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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

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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 />

736 GEOSYNTHETICS INTERNATIONAL S 1996, VOL. 3, NO. 6


ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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 />

738 GEOSYNTHETICS INTERNATIONAL S 1996, VOL. 3, NO. 6


ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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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ZHAO D Limit Analysis <strong>of</strong> Geosynthetic-Reinforced Soil Slopes<br />

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 />

740 GEOSYNTHETICS INTERNATIONAL S 1996, VOL. 3, NO. 6

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