在华盛顿大陆架上对中频声音传播的观测,其中有一个地下管道
Dajun Tang1, Brian T Hefner1, Guangyu Xu1
1Applied Physics Laboratory, University of Washington, Seattle, Washington 98105, USA.
The Journal of the Acoustical Society of America
|June 18, 2025
概括
华盛顿大陆架上的声学实验揭示了影响声音传输损失的地下管道. 海洋学过程导致声音传播在多个时间尺度上的变化.
科学领域:
- 海洋学 海洋学 海洋学
- 声学 声学 在声学上.
- 水下声音传播的传播方式
背景情况:
- 海洋学条件显著影响水下声学传播.
- 了解声音速度的变化对于声学应用至关重要.
研究的目的:
- 为了研究地下管道对中频声音传播的影响.
- 量化由于海洋学过程造成的传输损失变化.
主要方法:
- 在华盛顿大陆架上进行了联合海洋学和声学实验.
- 使用拖拉系统在现场测量声音速度和传输损失.
- 使用底部安装的声源进行长期监控.
主要成果:
- 确定了一个弱,持久的地下管道,声速最低在50-100米之间.
- 该管道对传输损失产生了10-13dB的影响.
- 在几分钟内观察到~10dB的声音强度变化和闪指数波动.
结论:
- 中频声音的传播在时间尺度上非常可变,从几分钟到几天.
- 海洋学过程,如内部潮和波浪驱动这种变化.
- 了解海洋过程对于减轻声波变化影响至关重要.
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