Abstract
In a previous publication [Richardson, in OceanSeismo-Acoustics (Plenum, New York, 1985), pp. 527–536] the author reviewed relationships between physical and biological processes and the resultant variability of values of sediment geoacoustic (compressional wave velocity and attenuation) and physical (grain size and porosity) properties. In this presentation the subject is revisited, using values of compressional and shear wave velocity measured insitu instead of the laboratory measurements considered in the previous paper.
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