Premium
Wave velocities and attenuation of shaley sandstones as a function of pore pressure and partial saturation
Author(s) -
Pham Nam H.,
Carcione José M.,
Helle Hans B.,
Ursin Bjørn
Publication year - 2002
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1046/j.1365-2478.2002.00343.x
Subject(s) - attenuation , saturation (graph theory) , biot number , geology , permeability (electromagnetism) , porosity , mineralogy , pore water pressure , igneous petrology , porous medium , mechanics , geotechnical engineering , engineering geology , optics , chemistry , physics , seismology , tectonics , biochemistry , mathematics , combinatorics , membrane , volcanism
We obtain the wave velocities and quality factors of clay‐bearing sandstones as a function of pore pressure, frequency and partial saturation. The model is based on a Biot‐type three‐phase theory that considers the coexistence of two solids (sand grains and clay particles) and a fluid mixture. Additional attenuation is described with the constant‐ Q model and viscodynamic functions to model the high‐frequency behaviour. We apply a uniform gas/fluid mixing law that satisfies the Wood and Voigt averages at low and high frequencies, respectively. Pressure effects are accounted for by using an effective stress law. By fitting a permeability model of the Kozeny– Carman type to core data, the model is able to predict wave velocity and attenuation from seismic to ultrasonic frequencies, including the effects of partial saturation. Testing of the model with laboratory data shows good agreement between predictions and measurements.