confidence: 99%
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