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Chirp sonar sediment characterization at the northern gulf of Mexico littoral acoustic demonstration center experimental site

机译:墨西哥北湾的Chirp Sonar沉积物表征沿海廊道声学演示中心实验遗址

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Chirp sonar subottom surveys have been conducted during a recent Littoral Acoustic Demonstration Center (LADC) experiment to invert bottom geoacoustic properties in the Northern Gulf of Mexico. Sediment properties such as density, porosity, and sound-speed profiles are inverted by using reflection amplitude and phase data obtained from a shallow-towed 2-12 kHz chirp sonar. High-quality subbottom images have been obtained with sub-meter resolution and up to 60 m penetration resolving several seafloor fault and diapir systems in the area. The attenuation coefficient is also estimated using the frequency shift method that seems to be relatively insensitive to reflection and transmission effects. The sound-speed and density structures of the LADC acoustic propagation tracks are efficiently mapped and made available for the numerical simulation studies of ambient noise and marine mammal acoustic propagation. The inversion results compare favorably with the previously reported sediment core data indicating that an accurate and rapid estimation of acoustical and physical properties of marine sediments is feasible.
机译:在最近的沿海声学示范中心(LADC)实验期间已经进行了Chirp Sonar概述调查,以颠覆墨西哥北部的底地理声学特性。通过使用从浅拖曳2-12kHz Chirp Sonar获得的反射幅度和相位数据,反转沉积物等沉积物特性。已经用亚米分辨率获得了高质量的亚副斑块图像,可在该地区的几个海底故障和尾随系统分辨出高达60米的渗透。还使用似乎对反射和传输效果相对不敏感的频移方法来估计衰减系数。 LADC声学传播轨道的声速和密度结构是有效的,可用于环境噪声和海洋哺乳动物声学传播的数值模拟研究。反演结果与先前报告的沉积物核心数据相比,表明海洋沉积物的声学和物理性质的准确和快速估计是可行的。

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