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Acoustic signals in air and water generated by very shallow marine seismic sources: An experimental study

机译:通过非常浅的海洋地震来源产生的空气和水中的声学信号:实验研究

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摘要

When a marine seismic source, like an airgun, is fired close to the water surface the oscillating bubble interacts with the water-air interface. The main interest for seismic applications is how this effect impacts the acoustic signal propagating into the water. It is known that the sound transmission into air is abnormally strong when the sound source is very close to the sea surface relative to the emitted wavelength. Detailed insight into how the acoustic signal changes when the source depth is changed is useful in seismic data analysis and processing. Two experiments are conducted in a water tank with two different types of seismic sources. In experiment A the source is a small cavity that is sufficiently far away from the water-air interface so that it can be assumed that no interaction between the cavity and water surface occurs. In experiment B the source is a larger air bubble that is very close to the water-air interface, and hence interaction between the bubble and water surface occurs. The effects on the water surface, oscillating bubble, and emitted acoustic pressure into air are discussed. It is demonstrated that the moving surface contributes significantly to the acoustic signal measured in air.
机译:当海洋地震源类似于气枪时,靠近水面,振荡气泡与水 - 空气接口相互作用。地震应用的主要兴趣是这种效果如何影响传播到水中的声学信号。众所周知,当声源相对于发射波长非常靠近海面时,声音传递异常强。详细了解声学信号如何在源深度改变时如何变化,可用于地震数据分析和处理。在具有两种不同类型的地震源的水箱中进行两次实验。在实验中,源极是一个小腔,其远离水 - 空气界面,使得可以假设腔和水表面之间没有相互作用。在实验B中,源是较大的气泡,其非常接近水 - 空气界面,因此发生气泡和水面之间的相互作用。讨论了对水面,振荡气泡和发射声压入空气的影响。证明移动表面显着贡献到空气中测量的声学信号。

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