53
Fig. 2.16 Comparison of P-wave attenuation and velocity dispersion data derived from ultrasonic transmission seismograms
with theoretical curves based on Biot-Stoll’s model for six traces of the turbidite layer of gravity core GeoB1510-2.
Permeabilities vary in the model curves according to constant ratios κ/a
2 = 0.030, 0.010, 0.003 (κ = permeability, a = pore size
parameter). The resulting permeabilities are given in each diagram. Modified after Breitzke et al. (1996).
2.5
Sediment Classification
Fig. 2.16 Comparison of P-wave attenuation and velocity dispersion data derived from ultrasonic transmission seismograms
with theoretical curves based on Biot-Stoll’s model for six traces of the turbidite layer of gravity core GeoB1510-2.
Permeabilities vary in the model curves according to constant ratios κ/a
2 = 0.030, 0.010, 0.003 (κ = permeability, a = pore size
parameter). The resulting permeabilities are given in each diagram. Modified after Breitzke et al. (1996).
2.5
Sediment Classification