2019
DOI: 10.1557/jmr.2019.143
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Enthalpy increments and redox thermodynamics of SrFeO3−δ

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Cited by 11 publications
(16 citation statements)
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“…This is the main reason why among RBaCo 2 O 6−δ double perovskites (R = Pr, Eu, Sm, or Gd) PrBaCo 2 O 6−δ , having a generally lower oxygen storage capacity (OSC), possesses a higher Δ H total ◦ , and also why SrFeO 3−δ with a greater specific heat capacity is an ≈20–30% more “capacious” energy storage material than RBaCo 2 O 6−δ (R = Pr, Eu, Sm, or Gd). The equilibrium OSC of strontium ferrite SrFeO 3−δ is higher than that of RBaCo 2 O 6−δ (R = Pr, Eu, Sm, or Gd), as shown in the inset of Figure , making Δ H red ◦ of SrFeO 3−δ greater despite the slightly lower (by absolute value) partial molar enthalpy of O 2 in this oxide. , …”
Section: Resultsmentioning
confidence: 92%
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“…This is the main reason why among RBaCo 2 O 6−δ double perovskites (R = Pr, Eu, Sm, or Gd) PrBaCo 2 O 6−δ , having a generally lower oxygen storage capacity (OSC), possesses a higher Δ H total ◦ , and also why SrFeO 3−δ with a greater specific heat capacity is an ≈20–30% more “capacious” energy storage material than RBaCo 2 O 6−δ (R = Pr, Eu, Sm, or Gd). The equilibrium OSC of strontium ferrite SrFeO 3−δ is higher than that of RBaCo 2 O 6−δ (R = Pr, Eu, Sm, or Gd), as shown in the inset of Figure , making Δ H red ◦ of SrFeO 3−δ greater despite the slightly lower (by absolute value) partial molar enthalpy of O 2 in this oxide. , …”
Section: Resultsmentioning
confidence: 92%
“…In the notation employed in this work, the enthalpy increments are denoted as Δ 298 T H °( T ), which corresponds to the enthalpy required to heat 1 mol of sample from 298.15 K to T and is equal to ∫ 298 T C p d T . The shape of Δ 298 T H °( T ) experimental dependences is typical of the oxides that are reduced upon being heated: the higher-temperature upward deviation from the near linear low-temperature trend is due to the additional contribution from the oxygen loss. ,,, In other words, the Δ 298 T H °( T ) values were actually measured for the RBaCo 2 O 6−δ (R = Eu or Sm) samples of variable oxygen content. To recalculate them for constant-composition samples, EuBaCo 2 O 5.56 and SmBaCo 2 O 5.6 , the following equation was used: where δ 0 = 0.44 for EuBaCo 2 O 5.56 and δ 0 = 0.40 for SmBaCo 2 O 5.6 and δ 1 is the nonstoichiometry of the sample at temperature T in air.…”
Section: Resultsmentioning
confidence: 98%
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