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A new method of determination of oxygen diffusivities in polycrystalline ferrite and its verification by a nuclear microanalysis method

机译:一种多晶铁素体中氧扩散性的新方法及其核微分分解方法的验证

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Two independent methods, the isotope method based on nuclear microanalysis and the method based on measuring the electronic-conductivity activation energy, are used to determine the grain-boundary diffusion and volume diffusion of an oxygen isotope /sup 18/O in a polycrystalline lithium-titanium ferrite at the thermal annealing temperature 1073 K. A comparative analysis is conducted of the potential of the methods in studying oxygen diffusion in the material concerned. It is shown that the technique for obtaining the diffusion parameters from the electronic conductivity measurements allows a comparatively precise determination of both the volume and grain-boundary diffusion coefficients of oxygen in polycrystalline ferrites.
机译:两种独立方法,基于核微透析的同位素方法和基于测量电子导电激活能量的方法,用于确定多晶锂中氧同位素/ sup 18 / o的晶界扩散和体积扩散 - 在热退火温度1073k处的钛铁氧体。对比较分析进行了研究有关材料中氧扩散的方法的潜力。结果表明,从电子电导率测量获得扩散参数的技术允许对多晶铁氧体中氧的体积和晶界扩散系数相对精确地确定。

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