Technical Papers
Dec 27, 2022

Pseudodynamic Analysis of Three-Dimensional Fissured Slopes Reinforced with Piles

Publication: International Journal of Geomechanics
Volume 23, Issue 3

Abstract

Cracks broadly exist within slopes due to desiccation, weathering, or wetting–drying cycles in Nature. The presence of cracks inevitably reduces slope stability. However, such fissured slopes have received little attention, especially when subject to earthquake action, which is considered one of the most significant inducements of slope instability. In practice, antislide piles have proven useful measures to stabilize slopes, while the performance of antislide piles in fissured slopes subjected to seismic action is inexplicit. To this end, this study aims to develop an effective method to assess the seismic stability of three-dimensional (3D) fissured slopes reinforced with piles. The modified pseudodynamic approach is introduced to properly present the dynamic characteristic of seismic waves in real cases. Based on the kinematic approach of limit analysis, a 3D failure mechanism integrating cracks and antislide piles is developed to describe the slope failure. Open cracks (cracks existing before slope failure) and formation cracks (cracks forming as part of the failure mechanism) are both considered. The effect of seismic action is expressed by incorporating the work rates of seismic force. Thanks to the principle of work–energy balance, solutions of safety factors can be obtained by the application of an optimization scheme. The proposed method is verified through a detailed comparison with previous investigations. This paper ends with a description of a parametric study to reveal the effects of cracks, pseudodynamic seismic action, and the design of antislide piles on slope stability.

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Data Availability Statement

Some or all data, models, or code that support the findings of this study are available from the corresponding author on reasonable request—specifically, all the data of comparison and parametric analysis and the code of the optimization scheme.

Notation

The following symbols are used in this paper:
ah
horizontal seismic acceleration;
B
total width of slope;
Bmax
maximum width of the 3D portion;
b
effective width of inserted portion of the piles;
c
soil cohesion;
c
critical soil cohesion;
Dc
internal energy dissipation rate generated by soil resistance;
Dcc
internal work rate generated by soil resistance;
Dcr
internal energy dissipation rate along crack;
Dp
internal energy dissipation rate generated by antislide piles;
D1
center-to-center interval of adjacent piles;
D2
clear interval of adjacent piles;
d
diameter of single pile;
F
safety factor;
f
amplification factor;
fc
uniaxial compressive strength;
ft
uniaxial tensile strength;
G
shear modulus;
g
acceleration due to gravity;
H
slope height;
H
crack height;
hmax
maximum crack depth;
kh
seismic coefficient;
L
length of AD, as shown in Fig. 1;
L
length of AB, as shown in Fig. 1;
Ls
horizontal distance between slope toe and slope crest;
n
coefficient of pile location;
p
lateral force of piles;
R
circle radius;
r
upper log-spiral;
r
lower log-spiral;
rh
length of OE, as shown in Fig. 1;
rm
distance between circle center and rotation center;
rM
length of OM, as shown in Fig. 1;
r0
length of OA, as shown in Fig. 1;
r0
length of OA′, as shown in Fig. 1;
S
area of failure surface;
Scr
area of crack surface;
T
vibration period;
uh
horizontal displacement;
uhb
horizontal displacement at slope base;
uh0
horizontal displacement at slope crest;
V
volume of failure blocks;
Vs
shear wave velocity;
v
magnitude of velocity at considered point;
w
effective width of piles in 3D portion;
Ws
external work rate generated by seismic force;
Wsc
external work rate generated by seismic forces;
Wγ
external work rate generated by self-weight of soils;
Wγc
external work rate generated by soil weigh;
wp
effective width of piles;
Xp
horizontal distance between slope toe and pile;
zi
distance between considered point and slope base;
β
slope angle;
γ
unit weight of soils;
δ
angle between vertical crack and velocity vector;
θ
polar angle at considered point;
θC, θh, θM, θN, θ0
angles to describe 3D failure mechanism, as shown in Fig. 1;
λs
wavelength of shear wave;
μ
soil viscosity;
ξ
soil damping ratio;
ρ
polar radius at considered point;
ρd
soil density;
φ
internal friction angle;
φ
critical internal friction angle;
ω
angular velocity about axis passing through Point O;
ω¯
angular velocity of shear wave; and
ω¯n
natural frequency of soils.

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 23Issue 3March 2023

History

Received: Mar 15, 2022
Accepted: Oct 14, 2022
Published online: Dec 27, 2022
Published in print: Mar 1, 2023
Discussion open until: May 27, 2023

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Ph.D. Candidate, School of Civil Engineering, Central South Univ., Changsha 410075 China (corresponding author). ORCID: https://orcid.org/0000-0002-0991-3143. Email: [email protected]
X. L. Yang, Ph.D. [email protected]
Professor, School of Civil Engineering, Central South Univ., Changsha 410075 China. Email: [email protected]

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