limit analysis of geosynthetic-reinforced soil slopes - IGS ...
limit analysis of geosynthetic-reinforced soil slopes - IGS ... limit analysis of geosynthetic-reinforced soil slopes - IGS ...
Technical Paper by A. Zhao LIMIT ANALYSIS OF GEOSYNTHETIC-REINFORCED SOIL SLOPES ABSTRACT: A kinematic solution of the plasticity theory applied to the stability of geosynthetic-reinforced soil slopes is presented in this paper. Translational and rotational failure mechanisms are considered and rigorously compared. For slopes heavily reinforced with geosynthetics, the limit loads obtained using a translational failure mechanism are smaller than those obtained using a rotational failure mechanism, while for slopes with a reduced amount of geosynthetic reinforcement, the latter yields better results. A rotational failure mechanism consistently yields lower stability factor values for load-free geosynthetic reinforced slopes. Limit analysis method solutions are compared to solutions obtained using limit equilibrium and slip-line methods. KEYWORDS: Geosynthetic-reinforced slopes, Limit analysis, Limit equilibrium, Slip-line method. AUTHOR: A. Zhao, Technical Director, Tenax Corporation, 4800 East Monument Street, Baltimore, Maryland 21205, USA, Telephone: 1/410-522-7000, Telefax: 1/410-522-3977. PUBLICATION: Geosynthetics International is published by the Industrial Fabrics Association International, 345 Cedar St., Suite 800, St. Paul, Minnesota 55101-1088, USA, Telephone: 1/612-222-2508, Telefax: 1/612-222-8215. Geosynthetics International is registered under ISSN 1072-6349. DATES: Original manuscript received 30 September 1996, revised version received 16 December 1996 and accepted 20 December 1996. Discussion open until 1 September 1997. REFERENCE: Zhao, A., 1996, “Limit Analysis of Geosynthetic-Reinforced Soil Slopes”, Geosynthetics International, Vol. 3, No. 6, pp. 721-740. GEOSYNTHETICS INTERNATIONAL S 1996, VOL. 3, NO. 6 721
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Technical Paper by A. Zhao<br />
LIMIT ANALYSIS OF<br />
GEOSYNTHETIC-REINFORCED SOIL SLOPES<br />
ABSTRACT: A kinematic solution <strong>of</strong> the plasticity theory applied to the stability <strong>of</strong><br />
<strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>soil</strong> <strong>slopes</strong> is presented in this paper. Translational and rotational<br />
failure mechanisms are considered and rigorously compared. For <strong>slopes</strong> heavily<br />
<strong>reinforced</strong> with <strong>geosynthetic</strong>s, the <strong>limit</strong> loads obtained using a translational failure<br />
mechanism are smaller than those obtained using a rotational failure mechanism, while<br />
for <strong>slopes</strong> with a reduced amount <strong>of</strong> <strong>geosynthetic</strong> reinforcement, the latter yields better<br />
results. A rotational failure mechanism consistently yields lower stability factor values<br />
for load-free <strong>geosynthetic</strong> <strong>reinforced</strong> <strong>slopes</strong>. Limit <strong>analysis</strong> method solutions are<br />
compared to solutions obtained using <strong>limit</strong> equilibrium and slip-line methods.<br />
KEYWORDS: Geosynthetic-<strong>reinforced</strong> <strong>slopes</strong>, Limit <strong>analysis</strong>, Limit equilibrium,<br />
Slip-line method.<br />
AUTHOR: A. Zhao, Technical Director, Tenax Corporation, 4800 East Monument<br />
Street, Baltimore, Maryland 21205, USA, Telephone: 1/410-522-7000, Telefax:<br />
1/410-522-3977.<br />
PUBLICATION: Geosynthetics International is published by the Industrial Fabrics<br />
Association International, 345 Cedar St., Suite 800, St. Paul, Minnesota 55101-1088,<br />
USA, Telephone: 1/612-222-2508, Telefax: 1/612-222-8215. Geosynthetics<br />
International is registered under ISSN 1072-6349.<br />
DATES: Original manuscript received 30 September 1996, revised version received<br />
16 December 1996 and accepted 20 December 1996. Discussion open until 1 September<br />
1997.<br />
REFERENCE: Zhao, A., 1996, “Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil<br />
Slopes”, Geosynthetics International, Vol. 3, No. 6, pp. 721-740.<br />
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1 INTRODUCTION<br />
Limit equilibrium methods are <strong>of</strong>ten used to design <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong>.<br />
Various <strong>limit</strong> equilibrium methods have been used in different studies (e.g. Leshchinsky<br />
and Volk (1985), Schmertmann et al. (1987) and Jewell (1990)). The <strong>limit</strong> <strong>analysis</strong> approach<br />
<strong>of</strong> plasticity is used in this paper as a solution technique. The stability <strong>of</strong> <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
<strong>slopes</strong> is assessed using translational and rotational failure mechanisms.<br />
A translational failure mechanism consists <strong>of</strong> a number <strong>of</strong> rigid blocks separated<br />
by internal planar rupture failure surfaces. This mechanism can be considered as a general<br />
case to the commonly used two-wedge failure mechanism. A rotational failure<br />
mechanism comprises a rigid block with a logarithmic rupture surface. A translational<br />
failure mechanism is used in the paper by Michalowski and Zhao (1995) to study the<br />
