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声波在过渡区楔形海域的传播特性研究
引用本文:史永臣,姜冠亭,杨士莪. 声波在过渡区楔形海域的传播特性研究[J]. 黑龙江大学自然科学学报, 2001, 18(1): 50-53
作者姓名:史永臣  姜冠亭  杨士莪
作者单位:1. 黑龙江八一农垦大学基础部,
2. 中国科学院声学研究所,
3. 哈尔滨工程大学水声工程系,
摘    要:声波在海洋中传播的特性,历来都是水声学一个极其重要的问题,本文通过模拟一个典型的楔形海底地形,用三维射线模型计算了声波在该海域传播的方向特性,计算结果指出,在海底倾角较大的海区,声线具有明显的水平折射,这种水平折射的效应,用于声源定位时必须予以修正。本文提出了一种简便易行的修正水平折射的方法。该结论对于水下目标定位具有重要的指导意义。

关 键 词:声波  楔形海域  水平折射
文章编号:1001-7011(2001)01-0050-04
修稿时间:2000-12-05

A research on characteristic of sound propagation in complicated bottom ocean
SHI Yong-chen,JIANG Guan-ting,YANG Shi-e. A research on characteristic of sound propagation in complicated bottom ocean[J]. Journal of Natural Science of Heilongjiang University, 2001, 18(1): 50-53
Authors:SHI Yong-chen  JIANG Guan-ting  YANG Shi-e
Abstract:Almost all of the sound rays will touch the bottom in shallow sea. So it is very important to research the characteristic of sea bed, especially its absorption and its contour reflection. A ray trace theory was discussed and applied to calculate sound trace and its loss. The best advantage of this method is its clear ray physical photo and its short calculating time.The result revealed, in shallow sea, the bottom mountains will remarkably influence sound transmission and made its intensity lower than flat bottom. At the same time, above the rest of the mountain, an additional convergence zone will be formed.
Keywords:sound wave   wedge sea area   level refraction
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