Technical Papers
Jun 23, 2023

Kinematical Analysis of 3D Seismic Stability of Slopes in Unsaturated and Inhomogeneous Soils Using a Pseudodynamic Method

Publication: International Journal of Geomechanics
Volume 23, Issue 9

Abstract

Earthquakes are recognized as one of the main causes of slope instability. Hence, assessment of slope seismic stability has attracted considerable attention from researchers. However, most studies currently focus on the seismic stability of dry or saturated homogeneous slopes and do not consider the spatial and time effect of the seismic waves. To fill this gap, under the framework of kinematical approach of limit analysis, this paper presents an analytical procedure for assessing the three-dimensional seismic stability of slopes in unsaturated and inhomogeneous soils, in which the variations in suction and effective unit weight profiles of soil were considered, and the soil cohesion was assumed to increase linearly with depth. A pseudodynamic approach was employed to take the dynamic characteristics of seismic waves into account. The expression of the factor of safety (Fs) for the slope was derived by the energy balance equation combined with the gravity increase method, and the minimum of Fs was optimized by a genetic algorithm. The methodology was well demonstrated by comparing the results with previous solutions and numerical simulations. Parametric analysis revealed that the sensitivity of slope stability with earthquake intensity becomes smaller with the increase in infiltration rate, whereas this does not vary with soil inhomogeneity. The enhancement of seismic intensity significantly weakens the influence of suction and soil inhomogeneity on slope stability. The soil amplification factor poses a great impact on Fs, especially for higher horizontal seismic coefficient and infiltration rates, while the effects of the shaking period and wave velocity are very small.

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Acknowledgments

The authors would like to thank the editor and the anonymous reviewers for their valuable suggestions to improve this paper. This work was supported by the National Natural Science Foundation of China (Grant No. 41807295). The financial support is greatly appreciated.

Notation

The following symbols are used in this paper:
ah
horizontal seismic acceleration;
ah0
horizontal seismic acceleration at the slope base;
B
maximum width of the rotational failure mechanism;
b
width of “plane-insert” block;
Bmax
maximum width of the 3D horn failure part;
capp
apparent cohesion;
c0, cf, and cs
effective cohesion strength of the slope base, slope face, and slip surface, respectively;
c3D and c2D
effective cohesion stress in 3D horn failure part and plane-insert failure part of the slope, respectively;
Dc-horn and Dc-insert
rate of the internal energy dissipation of 3D horn failure part and plane-insert failure part of slope done by effective soil cohesion, respectively;
Ds-horn and Ds-insert
rate of the internal energy dissipation of 3D horn failure part and plane-insert failure part of slope done by apparent cohesion, respectively;
d1, d2, and d3
distances from the centerline of the conical volume to slope crest, slope face, and slope base, respectively;
d′
distance from the center of the cross section to the water table;
E
Young’s modulus;
fa
amplification factor of soil;
Fs
factor of safety of slope;
g
gravitational acceleration;
Gs
specific gravity of soil;
H
slope height;
H
auxiliary height of slope;
hf and hs
distance from the slope face and slip face to the slope crest, respectively;
kh
horizontal seismic coefficient;
ks
saturated hydraulic conductivity;
N
distance from the toe of the slope to the lowest point on the failure surface;
n
distribution of the soil’s pore size;
nw and nd
pore size distribution parameter of wet path and dry path, respectively;
n0
inhomogeneous coefficient;
q
vertical steady flow rate;
R
radius of the conical volume;
r and r
radius of log-spiral and inner log-spiral, respectively;
r0 and r0
initial radius of log-spiral OA and OA′, respectively;
rh
final radius of the log-spiral;
rm
average radius of the two log-spirals;
rp and rp
radius of log-spiral OP and OP′, respectively;
ru
pore-water coefficient;
S
degree of pore-water saturation;
Se
normalized degree of saturation;
Sr
residual degree of saturation;
St
area of the sliding surface of the slope;
T
shaking period;
t
time;
ua
pore-air pressure;
(uauw)
matric suction;
uw
pore-water pressure;
Vs
shear-wave velocity;
Vus and Vsa
volume of unsaturated and saturated parts in the sliding body, respectively;
We-horn and We-insert
rate of external forces done by seismic force of the 3D horn failure part and plane-insert failure part of slope, respectively;
Wγ-horn and Wγ-insert
rate of external forces done by soil weight of the 3D horn failure part and plane-insert failure part of slope, respectively;
z0
vertical distance from the water table to the slope toe elevation;
z′
distance above the slope toe;
z3D
vertical distance from the any one point of failure block to the water table level;
z2D
vertical distance from the point on the sliding surface of the plane-insert block to the water table level;
α
inverse of air-entry pressure;
αw and αd
inverse of air-entry pressure of wet path and dry path, respectively;
β
slope inclination angle;
β
auxiliary slope inclination angle;
γ
effective soil unit weight;
γsat
unit weight of saturated soil;
γw
unit weight of water;
σ
total stress;
σ
effective stress;
σs
suction stress;
ϕ
effective internal friction angle;
ξ
damping ratio of soils;
μ
Poisson’s ratio;
λs
wavelength of the shear wave;
τf
shear strength;
θ
rotational angle;
θ0
initial rotational angle;
θB and θC
rotational angles from horizontal line to the line passing through point B and C, respectively;
θh
final rotational angle of log-spiral; and
θpandθp
rotational angles from horizontal line to the line passing through point P and P′, respectively.

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International Journal of Geomechanics
Volume 23Issue 9September 2023

History

Received: Jul 19, 2022
Accepted: Mar 26, 2023
Published online: Jun 23, 2023
Published in print: Sep 1, 2023
Discussion open until: Nov 23, 2023

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Associate Professor, School of Civil Engineering and Mechanics, Yanshan Univ., Qinhuangdao, Hebei 066004, China; Key Laboratory of Green Construction and Intelligent Maintenance for Civil Engineering of Hebei Province, Yanshan Univ., Qinhuangdao, Hebei 066004, China (corresponding author). Email: [email protected]
Master’s Student, School of Civil Engineering and Mechanics, Yanshan Univ., Qinhuangdao, Hebei 066004, China; Key Laboratory of Green Construction and Intelligent Maintenance for Civil Engineering of Hebei Province, Yanshan Univ., Qinhuangdao, Hebei 066004, China. ORCID: https://orcid.org/0000-0002-8047-3996. Email: [email protected]
Associate Professor, School of Civil Engineering and Mechanics, Yanshan Univ., Qinhuangdao, Hebei 066004, China; Key Laboratory of Green Construction and Intelligent Maintenance for Civil Engineering of Hebei Province, Yanshan Univ., Qinhuangdao, Hebei 066004, China. Email: [email protected]

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  • Three-Dimensional Active and Passive Seismic Stability Analysis of Shallow Shield Tunnel Faces, International Journal of Geomechanics, 10.1061/IJGNAI.GMENG-9711, 24, 10, (2024).

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