海洋压缩空气源阵列声场特征从海上测量:远程传播)
Kun Li1, Natalia Sidorovskaia2
1John W. Deming Department of Medicine, School of Medicine, Tulane University, New Orleans, Louisiana 70112, USA.
The Journal of the Acoustical Society of America
|September 26, 2024
概括
海洋地震调查会产生远距离传输的声音. 这项研究测量了声传播,发现由于接收器深度和海底条件等因素,声传播水平可能会随范围的意想不到地增加.
科学领域:
- 海洋学 海洋学 海洋学
- 海洋声学 海洋声学
- 地震勘探的地震勘探工作
背景情况:
- 海洋地震调查使用压缩空气阵列,产生大量的声能.
- 了解远程声学传播对于环境影响评估和地球物理调查至关重要.
研究的目的:
- 测量海洋地震源阵列的三维声学场.
- 分析远程声学传播特征,包括接收的声压和声暴露水平 (SEL).
- 调查接收器深度,阵列方向和传播条件对声信号的影响.
主要方法:
- 2007年在墨西哥湾北部进行了全面的实验.
- 使用标准的海洋压缩空气源阵列测量声场.
- 收集了各种范围和深度收到的声压水平和SEL的数据.
主要成果:
- 收到的峰值压力水平和SEL表现出与范围的非单调 (振荡) 行为,在更长的距离上增加了10dB.
- 在20公里之外,最浅的水音箱的声级超过了更深的水音箱的3-10dB,这表明了表面管道效应.
- 与范围依赖条件相比,范围独立的浴度测量导致接收的声级大约高出4dB.
结论:
- 来自地震阵列的远程声学传播是复杂的,并受到环境因素的影响.
- 实验数据为验证声源和传播模型提供了有价值的数据集.
- 准确的建模对于预测地震源远场中的声压和SEL至关重要.
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