High-temperature thermodynamic properties of Y-doped barium zirconates, BaZr1–xYxO3−x/2 (x = 0.1, 0.2), with perovskite-type structure

IF 1.2 4区 地球科学 Q4 MATERIALS SCIENCE, MULTIDISCIPLINARY Physics and Chemistry of Minerals Pub Date : 2024-12-19 DOI:10.1007/s00269-024-01304-6
Dmitry S. Tsvetkov, Dmitry A. Malyshkin, Vladimir V. Sereda, Ivan L. Ivanov, Nadezhda S. Tsvetkova, Andrey Yu. Zuev
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Abstract

Perovskite-type oxides BaZr1–xYxO3−x/2 (x = 0.1, 0.2) were synthesized and their enthalpy increments were measured by means of high-temperature drop calorimetry in the temperature range of (373–1273) K in air. The data obtained were used for estimating the high-temperature thermodynamic functions (constant pressure heat capacity and entropy increments) of the zirconates BaZr1–xYxO3−x/2 (x = 0.1, 0.2). They were found to be only weakly dependent on the concentration of Y-dopant. Thermal expansion coefficient of zirconates BaZr1–xYxO3−x/2 (x = 0.1, 0.2) was successfully estimated by Grüneisen equation. Also, Neumann-Kopp rule was shown to be inapplicable for accurate estimation of heat capacities of the studied oxides. Thermodynamic analysis showed that BaZr1–xYxO3−x/2 (x = 0.1, 0.2) oxides are prone to chemical interaction with CO2 at typical working temperatures of proton-conducting solid oxide fuel cells. Some possibilities to overcome this issue have been discussed.

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具有钙钛矿型结构的掺y锆酸钡BaZr1-xYxO3−x/2 (x = 0.1, 0.2)的高温热力学性质
合成了钙钛矿型氧化物BaZr1-xYxO3−x/2 (x = 0.1, 0.2),并在空气(373 ~ 1273)K温度范围内用高温滴量热法测定了它们的焓增量。所得数据用于估算锆酸盐BaZr1-xYxO3−x/2 (x = 0.1, 0.2)的高温热力学函数(恒压热容和熵增量)。发现它们对y掺杂剂浓度的依赖性较弱。利用gr neisen方程成功估算了锆酸盐BaZr1-xYxO3−x/2 (x = 0.1, 0.2)的热膨胀系数。此外,诺伊曼-科普规则也不能准确地估计所研究的氧化物的热容。热力学分析表明,在质子传导固体氧化物燃料电池的典型工作温度下,BaZr1-xYxO3−x/2 (x = 0.1, 0.2)氧化物易于与CO2发生化学相互作用。已经讨论了克服这个问题的一些可能性。
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来源期刊
Physics and Chemistry of Minerals
Physics and Chemistry of Minerals 地学-材料科学:综合
CiteScore
2.90
自引率
14.30%
发文量
43
审稿时长
3 months
期刊介绍: Physics and Chemistry of Minerals is an international journal devoted to publishing articles and short communications of physical or chemical studies on minerals or solids related to minerals. The aim of the journal is to support competent interdisciplinary work in mineralogy and physics or chemistry. Particular emphasis is placed on applications of modern techniques or new theories and models to interpret atomic structures and physical or chemical properties of minerals. Some subjects of interest are: -Relationships between atomic structure and crystalline state (structures of various states, crystal energies, crystal growth, thermodynamic studies, phase transformations, solid solution, exsolution phenomena, etc.) -General solid state spectroscopy (ultraviolet, visible, infrared, Raman, ESCA, luminescence, X-ray, electron paramagnetic resonance, nuclear magnetic resonance, gamma ray resonance, etc.) -Experimental and theoretical analysis of chemical bonding in minerals (application of crystal field, molecular orbital, band theories, etc.) -Physical properties (magnetic, mechanical, electric, optical, thermodynamic, etc.) -Relations between thermal expansion, compressibility, elastic constants, and fundamental properties of atomic structure, particularly as applied to geophysical problems -Electron microscopy in support of physical and chemical studies -Computational methods in the study of the structure and properties of minerals -Mineral surfaces (experimental methods, structure and properties)
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