Proceedings of Meetings on Acoustics

نویسنده

  • Nicholas Chotiros
چکیده

As the sand grain size approaches the acoustic wavelength, the underwater backscattering strength increases. Laboratory measurements show that the shallow-grazing angle backscattering strength increases as the third power of the normalized grain diameter, until it reaches a saturation level. In this regime, it has been shown that the attenuation of the sound in the sand increases as the fourth power of frequency and the speed of sound decreases with increasing frequency. The most likely explanation for the attenuation and speed dispersion is multiple scattering [Schwartz and Plona, Journal of Applied Physics, vol. 55, 1984, and Kimura, J. Acoust. Soc. Am. EL, vol. 129, 2011]. The multiple scattering model is applied to the backscattering process, and it is shown to be consistent with the published backscattering data. [Work supported by the Office of Naval Research, Ocean Acoustics Program].

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تاریخ انتشار 2013