Detailed information about the sediment properties and 
microstructure can be provided through the analysis of 
digital ultrasonic P-waveforms recorded automatically 
during full waveform core logging. The physical parameter 
which predominantly affects the elastic wave propagation 
in water-saturated sediments is the P-wave attenuation 
coefficient. The related sedimentological parameter is the 
grain size distribution. A set of high-resolution 
ultrasonic transmission seismograms (50-500 kHz), which 
indicate downcore variations in the grain size by their 
signal shape and frequency content, are presented. Layers 
of coarse-grained foraminiferal ooze can be identified by 
highly attenuated P-waves, whereas almost unattenuated 
waves are recorded in fine-grained areas of nannofossil 
ooze. Color-encoded pixel graphics of the seismograms and 
instantaneous frequencies present full waveform images of 
the lithology and attenuation. A modified spectral 
difference method is introduced to determine the 
attenuation coefficient and its power law 
. 
Applied to synthetic seismograms derived using a 'constant 
Q' model, even low attenuation coefficients can be 
quantified. A downcore analysis gives an attenuation log 
which ranges from 700 dB/m at 400 kHz and a power of 
n = 1.0 - 2 in coarse-grained sands to few decibels per 
metre and n < 0.5 in fine-grained clays. A least-squares 
fit of a second degree polynomial describes the mutual 
relationship between the mean grain size and the 
attenuation coefficient. When it is used to predict the 
mean grain size, an almost perfect coincidence with the 
values derived from sedimentological measurements is 
achieved.
AGU Index Terms: 3094 Instruments and techniques; 5144 Wave attenuation; 5102 Acoustic properties; 3099 General or miscellaneous
Keywords/Free Terms: Marine geophysics, physical properties of sediment cores, full waveform core logging, P-wave attenuation and grain sizes.
JGR-Solid Earth 96JB01891