A seismic-reflection-based approach  for determining the hydraulic permeability  of rocks in a subsurface region

Shapiro, Serge A.

doi:https://doi.org/10.5194/sand-2-77-2023

Articles | Volume 2

https://doi.org/10.5194/sand-2-77-2023

© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/sand-2-77-2023

© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 2

Conference Abstract

|

06 Sep 2023

Conference Abstract |

| 06 Sep 2023

A seismic-reflection-based approach for determining the hydraulic permeability of rocks in a subsurface region

Serge A. Shapiro

Related authors

Statistics of the Seismic Sequence and Rupture Directivity of the M5.5 Earthquake in Orkney, South Africa

Carsten Dinske, Jonas Folesky, Jörn Kummerow, Serge Shapiro, and Hiroshi Ogasawara

Solid Earth Discuss., https://doi.org/10.5194/se-2020-58,https://doi.org/10.5194/se-2020-58, 2020

Publication in SE not foreseen

Short summary

Cited articles

Shapiro, S. A. and Kaselow, A.: Porosity and elastic anisotropy of rocks under tectonic stress and pore-pressure changes, Geophysics, 70, N27–N38, 2005.

Short summary

The hydraulic permeability of rocks characterizes fluid mobility. This quantity is important for various applications. Because of the high resolution and large penetration range of seismic waves as well as the ability of seismic exploration to operate from the Earth's surface, a seismic-reflection-based method for characterizing the underground permeability is of importance. Stress-dependent rock-physics experiments allow one to calibrate seismic data for estimating permeability.