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This document discusses a theoretical model developed by Michael J. Buckingham for wave propagation in marine sediments, focusing on compressional and shear wave properties. The model, based on grain-to-grain interactions, accurately predicts the phase speed and attenuation of these waves using three macroscopic physical variables: porosity, grain size, and sediment depth, without adjustable parameters. The findings demonstrate that knowing one sediment property allows for reliable estimation of others, wit

Author

Nam Le

Language

EN