冲击波载荷对β1 Cu-Al-Ni马氏体单晶相变温度、弹性和非弹性性能的影响

S. Golyandin, S. Kustov, S. Nikanorov, K. Sapozhnikov, A. Sinani, J. Humbeeck, R. Schaller, R. Batist
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引用次数: 1

摘要

摘要:研究了高速冲击载荷对β′1马氏体Cu-Al-Ni形状记忆合金组织、相变温度、弹性和非弹性性能的影响。用轻气枪对晶体进行冲击加载,产生持续时间约为2 × 10−6 s的压缩平面应变波脉冲。应力在应变波传播方向上的法向分量范围为0.5 ~ 5 GPa,并以此作为冲击强度的特征。冲击载荷对相变温度和马氏体变异体组织的影响在目前的实验结果中还不能被识别出来。与晶体的宏观性质相反,在约100 kHz频率下,研究发现晶体的弹性和非弹性性质受到冲击载荷的强烈影响。冲击对晶体的弹性和非弹性性能以及宏观性能的影响之间的差异是在假设这些性能与不同的结构实体有关的情况下解释的。断裂马氏体中部分位错系统的变化和内应力的变化被认为是观察到的弹性和非弹性效应的基本因素。温度范围的稳定性和马氏体相变的迟滞性归因于相当稳定的马氏体变相结构(在目前的冲击条件下)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The effect of shock-wave loading on transformation temperatures, elastic and anelastic properties of β1 Cu-Al-Ni martensitic single crystals
Abstract The effect of high-velocity impact loading on the structure, transformation temperatures, elastic and anelastic properties has been studied for a Cu-Al-Ni shape memory alloy in the β′1 martensitic phase. The impact loading of crystals has been performed by means of a light gas gun, producing compressive plane-strain wave pulses with a duration of about 2 × 10−6 s. The normal component of stress in the direction of the strain wave propagation ranged from 0.5 to 5 GPa and was used as a characteristic of the impact magnitude. The influence of the impact loading on the transformation temperatures and the structure of martenistic variants cannot be discerned in the present experimental results. In contrast with the macroscopic properties of crystals, the elastic and anelastic properties, studied at a frequency of about 100 kHz, are found to be strongly influenced by the impact loading. The difference between the effects of the impact on elastic and anelastic properties and on the macroscopic performance of crystals is interpreted on the assumption that these properties are related to different structural entities. Changes in the system of partial dislocations in the faulted martensite and variations in internal stresses are considered as basic contributors to the observed elastic and anelastic effects. The stability of the temperature range and hysteresis of the martensitic transformation are ascribed to the rather stable (under the present impact conditions) martensitic variant structure.
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