物理学报2024,Vol.73Issue(5) :132-142.DOI:10.7498/aps.73.20231715

基于多层水平变化浅海海底模型的低频反演方法

Low frequency inversion method based on multi-layer holizontal variation shallow seafloor model

康娟 彭朝晖 何利 李晟昊 于小涛
物理学报2024,Vol.73Issue(5) :132-142.DOI:10.7498/aps.73.20231715

基于多层水平变化浅海海底模型的低频反演方法

Low frequency inversion method based on multi-layer holizontal variation shallow seafloor model

康娟 1彭朝晖 2何利 2李晟昊 2于小涛2
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作者信息

  • 1. 中国科学院声学研究所,声场声信息国家重点实验室,北京 100190;中国科学院大学物理学院,北京 101407
  • 2. 中国科学院声学研究所,声场声信息国家重点实验室,北京 100190
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摘要

准确获取海底声学参数对声场分析、声纳应用等具有重要意义.反演是获取海底声学参数的重要手段之一.为了避免反演中的多值问题,地声反演往往尽量减少待反演参数,多采用单层或双层水平不变地声模型,反演后的声学参数仅能在有限频段应用,难以同时应用于较宽频段.本文以实验中浅地层剖面仪测量的海底沉积层分层结构为基础建立地声模型,采用多物理量分步联合手段反演各沉积层声学参数,并通过匹配场定位、后验概率分析、采样等手段对反演结果进行验证.将反演结果与单层等效地声模型反演结果进行对比分析,结果说明,本文建立的多层水平变化海底声学参数更接近真实情况,可以应用在较宽频段范围,解释不同声学现象,且精度更高.

Abstract

Sound propagation in shallow water is significantly influenced by geoacoustic properties.Estimating these geoacoustic parameters is essential for sound field analysis and sonar performance assessment.As a common practice,the seafloor is often treated as a single-layer or two-layer range-independent geoacoustic model to reduce the number of involved parameters.However,acoustic parameters inverted through these two geoacoustic models are typically limited in their applicability to a specific frequency range,thus posing challenges when applied across a broader frequency range.A range-dependent multi-layer geoacoustic model based on experimental measurements obtained with a sub-bottom profiler is proposed in this study.The inversion scheme combines three inversion methods to estimate geoacoustic parameters,considering the different sensitivities of geoacoustic parameters to different physical parameters within the acoustic field.Firstly,modal dispersion is used to invert the geoacoustic parameters of each layer,with the dispersion curve obtained through warping transform and the Wigner-Ville distribution.After that,both the localization using matched field processing and the dispersion curve fitting demonstrate the effectiveness of the inversion results for each layer,although the peak of the probability distribution of sound speed in the first layer is broader than in others.Secondly,matched field processing is employed to invert the geoacoustic parameters of the first layer.This method is based on the theory that as frequency increases,the depth of sound rays penetrating the seabed decreases,revealing changes in the first layer's sound speed with the seabed depth.Lastly,bottom attenuation coefficients at different frequencies are inverted by the transmission loss(TL),and a fitting relationship between the attenuation coefficient and the frequency is derived.The inversion results obtained by using the range-dependent multi-layer geoacoustic model are compared with results estimated by the single-layer geoacoustic model.The findings indicate that the transmission loss(TL)error from the range-dependent multi-layer geoacoustic model in this study is smaller than that from the single-layer geoacoustic model,especially in the lower frequency band.The range-dependent multi-layer geoacoustic model proves to be suitable for a broader frequency range,providing better precision in explaining various acoustic phenomena.

关键词

宽带地声反演/多层水平变化海底/简正波频散/传播损失

Key words

broadband geoacoustic inversion/range-dependent multi-layer geoacoustic model/modal dispersion/transmission loss

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基金项目

国家重点研发计划(2021YFF0501200)

国家自然科学基金(12204507)

出版年

2024
物理学报
中国物理学会,中国科学院物理研究所

物理学报

CSTPCDCSCD北大核心
影响因子:1.038
ISSN:1000-3290
参考文献量27
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