Seismic attenuation due to wave-induced flow
By S. Pride, James G. Berryman, Jerry M. Harris. 2004
789 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/5d43c6154d47d54b37ab12812b379697e3b7ab5a
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In Geophysics
- Roland Martin
- Dimitri Komatitsch
- Abdelaâziz Ezziani
- M. Brajanovski
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- Marcel Frehner
- Holger Steeb
- S. Schmalholz
Citations in the corpus
- P‐wave dispersion and attenuation in fractured and porous reservoirs – poroelasticity approach (2009, background): “The mesoscopic effects are believed to be particularly important at seismic frequencies (Pride et al. 2004).”
- Biot-Rayleigh theory of wave propagation in double-porosity media (2011, methodology): “[40] Pride et al [2004] approximated the double‐porosity equations by an effective single‐porosity equation.”
- Physics and Seismic Modeling for Monitoring CO2 Storage (2006, background): “One of these mechanisms is the mesoscopic loss described by White’s model (WHITE, 1975; CARCIONE et al., 2003a,b; PRIDE et al., 2004).”
- An unsplit convolutional perfectly matched layer improved at grazing incidence for seismic wave propagation in poroelastic media (2008, methodology): “…in storage applies only in the ML layers and not in the main domain and is therefore negligible. or comparison, we also recall the number of arrays needed when no bsorbing conditions are implemented in the finite-difference techique. imes larger than the pore or grain sizes Pride et al., 2004 .”
- Poroelastic finite difference modeling of seismic attenuation and dispersion due to mesoscopic-scale heterogeneity (2007, methodology): “[23] In order to compare the numerical method to the double-porosity theory [e.g., Pride et al., 2004], two series of four numerical experiments have been realized.”
- Quasi-static finite element modeling of seismic attenuation and dispersion due to wave-induced fluid flow in poroelastic media (2011, background): “…provide various closed‐form analytical solutions for seismic attenuation in porous, saturated media with periodic mesoscopic‐ scale heterogeneities of particular geometries, such as layered media or media with spherical inclusions [e.g., Johnson, 2001; Pride et al., 2004; Vogelaar et al., 2010].”