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- W2023725797 abstract "Shear wave attenuation measurements were made using three different water-saturated sediments. The sediment assemblages used in the attenuation measurements included well-sorted spherical glass beads, a well-sorted angular quartz sand, and a moderately sorted angular quartz sand. The median grain size of the sediments was held constant while the grain shape and size distributions were varied. Sediment physical properties were measured under the same conditions prevailing during the acoustic measurements. The properties were used as inputs to a theoretical attenuation model based on the Biot theory of propagation of waves in porous media. The model allowed attenuation versus frequency predictions to be made for each of the three sediment assemblages over the measurement frequency range of 1–20 kHz. The resultant comparisons between the measured and predicted attenuations demonstrated the importance of using measured model inputs obtained under controlled laboratory conditions when theoretical model capabilities are being evaluated. The model comparisons shed significant light on the ability of this particular model to predict shear wave attenuation in nonideal sediments. [Work supported by NORDA.]" @default.
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- W2023725797 date "1983-11-01" @default.
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- W2023725797 title "A comparison between Biot model predictions and shear wave attenuation measurements in unconsolidated laboratory sediments" @default.
- W2023725797 doi "https://doi.org/10.1121/1.2021046" @default.
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