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Vacancy Formation and Diffusion in FeAI-Alloys

机译:FeAI合金中的空位形成和扩散

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Absolute concentrations of vacancies in FeAl-alloys have been measured by means of differential dilatometry and positron annihilation techniques, which have been calibrated by determination of positron trapping rates. At lower Al concentrations the defects appear to be single vacancies, whereas above 35 at.% Al aggregates as triple defects in B2(l) or additional divacancies have to be considered in B2(h). In this context the B2-phase field has to be split into several regions B2', B2(l) and B2(h). In B2(h) Arrhenius plots show sudden breaks followed by small slopes. These can be shown to be the result of temperature dependent thermodynamic changes in local order with higher order transitions. This has been deduced from positron lifetime measurements and their pressure dependence and the thus obtained formation volumes and the change in formation enthalpies and -entropies in the respective ranges. This view is further corroborated by coincidence spectra of the 511 keV positron annihilation line. Studying the annihilation of quenched-in defects by positrons, their mobility may be obtained, strongly decreasing with Al content. Several annealing steps can be found in some concentration ranges with different mobilities. Chemical diffusion D is characterized by an increase in A2 due to a strong Al-vacancy binding and the thermodynamic factor. At the A2-B2-transition D decreases sharply and stays relatively constant up to stoichiometry except in B2(h) above 35 at.% Al in agreement with. The magnitude and concentration dependence of the thermodynamic factor is still less clear. Kirkendall shift corrected for volume contraction indicates that the ratio of the intrinsic diffusivities D(Al)/D(Fe) is always larger than one in the order of 1.2-1.5 in ordered FeAl and 1.75-1.78 in disordered A2 at 20 at.% Al.
机译:FeAl合金中空位的绝对浓度已通过微分膨胀法和正电子an没技术进行了测量,这些技术已通过确定正电子俘获率进行了校准。在较低的Al浓度下,缺陷似乎是单空位,而在B2(l)中,大于35 at。%的Al聚集为三重缺陷或必须在B2(h)中考虑其他空位。在这种情况下,B 2相场必须被分成几个区域B 2′,B 2(1)和B 2(h)。在B2(h)中,阿雷尼乌斯(Arrhenius)图显示了突然的断裂,随后是小的坡度。这些可以证明是局部温度随更高阶跃迁的温度相关热力学变化的结果。这是从正电子寿命测量及其压力依赖性以及由此获得的地层体积以及各个范围内地层焓和熵的变化推论得出的。 511 keV正电子an灭线的重合光谱进一步证实了该视图。研究正电子对淬火缺陷的ni灭,可以获得其迁移率,随Al含量的降低而大大降低。可以发现在一些浓度范围内具有不同迁移率的几个退火步骤。化学扩散D的特征在于由于强的Al-空位结合和热力学因素而导致A2增加。在A2-B2处,D急剧下降,直到化学计量为止都保持相对恒定,除非B2(h)中高于35 at。%Al的B一致。热力学因数的大小和浓度依存性还不清楚。校正了体积收缩的Kirkendall位移表明,在20 at。%的有序FeAl中,固有扩散率D(Al)/ D(Fe)的比率始终大于1.2-1.5的一个,在无序A2中为1.75-1.78的一个。铝

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