在地震反射调查期间,从地质层反射的声音能量
Alexander S Douglass1, Shima Abadi1, Benjamin J Phrampus2
1School of Oceanography, University of Washington, Seattle, Washington 98195, USA.
The Journal of the Acoustical Society of America
|June 6, 2024
概括
深海底层显著影响低频声传播,即使在浅水深处. 海底下层,不仅仅是海底,对100Hz以下的反射能量做出了重大贡献.
科学领域:
- 地质物理学 地质物理学
- 海洋声学 海洋声学
- 海洋地震勘探 海洋地震勘探
背景情况:
- 海底特征极大地影响了声传播建模.
- 浅海底的特性已经得到了很好的研究,但深海底的特性往往被忽视.
- 深海底层会影响低频低于100赫兹的低频声信号.
研究的目的:
- 研究深海底特征对声学传播的影响.
- 量化海底层对反射声能量的贡献.
- 分析层深度和反射能量之间的关系.
主要方法:
- 对海洋地震反射调查数据的分析 (MGL2104).
- 使用了5700英寸3空气枪阵列和1200通道流器 (∼15公里).
- 检查了100Hz以下的三分之一八度频段中的声学反射.
主要成果:
- 海底下层对100Hz以下的反射能量有显著的贡献 (有时高达50%).
- 海底反射仅在临界角附近的范围内占主导地位.
- 增加海底层深度并不总是减少反射的能量.
结论:
- 深海底层在低频声传播建模中起着至关重要的作用.
- 忽视海底特征可能会导致声学传播模型的不准确性.
- 对深海底对声学影响的进一步研究是有必要的.
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