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A method of geo-acoustic parameter inversion in shallow sea by the Bayesian theory and the acoustic pressure field

机译:基于贝叶斯理论和声压场的浅海地声参数反演方法

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A method of geo-acoustic parameter inversion based on the Bayesian theory is proposed for the acquisition of acoustic parameters in shallow sea with the elastic seabed. Firstly, the theoretical prediction value of the sound pressure field is calculated by the fast field method (FFM). According to the Bayesian theory, we establish the misfit function between the measured sound pressure field and the theoretical pressure field. It is under the assumption of Gaussian data errors which are in line with the likelihood function. Finally, the posterior probability density (PPD) of parameters is given as the result of inversion. Our research is conducted in the light of Metropolis sample rules. Apart from numerical simulations, a scaled model experiment has been taken in the laboratory tank. The results of numerical simulations and tank experiments show that sound pressure field calculated by the result of inversion is consistent with the measured sound pressure field. Besides, s-wave velocities, p-wave velocities and seafloor density have fewer uncertainties and are more sensitive to complex sound pressure than s-wave attenuation and p-wave attenuation. The received signals calculated by inversion results are keeping with received signals in the experiment which verify the effectiveness of this method.
机译:提出了一种基于贝叶斯理论的地声参数反演方法,用于弹性海底浅海声参数的获取。首先,通过快速场法(FFM)计算声压场的理论预测值。根据贝叶斯理论,我们建立了测得的声压场与理论压力场之间的失配函数。它是在与似然函数一致的高斯数据误差的假设下进行的。最后,将参数的后验概率密度(PPD)作为反演的结果。我们的研究是根据Metropolis示例规​​则进行的。除数值模拟外,还对实验室水箱进行了比例模型实验。数值模拟和储罐实验的结果表明,反演结果计算出的声压场与实测声压场一致。此外,与s波衰减和p波衰减相比,s波速度,p波速度和海底密度具有更少的不确定性,并且对复杂的声压更敏感。反演结果计算出的接收信号与实验中接收到的信号一致,验证了该方法的有效性。

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