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    Technical Note

    A comprehensive method for analyzing the effect of geotextile layerson embankment stability

    A. Tolooiyan a,*, I. Abustan a, M.R. Selamat a, Sh. Ghaffari b

    a School of Civil Engineering, Universiti Sains Malaysia (USM), Engineering Campus, Pulau Pinang, Malaysiab Soil and Water Engineering, P.O. Box 3185838143, Karaj, Tehran, Iran

    a r t i c l e i n f o

    Article history:

    Received 28 March 2008

    Received in revised form

    20 November 2008

    Accepted 21 November 2008

    Available online 20 February 2009

    Keywords:

    Embankment

    Water condition

    Geotextile

    Mathematical model

    Stability

    Finite element method

    a b s t r a c t

    Commercial software is used widely in slope stability analyses of reinforced embankments. Almost all of

    these programs consider the tensile strength of geotextiles and soilgeotextile interface friction.

    However, currently available commercial software generally does not consider the drainage function of

    nonwoven geotextile reinforcement. In this paper, a reinforced channel embankment reinforced by

    a nonwoven geotextile is analyzed using two methods. The first method only considers the tensile

    strength and soilgeotextile interface friction. The second method also considers the drainage function.

    In both cases, the reinforced embankment is modeled in rapid drawdown condition since this is one of

    the most important conditions with regard to stability of channel embankments. It is shown that for this

    type of application, modeling a nonwoven geotextile reinforced embankment using commercial software

    which neglects the drainage function of the geotextile may be unrealistic.

    2009 Elsevier Ltd. All rights reserved.

    1. Introduction

    When it happens, embankment collapse can be disastrouscausing serious loss of life, money and time. Reconstructingcollapsed embankments can be very costly and from a purely

    economic standpoint, it would be more beneficial to reinforce theembankment so that it does not fail rather than reconstruct.Nowadays advances in technology in material science have

    produced geosynthetic materials for usage in various aspects ofcivil engineering.

    Geosynthetic materials that are used widely in embankments toincrease stability (Bergado and Teerawattanasuk, 2008; Brianon

    and Villard, 2008; Chen et al., 2008; Li and Rowe, 2008; Rowe and

    Taechakumthorn, 2008; Sarsby, 2007). Geotextile layers increasethe embankment stability by virtue of two primary functions:

    tensile reinforcement (as in the cases cited above) and as a drainageelement reducing pore pressures.

    Most analyses of geotextile reinforced embankments considerthe effect of the tensile stiffness of the geotextiles but generally

    do not consider the drainage function of nonwoven geotextilereinforcement. While this is suitable for most applications, in thecase of nonwoven geotextile reinforced channel embankments this

    may represent a significant oversight. Thus the objective of thispaper is to examine the effect of ignoring and considering thedrainage function for a channel embankment subject to rapid

    drawdown.

    2. Current numerical procedure

    Lemonnier et al. (1998), analyzed the effect of geotextile rein-forcement on the stability of embankments by a mathematicaldisplacement method presented by Gourc et al. (1986), where byonly the tensile strength of the geotextile was taken into consid-

    eration in the analysis. Sharma and Bolton (2001), Bergado et al.(2002), and Hinchberger and Rowe (2003), utilized different

    commercial and non-commercial FEM models to analyze thestability of geotextile reinforced embankments. In all of theseinvestigations, tensile strength and soilgeotextile interface frictionwere taken into consideration, while ignoring the geotextiledrainage ability. Nagahara et al. (2004) used FEM to analyze the

    effect of the drainage ability of geotextiles on stability of embank-ments. Nagahara and colleagues reported that the measured hori-zontal deformation of the case study embankment was much

    smaller than estimated by FEM due to the neglecting soilgeo-textile interface friction in their FEM analysis. Iryo and Rowe (2005)firstly used FEM to model the drainage ability of geotextile, then,after estimating the water surface in embankment, they used

    * Corresponding author.

    E-mail address: [email protected] (A. Tolooiyan).