stability <strong>of</strong> <strong>reinforced</strong> <strong>slopes</strong>, and a rotational failure mechanism is used in the paper<br />
by Michalowski and Zhao (1994) to study the effect <strong>of</strong> <strong>geosynthetic</strong> reinforcement<br />
length and distribution on the safety <strong>of</strong> <strong>slopes</strong>. However, a rigorous comparison <strong>of</strong> these<br />
two failure mechanisms for the <strong>analysis</strong> <strong>of</strong> <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> is lacking.<br />
Since the same kinematic admissibility requirement applies to both failure mechanisms,<br />
it is possible to use the <strong>limit</strong> <strong>analysis</strong> method to rigorously evaluate these two<br />
failure mechanisms for <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong>.<br />
The objective <strong>of</strong> this paper is not to provide comprehensive design charts; instead,<br />
this study will improve the understanding <strong>of</strong> the failure mechanism for <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
<strong>slopes</strong>, by examining various <strong>limit</strong> <strong>analysis</strong> methods.<br />
The fundamental equations <strong>of</strong> the <strong>limit</strong> <strong>analysis</strong> approach to the stability <strong>of</strong> <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
<strong>slopes</strong> are presented in Section 2, followed by detailed formulations<br />
<strong>of</strong> both translational and rotational failure mechanisms. The two failure mechanisms<br />
are then rigorously compared using <strong>limit</strong> loads and rupture surfaces. Comparisons <strong>of</strong><br />
<strong>limit</strong> <strong>analysis</strong> method solutions to solutions obtained using <strong>limit</strong> equilibrium and slipline<br />
methods are also presented.<br />
2 KINEMATIC APPROACH OF THE LIMIT ANALYSIS METHOD<br />
A kinematic solution <strong>of</strong> the plasticity theory applied to the stability <strong>of</strong> <strong>geosynthetic</strong><strong>reinforced</strong><br />
<strong>soil</strong> <strong>slopes</strong> is presented in this paper. This approach is based on the upperbound<br />
theorem <strong>of</strong> plasticity. The pro<strong>of</strong> <strong>of</strong> the upper-bound theorem requires that the following<br />
assumptions be made: (i) the <strong>soil</strong> is a perfectly plastic material; (ii) the yield<br />
function <strong>of</strong> the <strong>soil</strong> is convex in the stress space; and (iii) the <strong>soil</strong> obeys the flow rule<br />
associated with the yield condition. The following upper-bound theorem states that the<br />
energy dissipation rate is at least as large as the rate <strong>of</strong> work by external forces in any<br />
kinematic admissible failure mechanism (Drucker et al. 1952):<br />
σ * ij ε * ij dV ≥ T * i v i dS + γ i v * i dV i, j = 1, 2, 3<br />
(1)<br />
V<br />
S<br />
V<br />
where: ε ij * = strain rate tensor in a kinematic admissible velocity field; σ ij * = stress tensor<br />
associated with ε ij * ; γ i = unit weight vector; T i * = vector <strong>of</strong> traction on the boundary<br />
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S; v i = velocity on the loaded boundary, S; andv * i = velocity in the volume, V (Note:<br />
v * i = v i on the loaded boundary S <strong>of</strong> the volume V).<br />
In <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>soil</strong> structures, the total energy dissipation during the incipient<br />
plastic failure process is equal to the sum <strong>of</strong> the energy dissipation in the <strong>soil</strong><br />
and in the reinforcement. The energy dissipation by the <strong>geosynthetic</strong> reinforcement can<br />
be included as an additional energy dissipation term on the left-hand side <strong>of</strong> Equation<br />
1. The <strong>geosynthetic</strong> reinforcement is assumed to dissipate energy during incipient collapse<br />
only in the tensile mode (the <strong>geosynthetic</strong> reinforcement is assumed to have no<br />
resistance to bending and compression). It is further assumed that the <strong>soil</strong> is uniform<br />
and homogeneous, i.e. no planes <strong>of</strong> weakness along the interface between the <strong>soil</strong> and<br />
<strong>geosynthetic</strong> reinforcement exist. It should be noted that a pullout failure mode is not<br />
considered in this paper. For the rigid block collapse mechanism considered in this paper,<br />
all energy dissipation takes place along the velocity discontinuities. The energy dissipation<br />
rate per unit area <strong>of</strong> the velocity discontinuity by tensile failure <strong>of</strong> the <strong>geosynthetic</strong><br />
reinforcement is as follows (Figure 1):<br />
t∕ sin ξ<br />
d r = k t ε * x sin ξdx = k t [v] cos(ξ − Ô) sinξ<br />
0<br />
where: ε x ∗ = strain rate in the direction <strong>of</strong> the <strong>geosynthetic</strong> reinforcement; t = thickness<br />
<strong>of</strong> the rupture layer; ξ = angle <strong>of</strong> inclination <strong>of</strong> the <strong>geosynthetic</strong> reinforcement to the<br />
rupture surface; [v] = magnitude <strong>of</strong> the velocity jump across the velocity discontinuity;<br />
Ô = internal friction angle <strong>of</strong> the <strong>soil</strong>; x = incremental horizontal length <strong>of</strong> <strong>geosynthetic</strong><br />
