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The research of deep-sea water scattering strength measurement technology

机译:深海水散射强度测量技术研究

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There are many uneven “water masses”, layers, deep-sea creatures and seabed overflow bubbles in the deep sea. The scattering of incident acoustic waves on these scatterers contributes to the deep sea volume reverberation, and different seasons in different ocean regions contribute variously to scattering and their volume reverberation variesy. A research of volume reverberation in different seas and different times by measuring scattering strength of deep sea water, not only has an important role for performance prediction of active sonar system, but also makes a contribution to a better understanding of the acoustic characteristics of the deep sea. From the composition, classification, and characteristics of the main scatterers in the deep sea, this paper introduces the principle and method of scattering strength measuring, and then describes the composition and implementation of a scattering strength measurement sonar system. The scattering strength of each deep layer is measured by transmitting vertically downwards a narrow beam, and displaying the intensity value of scattering in an acoustic image. The sonar system is composed of transducer arrays, a power amplifier, a signal conditioner, a signal processor, and a sonar server. The system has been tested in the South China Sea, and has been used to measure the scattering strength at different time periods in a certain sea area, the depth of which is between 800 meters to 1400 meters, at a frequency of between 12kHz to 20kHz, when the ship speed was between 2kn to 6kn. Studies reveal that fishs within 100 meters of depth and the deep-sea creatures in the deep scattering layer are the major contributors to the volume reverberation. The deep scattering layer thickness is up to hundreds of meters, and the scatterer has obvious biological behaviour, namely deep during the daytime, and shallow at night. In addition, seabed overflow bubbles are also a kind of scatterer.
机译:深海中有许多不均匀的“水团”,层,深海生物和海床溢流气泡。入射声波在这些散射体上的散射导致深海体积混响,而不同海洋区域中的不同季节对散射的贡献也不同,并且它们的体积混响也各不相同。通过测量深海水的散射强度研究不同海洋和不同时间的体积混响,不仅对主动声纳系统的性能预测具有重要作用,而且有助于更好地理解深海的声学特性海。从深海主要散射体的组成,分类和特点出发,介绍了散射强度测量的原理和方法,然后介绍了散射强度测量声纳系统的组成和实现。每个深层的散射强度是通过垂直向下传播窄光束并在声像中显示散射强度值来测量的。声纳系统由换能器阵列,功率放大器,信号调节器,信号处理器和声纳服务器组成。该系统已在南中国海进行了测试,并已用于测量特定海域不同时间段的散射强度,该海域的深度在800米至1400米之间,频率在12kHz至20kHz之间,当时船速在2kn至6kn之间。研究表明,深度在100米以内的鱼类和深层散射层中的深海生物是造成体积混响的主要因素。深散射层厚度可达数百米,散射体具有明显的生物学行为,即白天较深,夜间较浅。此外,海底溢流气泡也是一种散射体。

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