    Contents lists available at ScienceDirect

    Geotextiles and Geomembranes

    j o u r n a l h o m e p a g e : w w w . e l s e v i e r . c o m / l o c a t e / g e o t e x m e m

    0266-1144/$ see front matter 2009 Elsevier Ltd. All rights reserved.

    doi:10.1016/j.geotexmem.2008.11.013

    Geotextiles and Geomembranes 27 (2009) 399405

    mailto:[email protected]://www.sciencedirect.com/science/journal/02661144http://www.sciencedirect.com/science/journal/02661144mailto:[email protected]
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    a limit equilibrium method to consider the tensile strength of thegeotextile.

    The FEM can be used to compute stresses and displacements inearth structures and soil masses. The method is particularly usefulfor soilstructure interaction problems, in which structuralmembers interact with a soil mass (USACE, 1995). In complex

    conditions, it is often difficult to anticipate failure modes, particu-larly if reinforcement or structural members such as geotextiles,concrete retaining walls, or sheet piles are included (USACE, 2003).Another important input to the stability analyses for reinforced

    slopes is the load in the reinforcement and FEM can provide usefulguidance for establishing the load that will be used ( USACE, 2003).The capabilities of FEM, led to it being used by many researchers toinvestigate the behavior of reinforced embankments e.g. Rowe

    (1982, 1984), Rowe and Soderman (1984), Humphrey and Holtz(1989), Hird and Kwok (1989), Rowe and Mylleville (1990), Bergadoet al. (2002), etc. However, Rowe and Mylleville (1994) explainedthat careful consideration must be given to the type of FEM and

    constitutive relationships that will be used to model the discretecomponents of the reinforced embankments.

    2.1. Serious limitations of mathematical models in modeling

    geotextile

    While commercial software such as Plaxis Ver.7.2 (1998), MStabVer.9.8 (2004), Geostab 2004 (2004), Stedwin Ver.2.6 (1999) andPcstabl Ver.6 (1999) are widely used to analyze geotextile rein-

    forced embankment, those just consider the geotextile tensilestrength and/or soilgeotextile interface friction. In some cases ofreinforced embankment analysis, the results may be unrealisticbecause the drainage function of geotextile is ignored by the

    previously mentioned commercial software.

    2.2. Equations to evaluate geotextile tensile strength and soil

    geotextile interface friction

    To evaluate the soilgeotextile interface in FE analysis theMohrCoulomb equation can be used as it is widelyemployed in FEmodeling of soilstructure interfaces. This equation is able toconsider both cohesion and friction angle of interfaces.

    The equation for considering geotextile tensile strength is

    usually strain energy equation that is shown in Eq. (1).

    Pa

    ZL0

    EA

    2

    du

    dx0

    2dx0 (1)

    wherePa is the strain energy, EA is the axial rigidity, L is the lengthof geotextile, u is the axial displacement along the geotextile, andx0

    is the distance along the geotextile.

    2.3. Necessity of equations associated with water in reinforcedembankment components

    In analyzing the embankment, one of the most important issues

    is pore water pressure since pore water pressure whether positiveor negative has a direct effect on the stability and safety factor ofembankment. Therefore realistic pore water pressure conditionsneed to be considered explicitly in the analysis.

    2.4. Water flow in reinforced embankment components

    Richards (1931) derived the governing equation for transient

    water flow within an unsaturated material from Darcys law andContinuity. For the two dimensional homogeneous anisotropic

    material, the equation is as Eq. (2).

    kxv

    2h

    vx2 ky

    v2h

    vy2

    vQ

    vt mwgw

    vh

    vt(2)

    where h is the total hydraulic head, kx, ky are the unsaturatedhydraulic conductivities for the x- and y-directions, mw is the slope

    of the water volume characteristic curve, gw is the unit weight ofwater, Q is the volumetric water content, and t is the time.

    2.5. Water storage in reinforced embankment components

    Both the soil and geotextile consists of a collection of solidparticles and interstitial voids. The pore spaces or voids could befilled either with water or air, or with a combination of both. In

    saturated materials (soil and/or geotextile), all the voids are filledwith water and the volumetric water content of the materials isequal to the porosity of the soil according to Eq. (3).

