2016
DOI: 10.1063/1.4961607
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Kinetics and intermediate phases in epitaxial growth of Fe3O4 films from deposition and thermal reduction

Abstract: We have studied the growth of Fe3O4 (111) epitaxial films on Al2O3 (001) substrates using a pulsed laser deposition / thermal reduction cycle using an α-Fe2O3 target. While direct deposition onto the Al2O3 (001) substrates results in an α-Fe2O3 epilayer, deposition on the Fe3O4 (111) surface results in a -Fe2O3 epilayer. The kinetics of the transitions between Fe2O3 and Fe3O4 were studied by measuring the time constants of the transitions. The transition from α-Fe2O3 to Fe3O4 via thermal reduction turns out t… Show more

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Cited by 24 publications
(19 citation statements)
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“…The formation of hematite is related to the atmospheres used in the heat treatment in this research. Hong et al [44] and Zhang et al [66] described that iron-based materials oxidized at temperatures between 377 • C and 527 • C under steam, and mainly with CO 2 atmospheres, producing negative free energy for the formation of hematite; therefore, under these conditions, part of the magnetite exposed to higher concentrations of oxygen (outermost layers) is oxidized to hematite (Fe 3 O 4 → α-Fe 2 O 3 ) [56,62,66]. Genuzio et al [62] also mentioned that the kinetics of this transformation are very fast and that it depends on the chemical composition and the availability of defects in the crystalline network, which allow for the growth of the new phase through specific crystallographic plans.…”
Section: Discussionmentioning
confidence: 99%
“…The formation of hematite is related to the atmospheres used in the heat treatment in this research. Hong et al [44] and Zhang et al [66] described that iron-based materials oxidized at temperatures between 377 • C and 527 • C under steam, and mainly with CO 2 atmospheres, producing negative free energy for the formation of hematite; therefore, under these conditions, part of the magnetite exposed to higher concentrations of oxygen (outermost layers) is oxidized to hematite (Fe 3 O 4 → α-Fe 2 O 3 ) [56,62,66]. Genuzio et al [62] also mentioned that the kinetics of this transformation are very fast and that it depends on the chemical composition and the availability of defects in the crystalline network, which allow for the growth of the new phase through specific crystallographic plans.…”
Section: Discussionmentioning
confidence: 99%
“…The in-plane epitaxial relation can be extracted from the RHEED pattern, as depicted in Fig. 2b, with a 30° rotation between the in-plane reciprocal unit cell of CFO relative to that of sapphire substrate, which is the same as that of the Fe3O4/Al2O3 films [19]. Time-resolved RHEED was carried out to elucidate the depth profile of the film by in-situ monitoring the top layer of the film during the growth [19].…”
Section: Structural Characterization and Evidence Of Interfacial Reco...mentioning
confidence: 99%
“…2b, with a 30° rotation between the in-plane reciprocal unit cell of CFO relative to that of sapphire substrate, which is the same as that of the Fe3O4/Al2O3 films [19]. Time-resolved RHEED was carried out to elucidate the depth profile of the film by in-situ monitoring the top layer of the film during the growth [19]. RHEED images along the [11 ̅ 00] direction of CFO was taken every 30 seconds during the film growth at a repetition rate of 1 Hz.…”
Section: Structural Characterization and Evidence Of Interfacial Reco...mentioning
confidence: 99%
“…Furthermore, hematite phase is formed due to the atmospheres used during aging process. Zhang et al [41] and Hong et al [42] described that during oxidation between 375 and 526 • C in atmospheres containing water vapor, the outermost layers are exposed to a higher concentration of oxygen, and part of the magnetite oxidizes to hematite (Fe 3 O 4 → α-Fe 2 O 3 ) [40][41][42][43].…”
Section: Eds Quantitative Analysis From Pointsmentioning
confidence: 99%