观测和建模由集装箱船发射的低频调的范围依赖的传播)
Peter H Dahl1, David R Dall'Osto1
1Applied Physics Laboratory, University of Washington, Seattle, Washington 98105, USA.
The Journal of the Acoustical Society of America
|October 8, 2025
概括
研究人员使用低频音频发射研究了新英格兰泥上的海底特性. 他们模拟了声音传播,以估计深层沉积物中的压缩波衰减,发现它在16 Hz时为0.17±0.03 dB/λ.
科学领域:
- 海洋声学 海洋声学
- 海洋地质物理学 海洋地质物理学
- 处理地震信号的地震信号处理.
背景情况:
- 新英格兰泥的特点是低音速的泥层.
- 了解海底特性对于声学传播建模至关重要.
研究的目的:
- 为了研究海底的特性,特别是压缩波衰减,在新英格兰泥.
- 为了利用商船的低频音频排放进行地球声学反转.
主要方法:
- 音响数据的前建模使用附带的正常模式.
- 为上层沉积物开发一个范围变化的地球声学模型.
- 贝叶斯倒数用于估计深沉沉积物中的频率依赖的压缩波衰减.
主要成果:
- 使用地球声学模型成功复制了声学模式干扰模式.
- 估计在深沉沉积物中的压缩波衰减在16 Hz时为0.17±0.03 dB/λ.
- 在模型中包含弹性效应可以将估计的压缩波减弱率降低10%-40%.
结论:
- 这项研究为新英格兰泥的地声学特性提供了宝贵的见解.
- 精确的弹性效应建模对于精确的衰减估计很重要.
- 低频声波可以有效地探测深层沉积物的特性.
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