reinforcement; and k t = tensile strength <strong>of</strong> the <strong>geosynthetic</strong> reinforcement per unit cross<br />
section <strong>of</strong> the <strong>soil</strong>-<strong>geosynthetic</strong> composite. For uniformly placed <strong>geosynthetic</strong> reinforcement,<br />
k t can be calculated as follows:<br />
(2)<br />
k t = T s<br />
(3)<br />
[v]<br />
Geosynthetic<br />
reinforcement<br />
Displaced <strong>geosynthetic</strong><br />
reinforcement<br />
Figure 1.<br />
Rupture <strong>of</strong> the <strong>geosynthetic</strong> reinforcement across a velocity discontinuity.<br />
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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />
where: T = tensile strength <strong>of</strong> the <strong>geosynthetic</strong> reinforcement; and s = spacing <strong>of</strong> the<br />
<strong>geosynthetic</strong> reinforcement layers.<br />
The following Mohr-Coulomb failure criterion and an associative flow rule are used<br />
to describe the plastic behavior <strong>of</strong> the <strong>soil</strong>:<br />
ε ij = λ ∂ f (σ ij)<br />
∂ σ ij<br />
where: ε ij = strain rate tensor; σ ij = stress tensor; λ = non-negative scalar function; and<br />
the failure criteria function, f(σ ij ), is expressed as follows:<br />
f (σ ij ) = (σ x + σ y + 2c cot Ô)sinÔ − (σ x − σ y ) 2 + 4σ 2 xy (5)<br />
where c is the <strong>soil</strong> cohesion. Thus, the energy dissipation rate in the <strong>soil</strong> per unit area<br />
<strong>of</strong> the velocity discontinuity is derived as follows:<br />
(4)<br />
d m = c[v]cosÔ<br />
(6)<br />
For a rigid block collapse mechanism, Equation 1 can now be written as:<br />
c[v]cosÔ dl + k t [v] cos(ξ − Ô)sinξdl ≥ T * i v i dS + γ i v * i dV<br />
L * L * S<br />
V<br />
where: l = infinitesimal area <strong>of</strong> the discontinuity surface; and L * = total surface area<br />
<strong>of</strong> all velocity discontinuities. By using Equation 7 it is possible to find an upper-bound<br />
to the true <strong>limit</strong> load (or critical height) <strong>of</strong> a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope. A good estimation<br />
<strong>of</strong> the upper-bound using the kinematic approach can be obtained by considering<br />
a failure mechanism in which geometric parameters are varied in an optimization<br />
scheme where the smallest value <strong>of</strong> the unknown load is sought. The “Constrained Simplex”<br />
(Complex) method developed by Box (1965) is used in the optimization scheme<br />
in this paper.<br />
(7)<br />
3 TRANSLATIONAL FAILURE MECHANISM<br />
The <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> considered in this paper are restricted to those<br />
resting on firm foundations and having a horizontal top surface. The translational failure<br />
mechanism is shown in Figure 2a, and consists <strong>of</strong> rigid blocks separated by rupture<br />
surfaces. Kinematic admissibility requires that all velocity jump vectors be inclined at<br />
an angle Ô (internal friction angle <strong>of</strong> the <strong>soil</strong>) to the rupture surface. The velocity hodograph<br />
is shown in Figure 2b. The geometric parameters chosen for the translational failure<br />
mechanism are the angles, ξ k and ζ k , and the dimensionless parameter z k = h k /H (k<br />
=1,2,3...N) where, N = number <strong>of</strong> rigid blocks used in the failure mechanism, H =<br />
slope height, and h k = vertical height <strong>of</strong> rigid block k bounded by rupture surfaces.<br />
Using trigonometric relationships, the velocity <strong>of</strong> each block, v k , and the velocity<br />
jumps between blocks, [v] k , can be derived as a function <strong>of</strong> the vertical velocity compo-<br />
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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />
(a)<br />
q<br />
[v] k<br />
Ô<br />
ζ k<br />
v k<br />
Ô<br />
lk<br />
ξ k<br />
Geosynthetic reinforcement<br />
(b)<br />
v n<br />
[v] n<br />
v 1<br />
v 0<br />
[v] 1<br />
Figure 2. Translational failure mechanism in a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope: (a) slope<br />
dimensions and notation; (b) velocity hodograph.<br />
nent <strong>of</strong> the first block, v 0 . The velocity magnitude <strong>of</strong> the first block is calculated as follows:<br />
v 1 =<br />
v 0<br />
sin(ξ 1 − Ô)<br />
(8)<br />
For k = 2 ... N, the velocities v k and [v] k are as follows:<br />
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v k = v k−1<br />
sin(ξ k−1 + ζ k−1 − β − 2Ô)<br />
sin(ξ k + ζ k−1 − β − 2Ô)<br />
[v] k = v k−1<br />
sin(ξ k−1 − ξ k )<br />
sin(ξ k + ζ k−1 − β − 2Ô)<br />
(9)<br />
(10)<br />
where β is the slope inclination angle.<br />
The total energy dissipation by the <strong>geosynthetic</strong> reinforcement, D r , is the sum <strong>of</strong> the<br />
dissipated energy along each velocity discontinuity. Equation 2 and the hodograph in<br />
Figure 2b lead to the following expression:<br />
D r = N<br />
1<br />
k t v k cos(ξ k − Ô) z k H<br />
(11)<br />
By adding the energy dissipation in the <strong>soil</strong>, the left-hand side <strong>of</strong> Equation 7 becomes:<br />
D = N<br />
1<br />
c ⋅ cos Ô(v k l k + [v] k s k ) + N<br />
1<br />
k t v k cos(ξ k − Ô) z k H<br />
(12)<br />
