Fig. 4From: Simultaneous measurements of elastic wave velocities and electrical conductivity in a brine-saturated granitic rock under confining pressures and their implication for interpretation of geophysical observationsVolumetric strain of dry rock sample AJG07 as a function of confining pressure. The increasing rate in the volumetric strain decreases with increasing confining pressure. The broken line passing two points at 150 and 180 MPa is extrapolated to 0 MPa to give 0.15 % as the lower bound of the crack porosityBack to article page