浅海异地混响理论与实验比较
The comparison of the bistatic reverberation theory and the experiment data in shallow water
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摘要: 在亚洲海国际声学实验(ASIAEX2001)中记录了本地混响和异地混响的实验数据。对数据进行处理时,发现异地混响数据和本地混响数据有较大差异:本地混响衰减和混响垂直相关小于异地混响衰减和垂直相关。为了解释这一现象,根据浅海混响的射线简正波理论,结合三维海底散射模型,给出了浅海异地混响衰减和混响垂直相关的一般表达式。讨论了与本地混响衰减和混响垂直相关的关系,并与实验数据进行了比较。理论计算和实验数据表明:在经过时延(从声源到接收器的传播时间)后,较远距离的异地混响衰减与混响垂直相关可以由本地混响衰减和垂直相关近似表示。Abstract: In ASIAEX2001, the experiment data of monostatic and bistatic reverberation were recorded. There is much difference between the two-experiment data: the monostatic reverberation loss and the vertical correlation are all much less than those of the bistatic. To explain the phenomena, on the basis of ray-mode reverberation theory and three-dimensional scattering model, the expressions of the bistatic reverberation loss and the vertical correlation are put forward. The relations between the monostatic and bistatic reverberation are discussed and compared with the experiment data. The calculation and the experiment data indicate: after a time delay (the transmission time from the source to the receiver), the long-range bistatic reverberation loss and the vertical correlation can be approximately expressed by the monostatic reverberation loss and the vertical correlation.