Journal
GEOPHYSICAL JOURNAL INTERNATIONAL
Volume 216, Issue 3, Pages 2037-2043Publisher
OXFORD UNIV PRESS
DOI: 10.1093/gji/ggy518
Keywords
Wave propagation; Elasticity and anelasticity; Microstructure
Categories
Funding
- UK Natural Environment Research Council [NE/K009656/1, NE/M016471/1]
- NERC [NE/K009656/1, NE/M016471/1] Funding Source: UKRI
Ask authors/readers for more resources
The evolution of the ratio between P- and S-wave velocities (V-P/V-S) with increasing fluid-saturated porosity is computed for isotropic rocks containing spheroidal pores. The ratio V-P/V-S is shown to either decrease or increase with increasing porosity, depending on the aspect ratio alpha of the pores, fluid to solid bulk modulus ratio zeta and Poisson's ratio nu(0) of the solid constituents of the rock. A critical initial Poisson's ratio nu(0, crit) is computed, separating cases where V-P/V-S increases (if nu(0) < nu(0), (crit)) or decreases (if nu(0) > nu(0, crit)) with increasing porosity. For thin cracks and highly compressible fluids, nu(0), (crit) is approximated by 0.157 zeta/alpha, whereas for spherical pores nu(0, crit) is given by 0.2 + 0.8 zeta. When nu(0) is close to nu(0, crit), the evolution of V-P/V-S with increasing fluid-saturated porosity is near neutral and depends on subtle changes in pore shape and fluid properties. This regime is found to be relevant to partially dehydrated serpentinites in subduction zones (porosity of aspect ratio near 0.1 and. in the range 0.01-0.1), and makes detection of these rocks and possibly elevated fluid pressures difficult from V-P/V-S only.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available