Unusually large oxygen non-stoichiometry and defect thermodynamics in Sr4Mn2–xFe1+xO10–δ Ruddlesden-Popper layered oxides

IF 9.3 1区 材料科学 Q1 MATERIALS SCIENCE, MULTIDISCIPLINARY Acta Materialia Pub Date : 2024-12-20 DOI:10.1016/j.actamat.2024.120675
I.S. Grobovoy, A.Yu. Suntsov, V.L. Kozhevnikov
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Abstract

The Ruddlesden-Popper oxides Sr4Mn2–xFe1+xO10–δ (x = 0, 0.5, and 1.0) with the layered tetragonal structure (SG I4/mmm) were synthesized at the heating of organometallic precursors to 1400 °C in air. The Rietveld refinement of the X-ray diffraction patterns indicates a disordered arrangement of Mn and Fe atoms in the crystal. The results of the electron density functional-based calculations of the total energy show noticeably larger oxygen vacancy formation enthalpy for OO2 positions in the structural rock salt layers of strontium oxide compared to the apical OO1 and equatorial OO3 and OO4 positions in perovskite slabs. The coulometric titration measurements show that the Sr4Mn2–xFe1+xO10–δ phases can endure harsh reducing conditions, staying stable even when up to two oxygen atoms are taken away from the structure. Simulations of equilibrium oxygen content data reveal that oxygen exchange is coupled with electron excitation processes involving d-cations and intrinsic anion disorder. It is suggested that this disorder may be caused by unequal vacancy formation energies at crystallographically different oxygen sites. The enthalpy and entropy changes in the defect formation reactions were derived from the fitting of the experimental plots for oxygen non-stoichiometry. The obtained thermodynamic parameters were applied to determine how the concentrations of electronic and ionic defects depend on variations in temperature and partial pressure of oxygen. The consistency of the thermodynamic analysis is supported by a good coincidence of the calculated and experimental plots of the partial thermodynamic functions of labile oxygen in Sr4Mn2xFe1+xO10–δ.

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Sr4Mn2-xFe1 +xO10 -δ Ruddlesden-Popper层状氧化物异常大的氧非化学计量学和缺陷热力学
将有机金属前驱体在空气中加热至1400℃,合成了具有层状四方结构(sgi4 /mmm)的rudlesdun - popper氧化物Sr4Mn2-xFe1 +xO10 -δ (x = 0,0.5和1.0)。x射线衍射图的Rietveld细化表明Mn和Fe原子在晶体中的无序排列。基于电子密度泛函的总能计算结果表明,与钙钛矿板的顶端OO1和赤道OO3、OO4位置相比,氧化锶结构岩盐层中OO2位置的氧空位形成焓明显更大。库仑滴定测量表明,Sr4Mn2-xFe1 +xO10 -δ相可以承受苛刻的还原条件,即使从结构中带走两个氧原子也能保持稳定。平衡氧含量数据的模拟表明,氧交换与电子激发过程耦合,涉及d-阳离子和本征阴离子紊乱。这可能是由于不同氧位上的空位形成能不等造成的。通过对氧非化学计量图的拟合,得到了缺陷形成反应的焓和熵的变化。得到的热力学参数被应用于确定电子和离子缺陷的浓度如何依赖于氧的温度和分压的变化。Sr4Mn2-xFe1+xO10 -δ中不稳定氧的部分热力学函数的计算图与实验图很好地吻合,支持了热力学分析的一致性。
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来源期刊
Acta Materialia
Acta Materialia 工程技术-材料科学:综合
CiteScore
16.10
自引率
8.50%
发文量
801
审稿时长
53 days
期刊介绍: Acta Materialia serves as a platform for publishing full-length, original papers and commissioned overviews that contribute to a profound understanding of the correlation between the processing, structure, and properties of inorganic materials. The journal seeks papers with high impact potential or those that significantly propel the field forward. The scope includes the atomic and molecular arrangements, chemical and electronic structures, and microstructure of materials, focusing on their mechanical or functional behavior across all length scales, including nanostructures.
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