where l k and s k are the surface areas <strong>of</strong> the velocity discontinuities as shown in Figure<br />
2a. The following expression gives the rate <strong>of</strong> work due to the uniform load, q,ontop<br />
<strong>of</strong> the slope:<br />
W q = qLv 0<br />
(13)<br />
where L is the area <strong>of</strong> the loaded boundary. The rate <strong>of</strong> work due to the <strong>soil</strong> self-weight<br />
is:<br />
W γ = N<br />
1<br />
A k γ v k sin(ξ k − Ô)<br />
(14)<br />
where: A k = volume <strong>of</strong> block k (with unit thickness); and γ = unit weight <strong>of</strong> the <strong>soil</strong>.<br />
Kinematic admissibility requires that the following inequality be satisfied:<br />
ξ k + ζ k−1 − β − 2Ô > 0<br />
k = 2, , N<br />
(15)<br />
Having derived the energy dissipation rates and the rate <strong>of</strong> work due to the external<br />
forces, Equation 7 can be used to compute the <strong>limit</strong> load, or critical height <strong>of</strong> the <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
slope. The following expression represents the <strong>limit</strong> load, q/k t ,ontop<br />
<strong>of</strong> a <strong>reinforced</strong> slope:<br />
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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />
q<br />
k t<br />
= 1<br />
Lv 0 N<br />
1<br />
v k cos(ξ k − Ô)z k H + N<br />
1<br />
c<br />
k t<br />
cos Ô(v k l k + [v] k s k ) − N<br />
1<br />
A k<br />
γ<br />
k t<br />
v k sin(ξ k − Ô)<br />
The critical height <strong>of</strong> a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope is represented by a dimensionless<br />
“stability factor”, γH/k t , that is calculated as follows:<br />
γH<br />
=<br />
k t<br />
N<br />
1<br />
1<br />
(A k ∕H)v k sin(ξ k − Ô) N<br />
1<br />
v k cos(ξ k − Ô)z k H + N<br />
1<br />
c<br />
cos Ô(v<br />
k k l k + [v] k s k ) − q Lv<br />
t k t 0<br />
The effect <strong>of</strong> the number <strong>of</strong> rigid blocks used in the translational failure mechanism<br />
on the <strong>limit</strong> loads <strong>of</strong> two <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> is shown in Figure 3. The <strong>limit</strong><br />
load obtained using a six-block failure mechanism is 18.4% less than the <strong>limit</strong> load obtained<br />
using a two-block failure mechanism for the 45_ slope. These values are within<br />
the expected range <strong>of</strong> results: the greater number <strong>of</strong> blocks used, the more accurate the<br />
upper-bound solution. The effect <strong>of</strong> the number <strong>of</strong> blocks used in the analyses on the<br />
computed <strong>limit</strong> load decreases as the slope increases. For a 60_ slope, the <strong>limit</strong> load<br />
obtained using a six-block failure mechanism is 8.2% lower than the <strong>limit</strong> load obtained<br />
using a two-block failure mechanism. The failure mechanisms for the 45_ slope using<br />
two- and six-block translational failure mechanisms are presented in Figures 4 and 5,<br />
(16)<br />
(17)<br />
Figure 3. Effect <strong>of</strong> the number <strong>of</strong> rigid blocks used in a translational failure mechanism<br />
<strong>analysis</strong> <strong>of</strong> a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope (Ô =30_, γH/k t =4).<br />
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respectively. The greater the number <strong>of</strong> rigid blocks used in the translational failure<br />
mechanism, the smoother the failure surface.<br />
The influence <strong>of</strong> the internal friction angle <strong>of</strong> the <strong>soil</strong>, Ô, on the failure surface geometry<br />
is shown in Figure 6. Figure 6 indicates that the greater the internal friction angle<br />
<strong>of</strong> the <strong>soil</strong>, the greater the <strong>limit</strong> loads, and the narrower the failure surfaces.<br />
4 ROTATIONAL FAILURE MECHANISM<br />
The rotational failure mechanism is also examined in order to compute the <strong>limit</strong> loads<br />
(or critical heights) for <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong>. The failure surface (velocity<br />
discontinuity) is assumed to pass through the toe <strong>of</strong> the slope. The normality rule in plasticity<br />
theory requires that the velocity discontinuity vector be inclined to the rupture<br />
surface at the internal friction angle <strong>of</strong> the <strong>soil</strong>, Ô, and the shape <strong>of</strong> the rupture surface<br />
in the rigid rotation mechanism must be a log-spiral:<br />
r = r o e (θ−θ o tan Ô)<br />
(18)<br />
Figure 4. Two-block translationalfailure mechanism in a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope(β<br />
=45_; Ô =30_, γH/k t =4).<br />
Figure 5. Six-block translational failure mechanism in a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope (β =<br />
45_; Ô =30_, γH/k t =4).<br />
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Ô= 25_, q/k t =2.43<br />
Ô= 30_, q/k t =4.08<br />
Ô= 35_, q/k t =6.44<br />
Ô= 40_, q/k t =9.98<br />
Figure 6. Failure surfaces in a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope using the translational failure<br />
mechanism and a range <strong>of</strong> <strong>soil</strong> friction angles (β =60_, γH/k t =4).<br />
where r o is the radius at the initial angle, θ o , as shown in Figure 7. The magnitude <strong>of</strong><br />