    Q nS (3)

    where Q is the volumetric water content, n is the porosity, and Sisthe degree of saturation (in saturated materials equal to 1.0 or100%)

    In unsaturated materials, the volume of water stored withinthe voids depends on the negative water pressure (suction). Thewater content is not constant and therefore so a function isrequired to describe how the water contents changes with

    different stresses in the materials. The volumetric water contentfunction describes the capability of materials to store water underchanges in pore water pressures (Krahn, 2004). A typical functionof volumetric water content and pore water pressure is shown in

    Fig. 1.The volumetric water content function describes what portion

    (or volume) of the voids remains water-filled as the materials

    drains. The three main features that characterize the volumetricwater content function are the air-entry value (AEV), the slope ofthe function for both the positive and negative pore water pressure

    (mw), and the residual water content (Qr). The air-entry value (AEV)corresponds to the value of negative pore water pressure when thelargest voids or pores begin to drain freely. It is a function of themaximum pore size in a soil and is also influenced by the pore-sizedistribution within a soil. Soils with large and uniformly shaped

    pores have relatively low AEVs (Krahn, 2004). Another key featureof the volumetric water content function is the residual volumetricwater content (Qr), which represents the volumetric water contentof a soil where a further increase in negative pore water pressure

    does not produce significant changes in water content (Krahn,2004).

    Fig. 1. Volumetric water content (storage) function (Krahn, 2004).

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    As shown in Fig. 1, the slope of the volumetric water contentversus pore water pressure has different slopes (mw) in positive and

    negative pore water pressure regions. The value of the slope in thepositive pressure range is the coefficient of volume compressibility,and in physical terms, it describes how much a saturated soilvolumewill swell or shrinkfor a given change in pore pressure. This

    coefficient can be back-calculated from consolidation test data(Krahn, 2004).

    mw 1

    E(4)

    where E is the elasticity modulus.

    Van Genuchtens (1980) predictive method for measurement ofa volumetric water content function in negative pore water pres-sure has been used in many studies and its validity has beenexamined for a wide range of soils. Iryo and Rowe (2004) also used

    this model to investigate infiltration into a soil column containinga nonwoven geotextile layer and found that it works well formodeling the unsaturated reaction of the nonwoven geotextile.Therefore, this method could be used in modeling to describe the

    hydraulic properties of both soil and the geotextile.

    Q Qr Qs Qrh

    1 Ja

    nim (5)

    where Q is the volumetric water content, Qr is the residual volu-metric water content,Qs is the saturated volumetric water content,

    J is the negative pore water pressure, and a, n, m are the curvefitting parameters.

    Rawls et al. (1982), and Carsel and Parrish (1988) conductedsubstantial experimental work and obtained the Van Genuchten

    model parameters for different soil textural groups according to theUSDA soil classification system. As a result of this work, laboratoryparticle size analysis can be directly related to the modeledparameters. Further, for geotextile, the Van Genuchten model

    parameters could be taken from the typical values evaluated frompublished data compiled by Iryo and Rowe (2003).

    2.6. Hydraulic conductivity in reinforced embankment components

    In a saturated soil, allthe pore spacesbetween the solid particlesare filled with water. Once the air-entry value is exceeded, airenters the largest pores and the air-filled pores become non-

    conductive conduits to flow and increase the tortuosity of the flowpath. As a result, the ability of the soil and geotextile to transportwater (the hydraulic conductivity) decreases. As pore water pres-sures become increasingly more negative, more pores become air-

    filled and the hydraulic conductivity decreases further. By thisdescription, it is clear that the ability of water to flow througha profile depends on how much water is present in the soil, which is

    represented by the volumetric water content function (Krahn,2004).

    The hydraulic conductivity function for an unsaturated soil canbe developed using Van Genuchten method. Van Genuchten (1980)offered the following closed form equation to describe the

    hydraulic conductivity of soil as a function of suction, as seen inEq. (6).

    kw ks

    h1

    aJn1

    1

    aJn

    mi21 aJn

    m2

    (6)

    where ks is the saturated hydraulic conductivity, a, n, m are thecurve fitting parameters, J is the required suction range, and n is

    equal to 1/(1m).

