首页> 外文会议>Conference on nonstoichiometric compounds >OXYGEN NONSTOICHIOMETRY AND THERMODYNAMIC QUANTITIES OF PEROVSKITE-TYPE La_(1-x)Sr_xFeO_(3-δ) (x=0.2, 0.5, 0.8)
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OXYGEN NONSTOICHIOMETRY AND THERMODYNAMIC QUANTITIES OF PEROVSKITE-TYPE La_(1-x)Sr_xFeO_(3-δ) (x=0.2, 0.5, 0.8)

机译:钙钛矿型La_(1-x)Sr_xFeO_(3-δ)的氧非化学计量和热力学量(x = 0.2,0.5,0.8)

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In this work, the defect structure analysis of La_(1-x)Sr_xFeO_(3-δ) (x=0.2, 0.5, 0.8) was presented. Thermogravimetric measurements were performed to determine the change in oxygen nonstoichiometry (Δδ) with oxygen partial pressure (pO_2) in 10~(-19) ≤ (pO_2/atm) ≤ 0.21 and temperature in 750 ≤ (T/℃) < 900 range. La_(1-x)Sr_xFeO_(3-δ) showed a clear electronic stoichiometric point around δ≈3-x/2. The relative partial molar enthalpy (h_o-h_o~o) and entropy (s_o-S_o~o) of oxygen were calculated from δ-pO_2-T relation by using Gibbs-Helmholtz equation. The negative sign of h_o-h_o~o and s_o-s_o~o indicated that the incorporation of oxygen was an exothermic process and showed that the experimentally observed variations in h_o-h_o~o and s_o-s_o~o with δ matched well with the statistical thermodynamic model proposed by Mizusaki. The defect diagram analysis showed that in n-type regime Fe~(2+) concentration varied with (pO_2)~(-1/4) whereas in p-type regime Fe~(4+) concentration varied with (pO_2)~(1/4).
机译:在这项工作中,提出了La_(1-x)Sr_xFeO_(3-δ)(x = 0.2,0.5,0.8)的缺陷结构分析。进行热重法测定,确定氧的非化学计量比(Δδ),其中氧分压(pO_2)在10〜(-19)≤(pO_2 / atm)≤0.21,温度在750≤(T /℃)<900范围内。 La_(1-x)Sr_xFeO_(3-δ)在δ≈3-x/ 2附近显示出清晰的电子化学计量点。利用Gibbs-Helmholtz方程,由δ-pO_2-T关系式计算出氧的相对部分摩尔焓(h_o-h_o〜o)和熵(s_o-S_o〜o)。 h_o-h_o〜o和s_o-s_o〜o的负号表明氧的掺入是一个放热过程,表明实验观察到的δ的h_o-h_o_o和s_o-s_o〜o的变化与氧的变化非常吻合。 Mizusaki提出的统计热力学模型。缺陷图分析表明,在n型态,Fe〜(2+)的浓度随(pO_2)〜(-1/4)变化,而在p型态,Fe〜(4+)的浓度随(pO_2)〜(-O)变化。 1/4)。

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