the velocity jump along the failure surface propagates according to the following expression:<br />
[v] = [v] o e (θ−θ o tan Ô)<br />
(19)<br />
where: [v] o =r o ω; and ω = velocity <strong>of</strong> rotation about the log-spiral center, O.<br />
The <strong>geosynthetic</strong> reinforcement energy dissipation rate along the entire log-spiral<br />
failure surface is calculated by integrating the unit energy dissipation given in Equation<br />
2 as follows:<br />
D r = <br />
(20)<br />
where:<br />
L * k t [v] cos(ξ − Ô) sinξdl<br />
(21)<br />
ξ = π 2 − θ + Ô (22)<br />
dl = rdθ<br />
cos Ô<br />
By substituting Equations 18, 19, 21 and 22 into Equation 20, the following expression<br />
is obtained:<br />
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O<br />
θ h<br />
θ<br />
θ o<br />
r o<br />
L<br />
q<br />
H<br />
[v]<br />
Ô<br />
ξ<br />
Log-spiral failure surface<br />
Geosynthetic reinforcement<br />
Figure 7.<br />
Rigid rotation failure mechanism in a <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>soil</strong> slope.<br />
h<br />
D r = k t r 2 o ω 1<br />
cos Ô θ e 2(θ−θ o)tanÔ<br />
sin θ cos(θ − Ô)dθ<br />
θo<br />
(23)<br />
Integration leads to:<br />
D r = 1 2 k t r 2 o [sin 2 θ h e 2(θ h −θ o)tanÔ<br />
− sin 2 θ o ]ω<br />
(24)<br />
where: θ = log-spiral angle; θ o = initial log-spiral angle (top <strong>of</strong> slope); θ h = final log-spiral<br />
angle (toe <strong>of</strong> slope) (Figure 7).<br />
The rate <strong>of</strong> energy dissipation in the <strong>soil</strong>, D m , and the rate <strong>of</strong> work due to the <strong>soil</strong> selfweight,<br />
W γ , were derived by Chen et al. (1969), and are given as follows for completeness:<br />
D m = 1 1<br />
2 cr2 o<br />
tan θ [e2 (θ h −θ o)tanÔ<br />
− 1]ω<br />
W γ = r 3 o γ (f 1 − f 2 − f 3 ) ω<br />
(25)<br />
(26)<br />
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where function f 1 , f 2 and f 3 are dependent on the geometry <strong>of</strong> the slope, the geometry<br />
<strong>of</strong> the failure surface, and the internal friction angle <strong>of</strong> the <strong>soil</strong> as follows:<br />
f 1 (θ o , θ h ) =<br />
1<br />
3(1 + 9tan 2 Ô) (3 tan Ô cos θ h + sin θ h )e 3(θ h −θo)tanÔ (3 tan Ô cos θ o + sin θ o )<br />
f 2 (θ o , θ h ) = 1 6<br />
L<br />
r o<br />
2cosθ o − L r o<br />
sin θ o<br />
f 3 (θ o , θ h ) = 1 6 e(θ h −θ o)tanÔsin(θ h − θ o ) − L r o<br />
sin θ h<br />
cos θ o − L r o<br />
+ cos θ h e (θ h −θ o)tanÔ<br />
(27)<br />
(28)<br />
(29)<br />
where:<br />
L<br />
r o<br />
= sin(θ h − θ o )<br />
− sin(θ h + β) H<br />
sin θ h sin θ h sin β<br />
(30)<br />
H<br />
r o<br />
= e (θ h −θ o)tanÔ<br />
sin θ h − sin θ o<br />
r o<br />
(31)<br />
The rate <strong>of</strong> work due to a uniform load q on top <strong>of</strong> the slope is:<br />
W q = qL(r o cos θ o − L∕2) ω<br />
(32)<br />
For a stable slope, the energy dissipation rate must be greater than the rate <strong>of</strong> work<br />
for any kinematic admissible mechanism. Again, the energy balance in Equation 7 is<br />
used to formulate the solution for one unknown quantity. The <strong>limit</strong> load, q/k t , and the<br />
stability factor, γH/k t , for a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope can be calculated using the<br />
following expressions:<br />
q<br />
=<br />
1<br />
k t L<br />
r<br />
2cosθ o − L<br />
o r o<br />
<br />
γH<br />
k t<br />
=<br />
⎡<br />
⎪<br />
⎣<br />
2 γH (f<br />
k 1 − f 2 − f 3 )<br />
tan Ô (e2(θ h −θo)tanÔ − 1) + sin 2 θ h e 2(θ h −θo)tanÔ − sin 2 θ o − t<br />
c 1<br />
k t<br />
H<br />
r o<br />
2(f 1 − f 2 − f 3 )<br />
c k t<br />
1<br />
tan Ô (e2(θ h −θ o)tanÔ − 1) + sin 2 θ h e 2(θ h −θ o)tanÔ − sin 2 θ o − q k t<br />
H<br />
r o<br />
⎪ ⎤ ⎦<br />
L<br />
ro<br />
2cosθ o − L r o<br />
<br />
(33)<br />
(34)<br />
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5 COMPARISON OF THE TWO FAILURE MECHANISMS<br />
The failure surfaces obtained using the translational and rotational failure mechanisms<br />
are presented in Figure 8 assuming a slope inclination angle, β =70_, γH/k t =<br />
6, and Ô =35_. Five blocks were used in the translational failure mechanism. The<br />
normalized <strong>limit</strong> loads, q/k t , from the translational and rotational failure mechanisms<br />
are 3.66 and 3.52, respectively.<br />
The <strong>limit</strong> loads on <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> calculated using a rotational failure<br />
mechanism along with the <strong>limit</strong> loads obtained using a translational mechanism are presented<br />
in Figure 9. For <strong>slopes</strong> that are heavily <strong>reinforced</strong> with <strong>geosynthetic</strong>s (small γH/k t<br />
value), the <strong>limit</strong> loads obtained using a translational failure mechanism are smaller than<br />
the <strong>limit</strong> loads obtained using a rotational mechanism. While for <strong>slopes</strong> that have a reduced<br />
amount <strong>of</strong> <strong>geosynthetic</strong> reinforcement (large γH/k t value), the <strong>limit</strong> loads obtained<br />
using a translational failure mechanism are greater than the <strong>limit</strong> loads obtained<br />
using a rotational mechanism. For a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope with β =90_, the two<br />
failure mechanisms produce almost identical solutions.<br />
