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引用次数: 0

摘要

通过使用宽带合成孔径声纳,可以测量沿声纳轴方向1厘米和横向方向4厘米的混响。有了这种高分辨率的测量,就有可能测量导致散射的沉积物低波数结构特征的声响应。当这些特征的波数位于传输信号的频带之外时,可以通过它们对后向散射信号中的高波数分量的调制来观察它们。利用将调制项与底部结构的确定性测量相结合的模型,表明在进行测量的地点,这些项对使用真实阵列的声纳的后向散射信号的方差没有显着贡献。而对于宽带合成孔径声呐,这些调制分量主导了后向散射信号的方差。这导致在混响中存在强结构,通过自适应匹配应用于信号和混响的滤波来实现额外的处理增益。这个增益是在经典理论预测的基础上增加的,它是由高分辨率声纳实现的底部不一致区域的减少引起的。
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The reverberation for a broadband synthetic aperture sonar
By use of a broadband synthetic aperture sonar it has been possible to measure the reverberation with a resolution in the order of 1 cm along the sonar axis and 4 cm in the transverse direction. With such high resolution measurements it is possible to measure the acoustic response of low wavenumber structural features of the sediment which contribute to the scattering. While the wavenumbers of these features lie outside the band of the transmitted signal they can be observed via their modulation of the high wavenumber components in the backscattered signal. Using models developed to incorporate the modulation terms, together with the deterministic measurements of the bottom structure, it was shown that at the site where the measurements were carried out these terms did not significantly contribute to the variance of the backscattered signal for a sonar using a real array. For a broadband synthetic aperture sonar however these modulation components dominated the variance of the backscattered signal. This resulted in strong structure being present in the reverberation against which additional processing gain was realised by adaptively matching the filtering applied to the signal and the reverberation. This gain is additional to that predicted by the classical theory, which arises from the reduction in the insonified area of the bottom realised with a high resolution sonar.
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