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Consider an external electric field propagating through a homogeneous medium. When the electric field crosses the surface boundary of the medium, it undergoes a discontinuity. The electric field can be resolved into normal and tangential components. The amount by which the field changes at any boundary is given by the difference between the field components above and below the surface boundary.
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An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
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在2022年海底表征实验中使用虚拟数组进行反转a)

Zoi-Heleni Michalopoulou1, Peter Gerstoft2, William S Hodgkiss2

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"2022年海底特性实验"使用基于高斯过程的匹配场反转 (GP-MFI) 来研究细粒度海底沉积物. 与传统技术相比,这种先进的方法提高了地理声学属性估计的准确性,并降低了不确定性.

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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
  • 信号处理 信号处理

背景情况:

  • 细粒度沉积物影响水下声学传播.
  • 精确的地声学特性对于声纳和水下通信至关重要.
  • 传统的匹配场倒置 (MFI) 在复杂的环境中存在局限性.

研究的目的:

  • 评估估计沉积物的地声学性质的方法.
  • 将传统的MFI与基于高斯过程 (GP) 的新型MFI进行比较.
  • 评估GP-MFI在细粒度沉积物的表征方面的表现.

主要方法:

  • 在2022年海底特性实验 (SBCEX22) 中收集的音调声学数据.
  • 使用传统的MFI和基于GP的MFI的来源定位和地声逆转.
  • 基于GP的MFI使用虚拟阵列来进行增强的数据插值和声场一致性分析.
  • 用于反转优化的遗传算法.

主要成果:

  • 基于GP的MFI在地声逆转方面表现出卓越的表现.
  • 总理-货币金融机构的方法产生了与地面真相数据强烈一致的结果.
  • 与传统的MFI相比,GP-MFI对地声学属性估计的不确定性减少.

结论:

  • 基于高斯过程的匹配场反转是一种更有效的技术,用于细粒度沉积物的表征.
  • GP-MFI提供了更高的准确性和可靠性,用于估计地声学属性.
  • 该方法显示了推动海底声学研究的巨大潜力.