Figure 10 shows a comparison <strong>of</strong> the stability factor for load-free <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
<strong>slopes</strong> using translational and rotational failure mechanisms. As shown in Figure<br />
10, a rotational failure mechanism always yields lower stability factor values for loadfree<br />
<strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong>.<br />
Both the <strong>limit</strong> loads and the rupture surfaces obtained using the two failure mechanisms<br />
are practically identical. This is due to the fact that a large number <strong>of</strong> blocks were<br />
used for the translational failure mechanism and all <strong>of</strong> the results were optimized. The<br />
Translational failure mechanism<br />
Rotational failure mechanism<br />
Figure 8. Translational versus rotational failure mechanisms in a <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
slope (β =70_, Ô =35_, γH/k t =6).<br />
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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />
Translational failure mechanism<br />
Rotational failure mechanism<br />
Figure 9.<br />
Limit loads on <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> (Ô =35_).<br />
Stability factor, γH/k t<br />
Translational failure mechanism<br />
Rotational failure mechanism<br />
Figure 10.<br />
Stability factors for load-free <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong>.<br />
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difference would be greater if less blocks are used, and the resulting failure surface<br />
would not be smooth (Figure 4).<br />
6 COMPARISON WITH LIMIT EQUILIBRIUM METHODS<br />
In Figure 11, the <strong>limit</strong> <strong>analysis</strong> method is compared to existing <strong>limit</strong> equilibrium<br />
methods for <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> with β =60_. The <strong>analysis</strong> results are<br />
presented using the stability factor, γH/k t , as a function <strong>of</strong> Ô. A rotational failure mechanism<br />
was used in the <strong>limit</strong> <strong>analysis</strong> method. In a paper by Michalowski and Zhao (1995),<br />
a translational failure mechanism was utilized. Figure 11 indicates that the <strong>limit</strong> <strong>analysis</strong><br />
method solution compares reasonably well to the solutions obtained using the <strong>limit</strong><br />
equilibrium methods. The solution obtained using the kinematic approach <strong>of</strong> the <strong>limit</strong><br />
<strong>analysis</strong> method is a rigorous upper-bound <strong>limit</strong> load (or critical height) solution while<br />
the <strong>limit</strong> equilibrium methods produce approximate solutions. This is due to the fact<br />
that, in the <strong>limit</strong> equilibrium methods, various assumptions are made regarding the<br />
stress distribution along the failure surface, and the forces in the <strong>geosynthetic</strong> reinforcement<br />
are usually not assumed to be fully mobilized in all layers. It has been demonstrated<br />
by Drescher and Detournay (1993) and Michalowski (1989) that the forces in<br />
translational failure mechanisms satisfy equilibrium equations. Also, moment equilibrium<br />
is satisfied for a rotational failure mechanism.<br />
and<br />
Stability factor, γH/k t<br />
Figure 11. Stability factors for <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> using <strong>limit</strong> <strong>analysis</strong> and<br />
<strong>limit</strong> equilibrium methods (β =65_).<br />
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7 COMPARISON WITH THE SLIP-LINE METHOD<br />
The slip-line method is based on the derived failure criterion describing the failure<br />
<strong>of</strong> a homogenized <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>soil</strong> composite and the application <strong>of</strong> the<br />
method <strong>of</strong> stress characteristics. The derivation <strong>of</strong> the failure criterion for a <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
<strong>soil</strong> composite is presented by Michalowski and Zhao (1995). The <strong>limit</strong><br />
loads on <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>soil</strong> <strong>slopes</strong>, walls and foundations are calculated using<br />
the slip-line method described by Zhao (1996). The stress characteristic fields for inclined<br />
<strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> at β =65_ and with <strong>soil</strong> internal friction angles<br />
<strong>of</strong> 30_, 35_ and 40_ are shown in Figures 12 to 14, respectively.<br />
The failure surface calculated using the slip-line method is compared to the failure<br />
surface from the <strong>limit</strong> <strong>analysis</strong> method (Figure 15). The two failure surfaces are similar.<br />
The <strong>limit</strong> load comparison using the slip-line and <strong>limit</strong> <strong>analysis</strong> methods is shown in<br />
Figure 16. The slip-line method yields lower <strong>limit</strong> load values at lesser γH/k t values, and<br />
β = 65_<br />
Ô = 30_<br />
γH/k t = 2<br />
q/k t = 4.33<br />
Figure 12. Stress characteristics for a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope obtained using the<br />
slip-line method.<br />
β = 65_<br />
Ô = 35_<br />
γH/k t = 2<br />
q/k t = 6.16<br />
