在低速度海底中,低到中频的声音衰减
Ji-Xun Zhou1,2, Zhenglin Li3, Xuezhen Zhang1
1State Key Laboratory of Acoustics, Institute of Acoustics, Chinese Academy of Sciences, Beijing 100190, China.
The Journal of the Acoustical Society of America
|May 28, 2024
概括
精确测量海底声衰减,特别是低速度海底 (LVB),是一个挑战. 这项研究使用黄海的声学传播特征来推导LVB声衰减.
科学领域:
- 地质物理学 地质物理学
- 声学 声学 在声学方面
- 海洋学 海洋学 海洋学
背景情况:
- 海底声学衰减很难确定,特别是对于低速度底部 (LVB).
- 由于LVB的低速度和衰减,在地声逆转方面面临挑战,称为海底速度-衰减合.
- 准确的海底速度概况对于LVB减弱反转至关重要.
研究的目的:
- 在黄海内的低速度底部 (LVB) 获得声衰减.
- 在具有强烈热线和LVB的复杂环境中研究声学传播特征.
- 为了克服LVB.在地球声学倒置方面的挑战.
主要方法:
- 在黄海分析爆炸声的传播.
- 利用声学现象,如模态分散,水波和吸管效应.
- 精确测量关键频率,艾瑞频率,艾瑞波速率和第一模式组速率.
主要成果:
- 在使用逆向海底参数的LVB层和地下层中推导速度.
- 计算的源级正常化传输损失和第一模式衰变率高达27.66公里.
- 在LVB中确定了13Hz至5000Hz的频率的声音衰减.
结论:
- 在黄海中成功地获得了低速度底部 (LVB) 的声衰减.
- 证明了声学传播特征对海底参数逆转的实用性.
- 为了解LVB环境的声学特性提供了有价值的数据.
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