摘要
海底作为声波在水中传播的下边界,其声学特性对水中声场分布的影响巨大。在近60年的研究中,海底沉积物的声学特性建模研究已取得众多成果,然而这些成果还远远不能满足现代化水声技术发展的要求。文章从基本的海底结构组成出发,在海底地声建模的基础上揭示出声波与海底的作用关系。
The seabed is the lowest boundary of sound propagation in the sea, so its acous-tic characteristics have a major effect on the sound field distribution. In the last sixty years, model-ing of the acoustic properties of seabed sediment has made much progress; however, it still does not satisfy the demands of modern underwater acoustic technology. In this article, based on the composition of the seabed, we present a geoacoustic model to describe the interaction of sound waves with the seabed.
出处
《物理》
CAS
北大核心
2014年第11期717-722,共6页
Physics
基金
国家自然科学基金(批准号:10774156
11374323)资助项目
关键词
沉积层
地声建模
声速
密度
衰减
sediment
geoacoustic model
velocity
density
attenuation