在新英格兰泥的剪切和压缩地球声学配置文件的贝叶斯匹配场反转)
Stan E Dosso1, Preston S Wilson2, David P Knobles3
1School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia V8W 2Y2, Canada.
JASA express letters
|April 3, 2025
概括
这项研究使用贝叶斯反转声学数据估计了海底的地声学概况. 结果显示,泥层的剪切波速度较低,压缩参数已确定.
科学领域:
- 海洋声学 海洋声学
- 地质物理学 地质物理学
- 海底特征的描述
背景情况:
- 准确的海底地球声学特性对于水下声学传播建模至关重要.
- 新英格兰泥是研究沉积物特性的一个关键地点.
研究的目的:
- 为了估计新英格兰泥的剪切和压缩海底地球声学配置文件.
- 评估剪切特性对压缩参数估计的影响.
主要方法:
- 匹配场声学数据的跨维贝叶斯反转.
- 在20至2000赫兹带宽的分析.
- 与剪切参数和没有剪切参数的反向的比较.
主要成果:
- 低剪波速度 (∼35 m/s) 在上层泥层中估计有小的不确定性.
- 剪波速度在底层的过渡层和沙层中增加.
- 包括衰减在内的压缩参数估计得很好,但剪切波衰减的确定不好.
- 压缩参数估计在很大程度上独立于剪切效应,除了可能在沙层中的压缩波衰减.
结论:
- 贝叶斯反转有效地估计了海底的地球声学配置文件.
- 在这种环境中,剪切特性对压缩参数估计的影响最小.
- 对特定层的剪切波衰减进行进一步的研究可能是有必要的.
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