在新英格兰泥的海洋沉积物声波导系统的正常模式
1Marine Physical Laboratory, Scripps Institution of Oceanography, University of California, San Diego, 9500 Gilman Drive, La Jolla, California 92093-0238, USA.
The Journal of the Acoustical Society of America
|September 23, 2025
概括
研究人员在新英格兰泥 (NEMP) 的三层波导中分析了声场. 他们发现了11个固有值,每一个与传播正常模式相关,揭示了波导的行为.
科学领域:
- 海洋声学 海洋声学
- 地质物理学 地质物理学
- 波导理论波导理论
背景情况:
- 新英格兰泥 (NEMP) 具有一个泥层,覆盖着一个沙泥地下室,具有反正方形的声速概况.
- 海洋和沉积物形成了一个三层声波导.
研究的目的:
- 分析NEMP波导的每个层内的声场.
- 调查这种特定的声环境的模式解决方案和特征方程.
主要方法:
- 使用空间里叶变换在深度和水平范围.
- 在海面,海底和地下室接口处应用的边界条件.
- 使用图形二分法解决了自值的超越性特征方程.
主要成果:
- 确定了11个固有值,每一个都对应于传播的正常模式.
- 证明NEMP波导在一个限制性情况下减少到一个反转的Pekeris波导.
- 显示的NEMP特征方程在这个极限中与Pekeris通道方程相同.
结论:
- 该研究提供了NEMP波导的详细声学分析.
- 这些发现证实了波导的行为及其与Pekeris通道的关系.
- 这项研究有助于理解复杂的海洋环境中的声学传播.
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