Articles | Volume 10, issue 4
https://doi.org/10.5194/se-10-1321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-10-1321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Aug 2019
Research article |
| 08 Aug 2019
| 08 Aug 2019
Seismic attenuation and dispersion in poroelastic media with fractures of variable aperture distributions
Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland
Nicolás D. Barbosa
Department of Earth Sciences, University of Geneva, Geneva, Switzerland
J. Germán Rubino
CONICET, Centro Atómico Bariloche – CNEA, San Carlos de Bariloche, Argentina
Beatriz Quintal
Institute of Earth Sciences, University of Lausanne, Lausanne, Switzerland
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Cited
17 citations as recorded by crossref.
- Attenuation and dispersion of P-waves in fluid-saturated porous rocks with a distribution of coplanar cracks — Scattering approach Y. Song et al. 10.1190/geo2020-0281.1
- Fluid Pressure Diffusion in Fractured Media: The Role Played by the Geometry of Real Fractures S. Lissa et al. 10.1029/2021JB022233
- Squirt Flow in Cracks with Rough Walls S. Lissa et al. 10.1029/2019JB019235
- Impact of poroelastic effects on the inversion of fracture properties from amplitude variation with offset and azimuth data in horizontal transversely isotropic media N. Barbosa et al. 10.1190/geo2019-0475.1
- Numerical Upscaling of Seismic Signatures of Poroelastic Rocks Containing Mesoscopic Fluid‐Saturated Voids Y. He et al. 10.1029/2021JB023473
- Effects of Acoustic Stimulation on Fluid Flow in Porous Media S. Khasi et al. 10.1021/acs.energyfuels.1c02631
- Sensitivity of seismic attenuation and dispersion to dynamic elastic interactions of connected fractures: Quasi-static finite element modeling study Y. He et al. 10.1016/j.petsci.2022.08.024
- Effective elastic properties of fractured rocks considering fracture interactions J. Guo & B. Fu 10.1111/1365-2478.13632
- Fracture Unclogging: A Numerical Study of Seismically Induced Viscous Shear Stresses in Fluid‐Saturated Fractured Rocks N. Barbosa et al. 10.1029/2019JB017984
- Anisotropic Effective Elastic Properties for Multi-Dimensional Fractured Models S. Jian et al. 10.3390/app12041873
- Stress Relaxing Simulation on Digital Rock: Characterize Attenuation Due To Wave‐Induced Fluid Flow and Scattering W. Zhu et al. 10.1029/2022JB024850
- Frequency‐Dependent P Wave Anisotropy Due to Wave‐Induced Fluid Flow and Elastic Scattering in a Fluid‐Saturated Porous Medium With Aligned Fractures J. Guo & B. Gurevich 10.1029/2020JB020320
- P-wave attenuation and dispersion in a fluid-saturated rock with aligned rectangular cracks Y. Song et al. 10.1016/j.mechmat.2020.103409
- Mechanical Compliance of Individual Fractures in a Heterogeneous Rock Mass From Production‐Type Full‐Waveform Sonic Data Z. Zhou et al. 10.1029/2022JB024302
- Azimuth-, angle- and frequency-dependent seismic velocities of cracked rocks due to squirt flow Y. Alkhimenkov et al. 10.5194/se-11-855-2020
- 3D finite-element modeling of effective elastic properties for fracture density and multiscale natural fractures S. Jian et al. 10.1093/jge/gxab036
- An improved wave equation of fractured-porous media for predicting reservoir permeability W. Zhao et al. 10.3389/feart.2023.1269616
16 citations as recorded by crossref.
- Attenuation and dispersion of P-waves in fluid-saturated porous rocks with a distribution of coplanar cracks — Scattering approach Y. Song et al. 10.1190/geo2020-0281.1
- Fluid Pressure Diffusion in Fractured Media: The Role Played by the Geometry of Real Fractures S. Lissa et al. 10.1029/2021JB022233
- Squirt Flow in Cracks with Rough Walls S. Lissa et al. 10.1029/2019JB019235
- Impact of poroelastic effects on the inversion of fracture properties from amplitude variation with offset and azimuth data in horizontal transversely isotropic media N. Barbosa et al. 10.1190/geo2019-0475.1
- Numerical Upscaling of Seismic Signatures of Poroelastic Rocks Containing Mesoscopic Fluid‐Saturated Voids Y. He et al. 10.1029/2021JB023473
- Effects of Acoustic Stimulation on Fluid Flow in Porous Media S. Khasi et al. 10.1021/acs.energyfuels.1c02631
- Sensitivity of seismic attenuation and dispersion to dynamic elastic interactions of connected fractures: Quasi-static finite element modeling study Y. He et al. 10.1016/j.petsci.2022.08.024
- Effective elastic properties of fractured rocks considering fracture interactions J. Guo & B. Fu 10.1111/1365-2478.13632
- Fracture Unclogging: A Numerical Study of Seismically Induced Viscous Shear Stresses in Fluid‐Saturated Fractured Rocks N. Barbosa et al. 10.1029/2019JB017984
- Anisotropic Effective Elastic Properties for Multi-Dimensional Fractured Models S. Jian et al. 10.3390/app12041873
- Stress Relaxing Simulation on Digital Rock: Characterize Attenuation Due To Wave‐Induced Fluid Flow and Scattering W. Zhu et al. 10.1029/2022JB024850
- Frequency‐Dependent P Wave Anisotropy Due to Wave‐Induced Fluid Flow and Elastic Scattering in a Fluid‐Saturated Porous Medium With Aligned Fractures J. Guo & B. Gurevich 10.1029/2020JB020320
- P-wave attenuation and dispersion in a fluid-saturated rock with aligned rectangular cracks Y. Song et al. 10.1016/j.mechmat.2020.103409
- Mechanical Compliance of Individual Fractures in a Heterogeneous Rock Mass From Production‐Type Full‐Waveform Sonic Data Z. Zhou et al. 10.1029/2022JB024302
- Azimuth-, angle- and frequency-dependent seismic velocities of cracked rocks due to squirt flow Y. Alkhimenkov et al. 10.5194/se-11-855-2020
- 3D finite-element modeling of effective elastic properties for fracture density and multiscale natural fractures S. Jian et al. 10.1093/jge/gxab036
1 citations as recorded by crossref.
Discussed (preprint)
Latest update: 04 Nov 2024
Short summary
We quantify the effects that 3-D fractures with realistic distributions of aperture have on seismic wave attenuation and velocity dispersion. Attenuation and dispersion are caused by fluid pressure diffusion between the fractures and the porous background. We show that (i) both an increase in the density of contact areas and a decrease in their correlation length reduce attenuation and (ii) a simple planar fracture can be used to emulate the seismic response of realistic fracture models.
We quantify the effects that 3-D fractures with realistic distributions of aperture have on...
