2012
DOI: 10.1016/j.matchemphys.2012.06.037
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Investigation of local structure effect and X-ray absorption characteristics (EXAFS) of Fe (Ti) K-edge on photocatalyst properties of SrTi(1−x)FexO(3−δ)

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Cited by 55 publications
(36 citation statements)
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“…The obtained result is in a good agreement with results reported in literature [48,49] according to that Fe ions in STFO have mixture of Fe 3+ (Oh) and Fe 4+ (Oh) states. It should be also noted that according to [50] the Fe ions in STFO can have a mixed Fe 2+/ Fe 3+ (Oh +Td) oxidation state.…”
Section: Iron 2p X-ray Absorptionsupporting
confidence: 92%
“…The obtained result is in a good agreement with results reported in literature [48,49] according to that Fe ions in STFO have mixture of Fe 3+ (Oh) and Fe 4+ (Oh) states. It should be also noted that according to [50] the Fe ions in STFO can have a mixed Fe 2+/ Fe 3+ (Oh +Td) oxidation state.…”
Section: Iron 2p X-ray Absorptionsupporting
confidence: 92%
“…The peaks are located at 710.2 eV (Fe 2p 3/2 ) and 723.5 eV (Fe 2p 1/2 ), which are similar to those reported in a recent study of Fe 2p corresponding to the presence of Fe 3? [29]. The second doublet was located at 713.3 eV (Fe 2p 3/2 ) and 727.2 eV (Fe 2p 1/2 ) and assigned to Fe 4?…”
Section: Xps Analysismentioning
confidence: 99%
“…Despite their technological relevance, magnetic contributions to thermal expansion behavior of divalent substituted lanthanum ferrites have not yet been reported in the open literature. Substitution of divalent cations on the trivalent lanthanum A‐site creates a charge imbalance, which requires compensation through either the formation of oxygen vacancies or an increase in the iron valence from Fe 3+ to Fe 4+ . Although it is possible for Fe 4+ to disproportionate into a mixture of Fe 3+ and Fe 5+ in orthoferrite systems, this has only been observed below 200 K .…”
Section: Introductionmentioning
confidence: 99%
“…Substitution of divalent cations on the trivalent lanthanum A-site creates a charge imbalance, which requires compensation through either the formation of oxygen vacancies or an increase in the iron valence from Fe 3+ to Fe 4+ . 12,13 Although it is possible for Fe 4+ to disproportionate into a mixture of Fe 3+ and Fe 5+ in orthoferrite systems, this has only been observed below 200 K. 14,15 In addition to electronic and chemical changes, the different ionic radii of cation substitutions will affect the local structure of the material. Previous studies have reported that divalent, cation substitutions in LSF and LCF cause a reduction in the N eel temperatures, to~390°C for 10% Sr doped 4,16 and 350°C-400°C for 20% Ca doped.…”
Section: Introductionmentioning
confidence: 99%