Effect of the sound velocity stratification in the bottom sediment layer on the diffraction focusing of an acoustic field in a shallow sea

被引:2
|
作者
Borodina, EL [1 ]
Petukhov, YV [1 ]
机构
[1] Russian Acad Sci, Inst Appl Phys, Nizhnii Novgorod 603600, Russia
基金
俄罗斯基础研究基金会;
关键词
D O I
10.1134/1.1507194
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
It is shown that an increase in the sound velocity gradient in the bottom sediment layer results in the formation of additional zones of diffraction focusing of the acoustic field generated by a vertical line array in the water layer. It is also established that, depending on the sound velocity step at the upper boundary of the sediment layer, the diffraction focusing of the acoustic field in the main focusing zones can be enhanced or reduced. (C) 2002 MAIK "NaukalInterperiodica".
引用
收藏
页码:529 / 534
页数:6
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