螺栓连接结构中与摩擦有关的声发射分析

Jiaying Sun, Huiyi Yang, Dongwu Li, Chao Xu
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引用次数: 0

摘要

在随机振荡载荷作用下,螺栓连接可能处于持续摩擦磨损状态,从而导致螺栓连接容易松动。因此,必须找到一种方法来及时监测螺栓连接的接触状态,并进行妥善处理。声发射(AE)信号会在螺栓连接界面的往复摩擦过程中产生。探索不同螺栓预紧力下摩擦滑移特征与声发射特征之间的关系,可为利用声发射技术监测螺栓连接的预紧状态奠定基础。本文通过实验研究了螺栓连接结构在不同预紧力下摩擦时的声发射信号,共进行了三次重复试验。研究了不同预紧力下摩擦行为与声发射特征之间的关系。还分析了经典声发射参数和运动学参数随螺栓预紧力水平的变化。分析了参数测试后试样的三维形貌。结果表明,爆破型和连续型声发射的特征都能反映不同螺栓预紧力下的不同摩擦行为。在摩擦运动学参数和螺栓预紧力水平的相互作用下,声发射参数的演化曲线发生了变化。对于三维表面形貌,往复摩擦剪切了表面峰值,填充了表面谷值,划痕表面区域的形貌重新分布。
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Analysis of friction‐related acoustic emission in bolted joint structures
A bolted joint may be in a state of continuous fretting friction and wear under random oscillatory loading, which makes the bolted joint prone to loosening. Therefore, it is essential to find a way to monitor the contact state of a bolted joint on time and handle it adeptly. Acoustic emission (AE) signals will be generated during the reciprocating friction of the bolted joint interface. Exploring the relationship between the frictional slip features and the acoustic emission characteristics under different bolt preloads can lay the foundation for using the acoustic emission techniques to monitor the pretightening state of bolted joints. This paper experimentally investigates the acoustic emission signals of a bolted joint structure during friction under different preloads, three repeated tests are implemented. The relationship between friction behavior and acoustic emission characteristics under different preloads is studied. The evolution of classical acoustic emission parameters and kinematic parameters with bolt preload levels is also analyzed. The 3‐D topography of the specimens after parametric tests is analyzed. The results show that the characteristics of both burst‐type and continuous‐type acoustic emission can reflect different friction behavior under different bolt preloads. The evolution curves of acoustic emission parameters changed under the interaction of both frictional kinematic parameters and bolt preload levels. For the 3‐D surface topography, the reciprocating friction shears the peaks and fills the surface valleys, and the topography of the scratched surface areas is redistributed.
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