海洋低频噪声传播建模方法的比较

Alexios Korakas, J. Hovem
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引用次数: 4

摘要

在这项研究中,射线模型的性能预测浅水场景,如在沿海地区遇到的远程声传播,进行了测试和讨论。近年来,海洋环境中人类活动的增加(地震勘探、风力发电、航运等)导致海洋噪音水平普遍显著提高,引起了人们对其对海洋生物和渔业影响的关注。海洋中的人为噪音覆盖了很宽的频谱范围,包括低至10赫兹的非常低的频率,并且可以传播几十公里的距离。因此,建立声学传播模型以预测海洋环境中的噪声影响,对于各种应用中的声学系统设计以及符合有关海洋中声音使用的规定变得非常重要。该研究将光线追踪模型(PlaneRay)计算的透射损耗与距离曲线与两种特别适用于浅水环境的波浪理论模型(即波数积分(WI)模型和抛物线方程(PE))的解进行了比较,这些模型基于许多日益复杂的典型测试案例。特别是,现有的WI模型允许在距离无关的环境中组合多个流体和弹性底层。另一方面,现有的PE模型允许在距离无关和距离相关的环境中进行比较,底部被描述为全流体或全弹性。测试用例相应地选择由位于流体或弹性底部半空间上的水层组成。在15至100赫兹的频谱范围内对每个案例进行分析和解释。对比结果表明,射线追踪模型与PE和WI模型具有较好的一致性。特别是,虽然基于高频近似值,但射线追踪模型似乎是一种可接受和有效的选择,即使在低频和/或浅水环境下也能提供可靠的预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Comparison of modeling approaches to low-frequency noise propagation in the ocean
In this study, the performance of a ray model for the prediction of long-range acoustic propagation in shallow-water scenarii, such as those encountered in coastal areas, is tested and discussed. Increased human activities in the marine environment over the recent years (seismic exploration, wind farming, shipping, etc.) has caused a significant general increase in ocean noise level, raising concerns over its impact on marine life and fisheries. Anthropogenic noise in the oceans covers a wide spectral range, including very low frequencies down to 10 Hz, and can propagate over large distances up to several tens of kilometers. Modeling the acoustic propagation to predict the noise impact in the marine environment thus becomes important for acoustic-system design in various applications and in compliance with the regulations regarding the uses of sound in the ocean. The study compares transmission-loss-versus-range curves calculated by a ray-tracing model (PlaneRay) with solutions by two wave-theoretic models particularly suited ti the shallow-water environment, namely a wavenumber integration (WI) model and a parabolic equation (PE)-based in a number of canonical test cases of increasing complexity. In particular, the WI model at hand allows for a combination of several fluid and elastic bottom layers in range-independent environments. On the other hand, the PE model at hand allows for comparisons in both range-independent and range-dependent environments with the bottom being described as all-fluid or all-elastic. The test cases are accordingly chosen to consist of a water layer lying over a fluid or elastic bottom half-space. Each case is analyzed and interpreted at several frequencies in the spectral range from 15 to 100 Hz. The comparison results show a good and promising agreement of the ray-tracing model with the PE and WI models. In particular, although based on the high-frequency approximation, the ray-tracing model appears to be an acceptable and efficient choice providing reliable predictions even at low frequencies and/or shallow-water environments.
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