    From Eq. (6), the hydraulic conductivity function of soil orgeotextile could be estimated once the saturated conductivity and

    the two curve fitting parameters, a and m are known.Van Genuchten showed that the curve fitting parameters could

    be estimated graphically based on the volumetric water contentfunction of the soil and suggested that the best point to evaluate

    these parameters is the halfway point between the residual andsaturated water content of the volumetric watercontent function. IfQp be the volumetric water content at the halfway point of thevolumetric water content function, and Jp be the suction at thesame point, then the slope Sp of the function could be calculated as

    Eq. (7) (Krahn, 2004).

    Sp 1

    Qs Qr

    dQpdlog Jp (7)

    Van Genuchten proposed Eqs. (8) and (9) to estimate the parame-ters m and a, when Sp is calculated.

    m 1 exp0:8Sp

    (8)

    where Sp is between 0 and 1.

    m 1 0:5755

    Sp

    0:1

    S2p

    0:025

    S3p(9)

    where Sp > 1.

    After calculating m, a could be estimated by Eq. (10).

    a 1

    J

    2

    1m 1

    1m(10)

    2.7. Analysis associated with drainage ability of geotextile

    By applying Eqs. (2)(10) to both the soil and geotextile, it ispossible to obtain water storage and hydraulic conductivity inembankment components and subsequently estimate the mannerof water flow in reinforced embankments. It follows that the effect

    of geotextiles as a drain layer could be taken into consideration inanalysis of reinforced embankment. In this research, the finiteelement computer program SEEP/W Ver. 5.18 (GEO-SLOPE Inter-

    national Ltd., 2002a) was used to solve Eqs. (2)(10).

    Table 1

    Specifications of nonwoven geotextile.

    Material property Value

    Thickness (mm) 2.5

    Unit weight (kN/m3) 1.11

    Hydraulic conductivity in plane direction (m/s) 2.72E3

    Hydra uli c conduc ti vi ty in c ross plan e dir ection (m/s) 7E2

    Elasticity modulus (kPa) 33,000

    Maximum tensile strength (kN/m) 21

    Table 2

    Soil characteristics and soilgeotextile interface specifications.

    Specification Value

    Water content (percentage) 32

    Dry unit weight (g/cm3) 1.43

    Poisson Ratio 0.38

    Specific gravity 2.71

    Hydraulic conductivity (m/s) 4.29E7

    Elasticity modulus (kPa) 12,500

    Soil cohesion in saturated condition (kPa) 10.571

    Soil f riction angle in saturat ed condition (degree) 50.06

    Soilgeotextile interface cohesion in saturated condition (kPa) 15.491

    Soilgeotextile interface friction angle in saturated condition (degree) 52.21

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    2.8. Analysis associated with geotextile tensile strength

    and soilgeotextile interface friction

    In this research, Eq. (1) was used in a linear-elastic mode tomodel the effect of tensile strength of geotextile. The finite elementcomputer program SIGMA/W Ver. 5.18 (GEO-SLOPE InternationalLtd., 2002b) was used to solve Eq. (1). To estimate the elasticity

    modulus of a particular kind of nonwoven geotextile, appropriatetests were done according to ASTM D4632 (2003) in the compositematerial laboratory of USM. The specifications of this particular

    nonwoven geotextile are mentioned in Table 1.To analyze the strain, stress and shape change in embankment

    components, an elasticplastic model was used by utilizing SIGMA/W Ver. 518. Also, this model can consider the soilgeotextile

    Fig. 2. Situation of the geotextile layers in reinforced channel embankment.

    Fig. 3. Slip surface of reinforced embankment during rapid drawdown, analyzed by proposed method.