Figure 13. Stress characteristics for a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope obtained using the<br />
slip-line method.<br />
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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />
β = 65_<br />
Ô = 40_<br />
γH/k t = 2<br />
q/k t = 8.91<br />
Figure 14. Stress characteristics for a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope obtained using the<br />
slip-line method.<br />
Slip-line method<br />
Limit <strong>analysis</strong> method<br />
Figure 15. Comparison <strong>of</strong> failure surfaces in a <strong>geosynthetic</strong>-<strong>reinforced</strong> slope obtained<br />
using the slip-line and <strong>limit</strong> <strong>analysis</strong> methods (β =65_, Ô =35_, γH/k t =2).<br />
higher <strong>limit</strong> load values at greater γH/k t values. Even though the slip-line method does<br />
not necessarily yield exact solutions for the <strong>limit</strong> loads, the solutions are typically good<br />
approximations, and are typically lower than the results using the kinematic approach.<br />
However, the <strong>limit</strong> loads presented in Figure 16 are the result <strong>of</strong> a problem that is not<br />
well-posed in that the length <strong>of</strong> the loaded boundary is not defined “a priori”, but is defined<br />
as a part <strong>of</strong> the solution. The calculated length <strong>of</strong> the loaded boundary using the<br />
slip-line and <strong>limit</strong> <strong>analysis</strong> methods are not the same. The slip-line solution presented<br />
in this paper is based on a “partial stress field”; when this stress field is extended to the<br />
entire body, a lower bound solution to the true load is obtained.<br />
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Figure 16. Comparison <strong>of</strong> <strong>limit</strong> loads on <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong> using the slip-line<br />
and <strong>limit</strong> <strong>analysis</strong> methods (β =70_, Ô =35_).<br />
8 CONCLUSIONS<br />
The kinematic approach <strong>of</strong> the plasticity theory to the stability <strong>of</strong> <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
<strong>soil</strong> <strong>slopes</strong> is presented in this paper. For <strong>slopes</strong> heavily <strong>reinforced</strong> with <strong>geosynthetic</strong>s,<br />
the <strong>limit</strong> loads obtained using a translational failure mechanism are smaller than<br />
the <strong>limit</strong> loads obtained using a rotational failure mechanism, while for <strong>slopes</strong> with a<br />
reduced amount <strong>of</strong> reinforcement, the latter yields better results. A rotational failure<br />
mechanism always yields lower stability factor values for load-free <strong>geosynthetic</strong>-<strong>reinforced</strong><br />
<strong>slopes</strong>. For translational failure mechanisms, a more accurate solution is<br />
achieved when a greater number <strong>of</strong> rigid blocks are used, particularily for <strong>slopes</strong> with<br />
smaller inclination angles.<br />
A kinematic approach to the <strong>limit</strong> <strong>analysis</strong> method <strong>of</strong> <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong><br />
is a rigorous upper-bound <strong>limit</strong> load (or critical height) solution. The application <strong>of</strong><br />
three design methods (i.e. <strong>limit</strong> <strong>analysis</strong>, <strong>limit</strong> equilibrium and slip-line methods) to the<br />
stability <strong>analysis</strong> <strong>of</strong> <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong>, are assessed. Comparisons <strong>of</strong> the<br />
<strong>limit</strong> <strong>analysis</strong> method to the <strong>limit</strong> equilibrium and the slip-line methods indicate that<br />
the <strong>limit</strong> <strong>analysis</strong> method produces reasonably similar results. The kinematic approach<br />
may prove to be useful in the design <strong>of</strong> <strong>geosynthetic</strong>-<strong>reinforced</strong> <strong>slopes</strong>.<br />
REFERENCES<br />
Box, M.J., 1965, “A New Method <strong>of</strong> Constrained Optimization and a Comparison with<br />
Other Methods”, Computer Journal, Vol. 8, No. 1, pp. 42-52.<br />
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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />
Chen, W.F., Giger, M.W. and Fang, H.Y., 1969, “On the Limit Analysis <strong>of</strong> Stability <strong>of</strong><br />
Slopes”, Soils and Foundations, Vol. 9, No. 4, pp. 23-32.<br />
Drescher, A. and Detournay, E., 1993, “Limit Load in Translational Failure Mechanisms<br />
for Associative and Non-Associative Materials”, Geotechnique, Vol. 43, No.<br />
3, pp. 443-456.<br />
Drucker, D.C., Prager, W. and Greenberg, H.T., 1952, “Extended Limit Design Theorems<br />
for Continuous Media”, Quarterly <strong>of</strong> Applied Mathematics, Vol. 9, No. 4, pp.<br />
381-389.<br />
Jewell, R.A., 1990, “Revised Design Charts for Steep Reinforced Slopes”, Reinforced<br />
Embankments, Theory and Practice, Shercliff, D.A., Editor, Thomas Telford, proceedings<br />
<strong>of</strong> the conference Reinforced Embankments, Theory and Practice in the<br />
British Isles held at Cambridge University, UK, September 1989, pp. 1-30.<br />
Leshchinsky, D. and Volk, J.C., 1985, “Stability Charts for Geotextile-Reinforced<br />
