在干燥的沙土中,压缩波传播和能量吸收效应的特征
Peng Cui1, Tian Su1,2, Le Liu3
1School of Architectural Engineering, ShanDong University of Technology, Zibo, 255049, Shandong, China.
Scientific reports
|December 31, 2024
概括
沙土样本的长度会显著影响峰值应力减弱. 增加样品密度和重复冲击增加了能量吸收,同时减少了对地质工程至关重要的波弱化.
科学领域:
- 地质技术工程 地质技术工程
- 保护工程 保护工程
- 土壤力学 土壤力学
背景情况:
- 了解在冲击负载下沙土的动态机械反应对于地质技术和保护工程应用至关重要.
- 在干燥的沙土中,压缩波的能量衰减定律和传播速度需要进一步研究.
研究的目的:
- 在干燥的沙土中研究压缩波的能量衰减定律和传播速度.
- 在单次和重复撞击条件下分析压缩波的动态反应.
主要方法:
- 利用改进的分裂霍普金森压力杆 (SHPB) 装置,对干燥的沙土样本进行冲击测试.
- 多种样本长度,冲击次数和样本密度,以评估它们对波浪传播和衰减的影响.
主要成果:
- 样本长度与峰值应力减弱呈指数关系;较长的样本导致较高的减弱率 (26.3%至99.0%).
- 峰值应力速度随着样本长度的增加而降低.
- 增加的撞击数量和样品密度降低了压缩波衰减,并显著增加了能量吸收密度 (386.3%的增加).
结论:
- 样本长度是压力波衰减的一个关键因素,在指数衰变之后.
- 较高的土壤密度和多重冲击改善了能量吸收能力,减少了波浪衰减.
- 能量吸收效率在两次冲击后稳定,在同等应变水平下保持一致,突出显示动态负载下的材料行为.
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