Technical Papers
Feb 2, 2022

Effect of Contact Areas on Seepage Behavior in Rough Fractures under Normal Stress

Publication: International Journal of Geomechanics
Volume 22, Issue 4

Abstract

The investigation of fluid flow in fractured rocks is a key issue in underground engineering. Three sandstone specimens with different roughnesses were generated by Brazilian splitting, and the geometric morphology and aperture distribution of specimens were obtained by three-dimensional scanning technology. Fractal dimension was introduced to characterize the roughness of fractures. Seepage experiments in rough fractures were conducted to analyze the influence of fractal dimension and contact ratio on the nonlinear flow behavior subjected to different normal stresses, which proves that the Forchheimer equation can better describe the flow nonlinearity. A modified Bandis model was proposed to calculate the max normal compression displacement of fracture under normal stress. Subsequently, a new model was developed to forecast the nonlinear coefficient based on fractal dimension and contact ratio. Moreover, a semiempirical equation was established to describe the critical Reynolds number. The influence of contact areas on the seepage path was simulated by COMSOL.

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Acknowledgments

The research was financially supported by the National Natural Science Foundation of China No. 51779021 and the Fundamental Research Funds for the Central Universities No. 2020CDCGJ021.

Notation

The following symbols are used in this paper:
em
average aperture of fracture (m);
σf
standard deviation of fracture aperture;
γ(x, l)
semivariogram (m2);
Z(xi)
heights of the profile at point ith (m);
l
space of the adjacent points of the baseline (m);
Kv
proportionality constant;
H
Hurst exponent;
Dv
fractal dimension;
Z2
root-mean square roughness (m);
Δu
normal displacement (m);
σn
normal stress (Pa);
kn0
normal stiffness of fracture (Pa/m);
umax
maximum compression displacement of fracture (m);
λ, f, m, n, p
dimensionless coefficient;
eij, eij
fracture aperture (m);
er
residual aperture (m);
eh
equivalent hydraulic aperture (m);
c
contact ratio;
Nc
number of contact elements of rough fracture;
NT
total elements of rough fracture;
P
pressure gradient (Pa/m);
Q
discharge at the exit of fracture (m3/s);
A
linear coefficients (kg · m−5 · s−1);
B
nonlinear coefficients (kg · m−8);
ρ
fluid density (kg/m3);
w
fracture width (m);
β
non-Darcy coefficient (1/m);
μ
dynamic viscosity (Pa · s);
Re
Reynolds number;
Rec
critical Reynolds number;
νf
average velocity of the fluid (m/s);
E
non-Darcy effect factor;
ξ
fracture peak asperity (m);
h
water head of the fluid (m);
g
gravitational acceleration (m/s2);
As
cross-sectional area (m2);
K
equivalent permeability (m2); and
L
height of specimen (m).

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 22Issue 4April 2022

History

Received: May 10, 2021
Accepted: Nov 28, 2021
Published online: Feb 2, 2022
Published in print: Apr 1, 2022
Discussion open until: Jul 2, 2022

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Ph.D. Candidate, School of Civil Engineering, Chongqing Univ., Chongqing 400045, China. Email: [email protected]
Professor, School of Civil Engineering, Chongqing Univ., Chongqing 400045, China (corresponding author). ORCID: https://orcid.org/0000-0001-6021-9475. Email: [email protected]
Master’s Degree Candidate, School of Civil Engineering, Chongqing Univ., Chongqing 400045, China. Email: [email protected]
Master’s Degree Candidate, School of Civil Engineering, Chongqing Univ., Chongqing 400045, China. Email: [email protected]
Shihao Qiao [email protected]
Master’s Degree Candidate, School of Civil Engineering, Chongqing Univ., Chongqing 400045, China. Email: [email protected]

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