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海底频域反射系数的阶段:测量和建模
1Electrical and Computer Engineering, Portland State University, Portland, Oregon 97207, USAcharles.holland@pdx.edu.
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|February 3, 2025
概括
本研究探讨了海底反射系数的相位,揭示了它对理解地球声学属性的潜力. 测量和建模表明,对于层叠的海底,相位信息可能比大小更有价值.
科学领域:
- 地质物理学 地质物理学
- 海洋学 海洋学 海洋学
- 声学 声学 在声学方面
背景情况:
- 海底的地球声学特性对于水下声学至关重要.
- 频域反射系数的相位是大部分未开发的地球声学信息来源.
- 多层和折射性海底对声学建模提出了独特的挑战.
研究的目的:
- 调查海底反射系数阶段对地球声学性质评估的潜力.
- 提供测量和分析阶段信息的模型.
- 为了比较地声学研究中相与大小的信息含量.
主要方法:
- 海底反射系数相的现场测量是在新英格兰泥区进行的.
- 开发了一个数值模型来分析相位数据.
- 阶段和大小的信息内容进行了比较.
主要成果:
- 测量表明,获取海底反射系数相位数据的可行性.
- 提出的模型成功地分析了相位信息.
- 在某些场景中,该阶段的地声信息含量高于大小.
结论:
- 海底反射系数的相位是一个有价值的,但尚未充分利用的参数,用于表征地球声学属性.
- 利用阶段信息为增强海底分析提供了一个有希望的途径.
- 需要进一步的研究来充分理解和应用基于阶段的地球声学评估.
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