通过加速测量发现雪崩源
Emil Bronstein1, Eilon Faran2, Ronen Talmon3
1Faculty of Mechanical Engineering, Technion - Israel Institute of Technology, Haifa, 3200003, Israel. emilbr@campus.technion.ac.il.
Nature communications
|August 29, 2024
概括
研究人员开发了一种新的加速度测量方法来研究材料中的雪崩来源. 这种技术揭示了独特的雪崩源特性,与声辐射信号不同,为变形过程提供了洞察力.
科学领域:
- 材料科学 材料科学 材料科学
- 固体力学 固体力学是什么
- 可变形物体的物理学
背景情况:
- 雪崩源是快速的,对于材料变形至关重要的局部事件.
- 声波发射 (AE) 信号被传输函数修改,掩盖源特征.
- 由于信号扭曲,理解雪崩源物理是具有挑战性的.
研究的目的:
- 开发一种新的实验方法来隔离和描述雪崩源.
- 在变形结合中研究雪崩源的物理性质.
- 要区分内在的雪崩源行为和转移函数效应.
主要方法:
- 利用加速度测量来消除声学转移功能的影响.
- 应用了该方法来研究中的变形结合.
- 分析了振幅,特征时间,以及雪崩来源的新特征.
主要成果:
- 雪崩源的幅度和时间缺乏明确的物理定律,与AE信号不同.
- 由于传输函数,AE信号的幅度和持续时间遵循功率定律.
- 确定了一个新的雪崩源特征,与结合的体积增长率有关.
- 观察到这个新功能的一种权力定律分布,表明了动态的关键性.
- 确定了雪崩源特征时间的内在上限.
结论:
- 这种新的加速度测量方法成功地隔离了雪崩源的特性.
- 区分内在的雪崩源行为与人工的AE信号关系.
- 揭示了结合过程中不可预测的动态关键性和物理限制.
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