用海洋底分布式声学传感来观察以模式传播的T波的散射关系
Jean Lecoulant1, Samuel Pinson1
1IRENav, École Navale, Brest 29200, France.
The Journal of the Acoustical Society of America
|July 24, 2025
概括
海底分布式声学传感 (DAS) 有效地测量地震波. 这项研究使用Scholte和T波来逆转海底特性,推进海洋学和地震研究.
科学领域:
- 地质物理学 地质物理学
- 海洋学 海洋学 海洋学
- 地震学 地震学
背景情况:
- 海底分布式声学传感 (DAS) 测量来自地震声波的应力.
- 在音速下,T波在水柱中以模式传播.
- DAS提供密集的时空采样,用于分析波散.
研究的目的:
- 使用DAS数据来利用Scholte和T波逆转海底特性.
- 为了确定剪切速度配置和海底密度.
- 为了在海底逆转压缩波速度.
主要方法:
- 分析肖尔特波 (0.1-1.5 Hz) 以确定功率法分散曲线.
- 使用分析模型的功率定律剪切速度形状和海底密度的决定性反转.
- 在流体-流体-固体波导模型中,分析T波 (2-30 Hz) 来逆转压缩波速度.
主要成果:
- 肖尔特波浪能量在频率波数域中展示了电力规律区域.
- 一个恒定的海底密度和一个动力定律剪切速度概况被成功反转.
- 一个T波模式被确定用于压缩波速度逆转,利用逆转的海底密度.
结论:
- 通过地震声波分析,DAS有效地描述了海洋底的特性.
- 这项研究强调了舒尔特波和T波在地球物理逆转中的实用性.
- 关于波导模式差异的讨论提供了关于海底组成的见解.
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