Al-Zn-Mg合金自然时效GP区形核的原位透射电镜研究

A. Chatterjee, L. Qi, A. Misra
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引用次数: 19

摘要

研究表明,Al-Zn-Mg合金自然时效过程的早期(1小时内)析出过程非常复杂,析出物类型和形成机制波动较大。在透射电镜下进行原位加热、淬火和室温自然时效,研究了早期析出物的形成和演化过程。研究表明,在非常早期的自然时效过程中,溶质团簇在~2分钟形成,随后在~10分钟形成邻近团簇的GP-II区成核。此外,发现GP-II的成核与GP-I有关,但不是一种独特的机制。观察到GP-I沉淀通过“分离”成核(即从GP-I和Al基体之间的界面)或通过原位成核(即在GP-I沉淀中)作为GP-II形成的位点。偶尔,一些GP-II析出物被观察到溶解到Al基体中,而没有进一步转化为析出物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
In situ Transmission Electron Microscopy Investigation of Nucleation of GP Zones Under Natural Aging in Al-Zn-Mg Alloy
This investigation reveals very early-stage (within an hour) precipitation during natural-aging of Al-Zn-Mg alloy can have very complex processes with strong fluctuations in precipitate types and formation mechanisms. In situ heating followed by quenching and subsequent natural-aging at room temperature was carried inside transmission electron microscope to study the formation and evolution of early-stage precipitation. Investigation reveals formation of solute clusters at ~2 mins and subsequent nucleation of GP-II zone adjacent to clusters at ~10 mins during very early-stage natural-aging. Moreover, nucleation of GP-II is found to be related to GP-I but not in one unique mechanism. GP-I precipitates were observed to act as sites for the formation of GP-II either by ‘separated’ nucleation (i.e. from the interface between GP-I and Al matrix) or via in situ nucleation (i.e. within a GP-I precipitate). Occasionally, some GP-II precipitates were observed to dissolve into Al matrix without further transforming to ƞ՛ precipitates.
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