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METHOD OF DETERMINING COEFFICIENT OF DISPERSING ACOUSTIC WAVES BY OCEAN BOTTOM

机译:海洋底部测定分散声波系数的方法

摘要

FIELD: hydroacoustic measurements. SUBSTANCE: method of determining coefficient of dispersing acoustic waves by bottom of ocean is based on directed reception of an acoustic field by a moving submerged apparatus and on evaluation of reflection coefficient of sound from the bottom of ocean. The method comprises steps of using as acoustic field dynamic noise of ocean, being swell with force of two or more; performing three- dimension filtering of that noise with use of four-channel reception tract; simultaneously converting the ocean noise, had been received, to energy spectra at outputs of four reception channels; determining before- hand energy spectra of own noises of a receiving antenna of the submerged apparatus, being moved with the same speed as upon measuring the dispersion coefficient at outputs of the same receiving channels; then according to data, had been received, determining the coefficient of dispersing sound by bottom of ocean. EFFECT: enhanced accuracy of metering the coefficient of dispersion of sound by ocean bottom. 3 cl, 2 dwg
机译:领域:水声测量。物质:确定通过海底传播声波的系数的方法是基于移动的水下设备对声场的直接接收,以及对来自海底的声音反射系数的评估。该方法包括以下步骤:将以两个或更多个力膨胀的海洋动态噪声用作声场;使用四通道接收通道对该噪声进行三维滤波;同时将已接收到的海洋噪声转换为四个接收通道输出处的能谱;预先确定浸没设备的接收天线自身噪声的能谱,其移动速度与在相同接收信道的输出端测量色散系数时的移动速度相同;然后根据数据,已经接收到,确定了海底传播声音的系数。效果:增强了测量海底声音扩散系数的准确性。 3厘升,2载重吨

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