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Methods of isotopic relaxations for estimation of oxygen diffusion coefficients in solid electrolytes and materials with mixed ionic-electronic conductivity

机译:同位素弛豫方法估计固体电解质和具有混合离子电导率的材料中的氧扩散系数

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摘要

Theoretical basis of isotopic oxygen exchange in a gas-solid oxide system are considered. A generalized model is suggested that accounts for diffusion of tracer oxygen atoms and allows within a single approach to perform numeric analysis of isotope experiments implemented in reactors of various types and in different temperature modes. It is shown that when (CO2)-O-18 is used as an isotopic reagent, the oxygen exchange rate on the metal oxide surface increases manifold (as compared to O-18(2)), which allows determining more precisely diffusion limitations in case of isotopic exchange of oxygen in the oxide bulk. Estimates of oxygen self-diffusion coefficients are obtained in dispersed systems based on doped cerium-zirconium oxides with a fluorite-type structure, doped lanthanum silicates with an apatite-type structure, and also mixed praseodymium nickelates-cobaltites and their composites with yttrium-doped ceria.
机译:考虑了气固氧化物体系中同位素氧交换的理论基础。提出了一种通用模型,该模型考虑了示踪氧原子的扩散,并允许在单一方法内对在各种类型和不同温度模式下的反应堆中进行的同位素实验进行数值分析。结果表明,当(CO2)-O-18用作同位素试剂时,金属氧化物表面的氧交换速率增加(与O-18(2)相比),这可以更精确地确定在氧化物主体中进行氧同位素交换的情况。氧自扩散系数的估算是在分散系统中进行的,这些系统基于具有萤石型结构的掺杂铈锆锆氧化物,具有磷灰石型结构的掺杂硅酸镧硅酸盐,以及混合的nickel酸镍-钴和它们的掺钇钇的复合物氧化铈。

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