首页> 外文期刊>The Journal of the Acoustical Society of America >Synthetic array measurements of acoustical waves propagating into a water-saturated sandy bottom for a smoothed and a roughened interface
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Synthetic array measurements of acoustical waves propagating into a water-saturated sandy bottom for a smoothed and a roughened interface

机译:传播到水饱和沙质底部中的声波的合成阵列测量,以实现平滑和粗糙的界面

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摘要

Measurements of acoustical waves propagating in an unconsolidated water-saturated porous medium that involved the use of a two-dimensional synthetic array technique are presented. From these measurements, wave-front propagation is evaluated using time domain, wave-number frequency and two-dimensional spatial analysis techniques. First, a synthetic array measurement is employed to study sound penetration for a "smoothed" interface condition. This smoothed interface measurement is then compared to an identical synthetic array measurement with a "roughened" interface. A comparison of the smoothed and roughened interface measurements shows enhanced bottom penetration at shallow grazing angles as a result of the roughened interface. At shallow grazing angles, this scattered pressure from the roughened interface has the appearance of a wave front in the water-saturated porous medium that has a virtual wave speed of ~1200 m/s. Slower compressional waves in the sandy bottom are not observed.
机译:提出了测量声波在非固结水饱和多孔介质中传播的方法,涉及使用二维合成阵列技术。通过这些测量,可以使用时域,波数频率和二维空间分析技术评估波前传播。首先,采用合成阵列测量来研究“平滑”界面条件下的声音穿透。然后将此平滑的界面测量结果与具有“粗糙”界面的相同合成阵列测量结果进行比较。平滑和粗糙界面测量的比较表明,由于粗糙界面,在浅掠角处的底部穿透性增强。在较浅的掠射角处,来自粗糙界面的分散压力在水饱和的多孔介质中具有波前的外观,其波速约为1200 m / s。在沙质底部没有观察到较慢的压缩波。

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