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At-sea Observation and Theoretical Simulation on Very-low-frequency Sound Propagation in Shallow Water

机译:浅水中非常低频声音传播的海上观察与理论模拟

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A very-low-frequency (VLF) sound propagation experiment with a reflective and refractive wide-angle Ocean Bottom Seismometer (OBS) and a large volume air-gun was conducted across the northeastern continental margin of the South China Sea (SCS). With air-gun shot spacing of approximately 190 m, high-quality Scholte wave data was recorded by the horizontal and vertical geophones of OBS within 0.4-6 km offset. At least four modal phase-velocity dispersion curves of Scholte waves in the frequency band of 1.2-3 Hz were extracted from common receiver gathers (CRGs) using phase-shift method. We retrieved the first three higher modes from the horizontal component, and the fundamental and the first higher mode can be extracted from the vertical component, but no Scholte wave was found on the hydrophone. The dispersion results show that the phase velocity of the fundamental Scholte wave varies from 240 m/s to 400 m/s, and the phase velocity of the higher order of Scholte waves vary from 400 m/s to 1000 m/s.
机译:一种非常低频(VLF)声音传播实验,具有反射和屈光广角海底地震计(OBS)和大批量气枪在南海(SCS)的东北大陆边缘进行。带气枪射击间距约为190米,高质量的学者波浪数据被OBS的水平和垂直地震检波器记录在0.4-6 km偏移量内。使用相移法从公共接收器聚集(CRG)中提取至少四个频带中的学者波的模态相位速度分散曲线。我们从水平分量检索了前三种更高模式,并且可以从垂直分量中提取基本和第一更高模式,但在水中没有发现学者波浪。分散结果表明,基本学者波的相速度从240米/秒变化到400米/秒,学者波浪高阶的相位速度从400米/秒变化到1000米/秒。

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