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EXPERIMENTAL ANALYSIS OF BOTTOM-SEISMIC AND HYDROACOUSTIC SIGNALS GENERATED BY RIVER BOATS

机译:河船产生的底部地震和水声信号的实验分析

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Hydroacoustic and bottom-seismic signals generated by river motor boats moving along the river are recorded experimentally. Hydroacoustic signals are recorded in water at a distance of several meters from the river bank, whereas bottom-seismic signals are recorded close to the water boundary where dry sand is the natural continuation of the river bottom. Main attention is paid to analysis of seismic oscillations, since hydroacoustic noise caused by a river boat has been actively discussed in literature. Several spectra of bottom-seismic and hydroacoustic signals of a moving boat are presented to illustrate the report. Absolute values of principal components of the spectra and the general level of bottom-seismic signals recorded at distances less than the first hundreds of meters from the source are measured. The spectral peculiarities have demonstrated principal distinctions between seismic and hydroacoustic signals. Models of seismo-acoustic field radiation in several spectral windows, based on the analysis of the obtained spectral characteristics, are proposed. Data of the analysis can be of interest in study of physical mechanisms of noise caused by river navigation. They can be also useful for the development and improvement of environmental monitoring methods and for control of ecological situation near rivers.
机译:实验记录了沿河行驶的河上摩托艇产生的水声和底震信号。水声信号记录在距河岸几米处的水中,而底震信号记录在靠近水边界的位置,那里的干砂是河底的自然延续。由于在文献中已积极讨论了由河船引起的水声噪声,因此主要关注地震振荡的分析。提出了移动船的底部地震和水声信号的几个频谱来说明该报告。测量频谱主成分的绝对值和在距震源不到前几百米的距离处记录的底部地震信号的一般水平。频谱特性已经证明了地震信号和水声信号之间的主要区别。在对获得的频谱特征进行分析的基础上,提出了在几个频谱窗口中的地震声场辐射模型。分析的数据可能对研究河流航行引起的噪声的物理机制感兴趣。它们还可用于开发和改善环境监测方法以及控制河流附近的生态状况。

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