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Oxygen diffusivities in mullite/zirconia composites measured by ~(18)O/~(16)O isotope exchange and secondary ion mass spectrometry

机译:〜(18)O /〜(16)O同位素交换和二次离子质谱法测量莫来石/氧化锆复合材料中的氧扩散率

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Oxygen diffusivities in mullite/zirconia composites were measured by ~(18)O/~(16)O isotope exchange and secondary ion mass spectrometry. They exhibited a wide range of values from 10~(-21) to 10~(-10) m~2/s at temperatures between 1000 and 1350 ℃ in the composites with 0 to 80 vol% zirconia. At a fixed temperature, oxygen diffusivities in high-zirconia composites were larger by at least eight orders of magnitude than those in low-zirconia composites. The percolation threshold occurred between 30 and 40 vol% zirconia, where oxygen diffusivities dramatically changed. There was a clear tendency of the activation energies of oxygen diffusion in composites to decrease with increasing zirconia contents. The large oxygen diffusivities in the high-zirconia composites were attributed to the interconnected channels of zirconia from the microstractural aspect.
机译:通过〜(18)O /〜(16)O同位素交换和二次离子质谱法测量莫来石/氧化锆复合材料中的氧扩散率。在氧化锆体积分数为0至80的复合材料中,它们在1000至1350℃的温度下表现出从10〜(-21)到10〜(-10)m〜2 / s的宽范围值。在固定温度下,高氧化锆复合材料的氧气扩散率比低氧化锆复合材料的氧气扩散率大至少八个数量级。渗滤阈值发生在30%至40%(体积)的氧化锆之间,其中氧的扩散率急剧变化。随着氧化锆含量的增加,复合材料中氧扩散的活化能明显降低。从微观结构的角度来看,高氧化锆复合材料中较大的氧扩散性归因于氧化锆的互连通道。

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