Estimating hydraulic permeability in dual-porosity–dual-permeability media using joint inversion of electrical resistivity and acoustic data: effective medium theory, surface electrical conductivity and sensitivity analysis (part I)

Abstract This study establishes a link between electrical and acoustic properties using effective medium theory to estimate permeability in porous-fractured media. The proposed method, applicable across diverse geological formations, employs the T-matrix approach to model elastic moduli, electrical conductivity, and hydraulic conductivity within a dual-porosity–dual-permeability framework. The model incorporates micro- and macro-scale structural parameters—including void alignment, concentration, and aspect ratio—while accounting for electrochemical fluid–mineral interactions that influence surface conductivity. A novel concept for tortuosity is introduced, defined as the ratio of the longest electrical flow path along a void’s surface to its axial length in the flow direction. Results show tortuosity decreases along elongating axes but increases perpendicularly. The surface area-to-volume ratio declines with increasing α₁ and α₂ axes but rises with α₃, particularly in micro voids where α₁ expansion sharply reduces the ratio if α₃ is large. Macro voids follow similar trends, with α₃ playing a dominant role. Surface conductivity depends on the interplay between tortuosity and surface area-to-volume ratio, leading to non-universal electrical conductivity trends. Permeability is highly sensitive to α₃: in micro voids, it drops rapidly as α₃ shortens, while macro voids show increased principal permeabilities (κ₁, κ₂) with decreasing α₃ and rising κ₃ with α₃ elongation. Although the model assumes elastic isotropy, void geometry variations induce electrical and hydraulic anisotropy. Acoustic velocities are minimized when α₁ is small and α₂ large (or vice versa), with extreme α₃ values shifting velocity minima to maximal α₁ and α₂. These insights advance predictive capabilities for heterogeneous reservoirs by integrating multi-physical property relationships.

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Publication Details

Journal
Journal of Geophysics and Engineering
Published
2025-09-09
DOI
https://doi.org/10.1093/jge/gxaf120
Citations
1
Primary Topic
Geophysical and Geoelectrical Methods
Type
article
Field-Weighted Citation Impact
1.87
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article

Estimating hydraulic permeability in dual-porosity–dual-permeability media using joint inversion of electrical resistivity and acoustic data: effective medium theory, surface electrical conductivity and sensitivity analysis (part I)

Mohammadfarid Ghasemi, Amir Hossein Javid
1 citations
Journal of Geophysics and Engineering
Geophysical and Geoelectrical Methods
1.87
article

Estimating hydraulic permeability in dual-porosity–dual-permeability media using joint inversion of electrical resistivity and acoustic data: effective medium theory, surface electrical conductivity and sensitivity analysis (part I)

Mohammadfarid Ghasemi, Amir Hossein Javid
article en
1 citations

Abstract

Abstract This study establishes a link between electrical and acoustic properties using effective medium theory to estimate permeability in porous-fractured media. The proposed method, applicable across diverse geological formations, employs the T-matrix approach to model elastic moduli, electrical conductivity, and hydraulic conductivity within a dual-porosity–dual-permeability framework. The model incorporates micro- and macro-scale structural parameters—including void alignment, concentration, and aspect ratio—while accounting for electrochemical fluid–mineral interactions that influence surface conductivity. A novel concept for tortuosity is introduced, defined as the ratio of the longest electrical flow path along a void’s surface to its axial length in the flow direction. Results show tortuosity decreases along elongating axes but increases perpendicularly. The surface area-to-volume ratio declines with increasing α₁ and α₂ axes but rises with α₃, particularly in micro voids where α₁ expansion sharply reduces the ratio if α₃ is large. Macro voids follow similar trends, with α₃ playing a dominant role. Surface conductivity depends on the interplay between tortuosity and surface area-to-volume ratio, leading to non-universal electrical conductivity trends. Permeability is highly sensitive to α₃: in micro voids, it drops rapidly as α₃ shortens, while macro voids show increased principal permeabilities (κ₁, κ₂) with decreasing α₃ and rising κ₃ with α₃ elongation. Although the model assumes elastic isotropy, void geometry variations induce electrical and hydraulic anisotropy. Acoustic velocities are minimized when α₁ is small and α₂ large (or vice versa), with extreme α₃ values shifting velocity minima to maximal α₁ and α₂. These insights advance predictive capabilities for heterogeneous reservoirs by integrating multi-physical property relationships.

Journal of Geophysics and EngineeringVol. 22(6)
University of Houston (US), Shahid Beheshti University (IR)
Openalex Percentile: Top 14%
Geophysical and Geoelectrical Methods
1.87
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