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Journal of Porous Media
IF: 1.49 5-Year IF: 1.159 SJR: 0.43 SNIP: 0.671 CiteScore™: 1.58

ISSN Print: 1091-028X
ISSN Online: 1934-0508

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Journal of Porous Media

DOI: 10.1615/JPorMedia.2018021864
pages 447-466


Khemraj Shukla
Boone Pickens School of Geology, 105 Noble Research Center, Oklahoma State University, Stillwater, OK, 74078
José M. Carcione
Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42c, 34010 Sgonico, Trieste, Italy; School of Earth Science and Technology, Hohai University, Nanjing, 211100, China
Priyank Jaiswal
Boone Pickens School of Geology, 105 Noble Research Center, Oklahoma State University, Stillwater, OK, 74078
Juan Enrique Santos
CONICET, Instituto del Gas y del Petróleo, Facultad de Ingeniería, Universidad de Buenos Aires, Av. Las Heras 2214 Piso 3, C1127AAR Buenos Aires, Argentina; Department of Mathematics, Purdue University, 150 N. University Street, West Lafayette, Indiana, 47907-2067, USA; Universidad Nacional de La Plata, Argentina
Jing Ba
School of Earth Science and Technology, Hohai University, Nanjing, 211100, China


Biot's theory allows incorporation of permeability and viscosity in computing seismic amplitudes for a porous medium that is fully saturated with a single-phase fluid. In its original form, Biot's theory does not explicitly account for capillary effects; for example, the surface tension between the wetting and nonwetting fluids. This paper uses a model to quantify capillary effects on velocity and attenuation. Studies that have attempted to extend Biot's poroelasticity to include capillary effects found changes in fast P-wave velocity of up to 5% between the sonic and ultrasonic frequency ranges. Simulations of wave propagation at varying capillary pressure in a rock saturated with multiphase fluid are also presented. The poroelastic equation for multiphase fluid is solved by using spectral methods with Fourier grids as collocations points in space and the Runge-Kutta scheme for numerical integration. The numerical simulations show the presence of three compressional (P)-waves, one fast and two slow compressional waves corresponding to the wetting and nonwetting phases. The results show that the slow P-wave amplitude is significantly affected by capillary pressure variations.


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