Technical Papers
May 21, 2024

Active and Passive Lateral Earth Pressure with Anisotropic Seepage Effect

Publication: International Journal of Geomechanics
Volume 24, Issue 8

Abstract

This study investigated active and passive lateral earth pressure in the presence of anisotropic seepage conditions. The soil was assumed to be granular and fully saturated. Three methods were used to solve the problem: (1) the upper bound limit analysis method (UBM); (2) upper and lower bound solutions of finite-element limit analysis (FELA); and (3) the stress characteristic method (SCM). The proposed analytical solution for the UBM employed the logarithmic spiral slip surface. The lateral earth pressure coefficients for the active and passive cases were calculated and presented, considering variations in the vertical-to-horizontal hydraulic conductivity ratio, friction angle, and soil–wall interface friction angle. The obtained results for the active and passive cases agree with those of previous studies. The results of the SCM showed that in the presence of seepage, the distribution of stress on the soil–wall interface is nonlinear. In addition, the failure zone obtained from different methods was compared and examined. The failure patterns obtained from the SCM and FELA were almost identical.

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Data Availability Statement

All data that support the findings of this study are available from the corresponding author upon reasonable request.

Notation

The following symbols are used in this paper:
H
height of the wall;
ix
horizontal hydraulic gradient;
iz
vertical hydraulic gradient;
Ka
active lateral earth pressure coefficient;
Kp
passive lateral earth pressure coefficient;
kx
horizontal hydraulic conductivity;
kz
vertical hydraulic conductivity;
Pa
active earth force;
Pp
passive earth force;
p
mean stress;
q
surcharge;
u
pore-water pressure;
WFx
work of the horizontal seepage force;
WFz
work of the vertical seepage force;
Wp
work of the active or passive force;
WW
work of the weight;
X
body and/or inertial forces in the x-direction;
Z
body and/or inertial forces in the z-direction;
z
depth;
δw
soil–wall interface friction angle;
ϕ
soil friction angle;
γ
submerged unit weight;
γ
soil unit weight;
γw
water unit weight;
θ
failure surface inclination angle;
σx
horizontal normal stress;
σz
vertical normal stress;
τxz
shear stress;
ψ
angle between the positive x-axis and the major principal stress; and
ξ
kz/kx.

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 24Issue 8August 2024

History

Received: Jul 6, 2023
Accepted: Feb 5, 2024
Published online: May 21, 2024
Published in print: Aug 1, 2024
Discussion open until: Oct 21, 2024

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Associate Professor, School of Engineering, Persian Gulf Univ., Bushehr 7516913817, Iran (corresponding author). ORCID: https://orcid.org/0000-0002-8951-9233. Email: [email protected]
Fatemeh Khani [email protected]
Graduate Student, School of Engineering, Persian Gulf Univ., Bushehr 7516913817, Iran. Email: [email protected]

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