2017
DOI: 10.1016/j.ssi.2017.06.014
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Redox thermodynamics and phase composition in the system SrFeO3δ — SrMnO3δ

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Cited by 61 publications
(51 citation statements)
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“…B-site substitution only increased the redox capacity for B’ = Co, and the redox capacities for B’ = Cr, Cu, and Mn were significantly reduced. The B’ = Mn and Cu redox capacities were consistent with previously published literature [ 26 , 27 ]. The results showed no significant dependence with x or y on the redox capacity except for B’ = Cr, which reduced the overall Δ m / m initial from 1.78% (Δδ = 0.21) to 1.37% (Δδ = 0.16) as y increased from 0.10 to 0.20.…”
Section: Resultssupporting
confidence: 91%
“…B-site substitution only increased the redox capacity for B’ = Co, and the redox capacities for B’ = Cr, Cu, and Mn were significantly reduced. The B’ = Mn and Cu redox capacities were consistent with previously published literature [ 26 , 27 ]. The results showed no significant dependence with x or y on the redox capacity except for B’ = Cr, which reduced the overall Δ m / m initial from 1.78% (Δδ = 0.21) to 1.37% (Δδ = 0.16) as y increased from 0.10 to 0.20.…”
Section: Resultssupporting
confidence: 91%
“…By oxygen partial pressure swing between air and helium at 600 • C,~1 wt% oxygen capacity was achieved for oxygen production [39]. Recently, SrFeO 3 based oxygen sorbents have received many research interests, owing to its large oxygen capacity and low operating temperature [40][41][42]. The versatile structure of SrFeO 3 offers many opportunities to introduce dopants at A and/or B site to further tuning the redox property [43][44][45].…”
Section: Introductionmentioning
confidence: 99%
“…Perovskites of the general composition A 2 + M 3/4 + O 3-δ with δ = 0-0.5 constitute stable phases for many different alkali earth metals A and transition metals M. The large variety of possible phases can be even extended by solid solution formation, as many of these perovskites form stable mixed phases in a large range of mixture ratios. [7] SrFeO 3-δ is a simple, grossly non-stoichiometric perovskite oxide, which is well known for its oxygen non-stoichiometry and mixed + III/ + IV Fe valence, which makes it a suitable oxygen carrier for thermochemical air separation. [8] To a small extent, iron cations in this phase can be exchanged by copper cations, forming solid solutions, i. e. SrFe 0.95 Cu 0.05 O 3-δ , as demonstrated previously by the authors.…”
Section: Introductionmentioning
confidence: 99%