基于神经网络模型的浅水分层海底地声参数反演方法

Xiaorou Zhang, Z. Cui, Qile Wang, Hanhao Zhu, Wei Liu, Z. Chai
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引用次数: 0

摘要

现阶段,在浅海地声参数反演研究中,传统的反演方法侧重于计算默认海底分层下的参数反演,并没有明确海底分层。因此,在处理未知海底分层下的实验数据时,无法准确给出符合特定海底分层的地声参数。针对这些问题,本文提出了一种基于海底分层物理模型和神经网络算法模型的分层浅海地声参数反演方法。首先,通过仿真选择具有分层结构的海底物理模型,利用快速场声场法(FFM)对声场进行计算,得到不同分层条件下浅海声压场的理论预测值。其次,建立模式识别神经网络算法,分析不同海底层下预测声压场的特征;最后,根据分层结果,将声压场代入相应层的海底参数反演模型,进行海底参数反演,得到反演结果。实验结果表明,神经网络算法的模型迭代次数少,效率高。通过对声压场的特征分析,有效地解决了海底分层问题,大大提高了反演工作的便利性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Neural Network Model-Based Inversion Method for Stratified Seafloor Geoacoustic Parameters in Shallow Water
At this stage, in the inversion research of shallow sea geoacoustic parameters, the traditional inversion method focuses on calculating the parameter inversion under the default seafloor layering, and does not clarify the seafloor layering. Therefore, when dealing with the experimental data under the unknown seabed stratification, the geoacoustic parameters that conform to the specific seabed stratification cannot be accurately given. Aiming at such problems, this paper proposes a layered shallow sea geoacoustic parameters inversion method based on a layered physical model of the seafloor and a neural network algorithm model. First, a subsea physical model with a layered structure is selected through simulation, and the fast field sound field method (FFM) is used to calculate the sound field, then the theoretical prediction value of the shallow sea acoustic pressure field under different layered conditions is obtained. Second, the pattern recognition neural network algorithm is established to analyze the characteristics of the predicted sound pressure field under different seabed layers. Finally, according to the layered results, the sound pressure field is substituted into the seabed parameters inversion model of the corresponding layers, and the seabed parameters inversion is performed to obtain the inversion results. Experiments results show that the number of model iterations in the neural network algorithm is less and the efficiency is higher. The problem of seabed stratification is effectively solved through the characteristic analysis of the sound pressure field, which greatly improves the convenience of the inversion work.
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