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