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Inversion of seabed acoustic parameters by using the bubble pulses and the shock wave

机译:利用气泡脉冲和冲击波反演海床声学参数

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Explosive charges are widely used in underwater acoustics experiments because it has wide bandwidth and high source level. the received signals are the shock wave and followed by a series of bubble pulses, which seriously affect the observation and applications of the signal. But for the shallow water waveguides, the bubble pulses could be seen as anther “signal”. In this paper, we treat the first bubble pulse as a signal to extract the dispersion curve through the warping transformation and then to invert the seabed velocity and density; At the same time, we get the shock wave of data from some depth with a higher SNR(signal to noise ratio) and its first mode wave, then the distance normalized normal modes transmission loss is used to obtain the seabed attenuation.
机译:由于炸药具有宽带宽和高声源水平,因此在水下声学实验中被广泛使用。接收到的信号是冲击波,然后是一系列气泡脉冲,这严重影响了信号的观察和应用。但是对于浅水波导,气泡脉冲可以看作是花药“信号”。在本文中,我们将第一个气泡脉冲作为信号,通过翘曲变换提取色散曲线,然后反转海床速度和密度。同时,从一定深度获得具有较高信噪比的数据冲击波及其第一模态波,然后利用距离归一化的标准模态传输损耗来获得海底衰减。

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