Walls”, Transportation Research Record 1131, pp. 5-16.<br />
Michalowski, R.L. and Zhao, A., 1995, “Continuum Versus Structural Approach to Stability<br />
<strong>of</strong> Reinforced Soil Structures”, Journal <strong>of</strong> Geotechnical Engineering,ASCE,<br />
Vol. 121, No. 2, pp.152-162.<br />
Michalowski, R.L. and Zhao, A., 1994, “The Effect <strong>of</strong> Reinforcement Length and Distribution<br />
on Safety <strong>of</strong> Slopes”, Proceedings <strong>of</strong> the Fifth International Conference on<br />
Geotextiles, Geomembranes and Related Products, Vol. 1, Singapore, September<br />
1994, pp. 495-498.<br />
Michalowski, R.L., 1989, “Three Dimensional Analysis <strong>of</strong> Locally Loaded Slopes”,<br />
Geotechnique, Vol. 39, No. 1, pp. 27-38.<br />
Schmertmann, G.R., Chouery-Curtis, V.E., Johnson, R.D. and Bonaparte, R., 1987,<br />
“Design Charts for Geogrid Reinforced Soil Slopes”, Proceedings <strong>of</strong> Geosynthetics<br />
’87, IFAI, Vol. 1, New Orleans, Louisiana, USA, February 1987, pp. 108-120.<br />
Zhao, A., 1996, “Failure Loads on Geosynthetic Reinforced Soil Structures”, Geotextiles<br />
and Geomembranes, Vol. 14, Nos. 5 and 6, pp. 289-300.<br />
NOTATIONS<br />
Basic SI units are given in parentheses.<br />
c = <strong>soil</strong> cohesion (N/m 2 )<br />
d m = energy dissipation rate in <strong>soil</strong> per unit area <strong>of</strong> velocity discontinuity<br />
(Nm -1 s -1 )<br />
d r = energy dissipation rate in <strong>geosynthetic</strong> reinforcement per unit area <strong>of</strong><br />
velocity discontinuity (Nm -1 s -1 )<br />
D = total energy dissipation rate in <strong>soil</strong> and <strong>geosynthetic</strong> reinforcement<br />
(Nm -1 s -1 )<br />
D m = total energy dissipation rate in <strong>soil</strong> (Nm -1 s -1 )<br />
D r = total energy dissipation rate in <strong>geosynthetic</strong> reinforcement (Nm -1 s -1 )<br />
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f 1 , f 2 , f 3 = functions dependent on geometry <strong>of</strong> slope and failure surface, and Ô<br />
(Equations 27, 28 and 29, respectively) (dimensionless)<br />
H = slope height (m)<br />
h k = vertical height <strong>of</strong> rigid block bounded by rupture surfaces (Figure 2) (m)<br />
k t = tensile strength <strong>of</strong> <strong>geosynthetic</strong> reinforcement per unit area <strong>of</strong> composite<br />
(N/m 2 )<br />
L = area <strong>of</strong> loaded boundary (m 2 )<br />
L * = total surface area <strong>of</strong> all velocity discontinuities (m 2 )<br />
l = infinitesimal area <strong>of</strong> discontinuity surface (m 2 )<br />
l k = surface area <strong>of</strong> velocity discontinuity (m 2 )<br />
N = number <strong>of</strong> rigid blocks in translational failure mechanism<br />
(dimensionless)<br />
q = uniform load on top <strong>of</strong> the slope (N/m 2 )<br />
r = log-spiral radius (m)<br />
r o = log-spiral radius at initial angle, θ o (m)<br />
S = loaded boundary area (m 2 )<br />
s = spacing <strong>of</strong> <strong>geosynthetic</strong> reinforcement layers (m)<br />
s k = surface area <strong>of</strong> velocity discontinuity (m 2 )<br />
t = rupture layer thickness (m)<br />
T = tensile strength <strong>of</strong> <strong>geosynthetic</strong> reinforcement per unit width (N/m)<br />
T * i = vector <strong>of</strong> traction on the boundary S (N/m 2 )<br />
V = volume (m 3 )<br />
V k = volume <strong>of</strong> block k with unit thickness (Equation 14) (m 3 )<br />
v i = velocity vector on the loaded boundary S (m/s)<br />
v * i = velocity in the volume V (m/s)<br />
v k = velocity <strong>of</strong> rigid blocks in translational failure mechanism (m/s)<br />
[v] = magnitude <strong>of</strong> velocity jump vector (m/s)<br />
x = incremental length <strong>of</strong> <strong>geosynthetic</strong> reinforcement (m)<br />
z k = dimensionless parameter, z k = h k /H<br />
W q = rate <strong>of</strong> work due to uniform load q (Nms -1 )<br />
W γ = rate <strong>of</strong> work due to self-weight <strong>of</strong> <strong>soil</strong> (Nms -1 )<br />
α = inclination angle <strong>of</strong> <strong>geosynthetic</strong> reinforcement with respect to x-axis (_)<br />
β = slope inclination angle from horizontal (_)<br />
γ = unit weight <strong>of</strong> <strong>soil</strong> (N/m 3 )<br />
γ i = unit weight <strong>of</strong> <strong>soil</strong> vector (N/m 3 )<br />
ε ij = strain rate tensor (s -1 )<br />
ε * ij = strain rate tensor in kinematic admissible velocity field (s -1 )<br />
ε * x = strain rate in direction <strong>of</strong> reinforcement (s -1 )<br />
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ζ k = angular variable used in translational failure mechanism (Figure 2) (_)<br />
θ = log-spiral angle (_)<br />
θ h = final log-spiral angle (top <strong>of</strong> slope) (_)<br />
θ o = inital log-spiral angle (toe <strong>of</strong> slope) (_)<br />
λ = non-negative scalar function (dimensionless)<br />
ξ , ξ k = angle <strong>of</strong> inclination <strong>of</strong> reinforcement to failure surface (_)<br />
σ ij = stress tensor associated with ε ij (N/m 2 )<br />
σ * ij = stress tensor associated with ε * ij (N/m 2 )<br />
Ô = internal friction angle <strong>of</strong> <strong>soil</strong> (_)<br />
ω = velocity <strong>of</strong> rotation (_/s)<br />
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