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    interface friction by very fine meshes in the soilgeotextile inter-face. The friction angle and cohesion between the soil and geo-textile were determined using direct shear tests in the geotechnical

    laboratory of USM. The geotextile layers were cut to square piecesof 100 mm by 100 mm and then it was glued using epoxy glue tothe top of a piece of hard wood having the same dimensions(100 mm by 100 mm). This procedure was used previously by

    Mahmood et al. (2002). The soil used was classified as Silt Loamand Lean Clay with Sand in USDA and Unified Soil ClassificationSystem, respectively. Soilgeotextile interface specifications andcharacteristics of the soil are mentioned in Table 2.

    3. Modeling reinforced channel embankment

    Different size of three node triangular meshes with three inte-gration points was employed to model the embankment, althoughground surface and the geotextile layers were formed by very finefour node quadrilateral meshes with four integration points. In

    seepage analysis, the left and right boundaries were modeled by

    infinite elements however in stressstrain analysis the embank-ment bounded with zero displacement along edges. As a multi-

    joined analysis, the stressstrain distribution FEM analysis was

    conducted by SIGMA/W. In parallel, the FEM analysis was con-ducted by SEEP/W to model pore water pressure distribution in theembankment material.Finally, the FE results of SIGMA/Wand SEEP/

    W were jointly imported into the SLOPE/W (GEO-SLOPE Interna-tional Ltd., 2002c) to analyze the embankment stability and safetyfactor.

    To estimate the effect of reinforcement and to compare between

    the conventional analysis and the proposed analysis method,a channel embankment was simulated using three methods duringrapid drawdown condition. Firstly, the channel embankment wasanalyzed without reinforcement (non-reinforced embankment).

    Secondly, with the same rapid drawdown condition, a geotextile

    reinforced embankment was analyzed by using the conventional

    method and the geotextile tensile strength and soilgeotextileinterface friction were considered together. Thirdly, with the samerapid drawdown condition and reinforcing method, the reinforcedembankment was analyzed by using the proposed method that

    considered geotextile tensile strength, soilgeotextile interfacefriction, and the drainage ability of the geotextile, together. Beforerapid drawdown, the water level in the channel was 3 m. In 8 h thewater level was dropped down about 2.5 m and the water level in

    the channel reached 0.5 m. In all of the three mentioned analyses,

    Fig. 4. Water table at 3 h and 8 h after start of rapid drawdown, analyzed by conventional method (a) and proposed method (b).

    Fig. 5. Maximum effective stress at 3 h after start of rapid drawdown, analyzed by

    conventional method (a) and proposed method (b).

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    embankment stability was calculated at 3 h after the start of rapiddrawdown. USACE (2003) emphasize that the minimum required

    safety factor of earth slope should be 1.30 during rapid drawdowncondition.

    3.1. Stability safety factor of reinforced and non-reinforced

    embankment

    Analysis of the non-reinforced embankment gives a stabilitysafety factor equal to 1.26. According to USACE (2003), thisembankment might be unstable during rapid drawdown condition,indicating reinforcement is needed to prevent instability.

    To reinforce the embankment, as shown in Fig. 2, three layers ofneedle-punched nonwoven geotextile with 1.5 m length and 1 mdistance in between were laid inside the embankment. The

    reinforced embankment was analyzed by the aforementionedconventional method under the rapid drawdown condition.Analysis of the reinforced embankment gave a stabilitysafety factorequal to1.29. The increase in safety factor in the reinforcedembankment is due to the effect of tensile strength and soilgeo-

    textile interface friction.To find the more complete effect of geotextile, the reinforced

    embankment was analyzed by the proposed method with the samerapid drawdown condition. A safety factor of 1.33 was obtained

    from the analysis which considered the drainage property of thegeotextile. This factorof safety meets the USACE (2003) guideline inembankment stability which requires a minimum value of 1.3 forrapid drawdown conditions. The slip surface of the reinforced

    embankment, analyzed by the proposed method is shown in Fig. 3.

    Fig. 4(a) and (b) show the water table at 3 h and 8 h after start ofrapid drawdown analyzed by conventional and proposed method,respectively. Comparing the water table in Fig. 4(a) and (b), shows

    that geotextile layers drain the embankment internal water duringthe rapid drawdown and the embankment becoming lighter. Fig. 5shows the result of stressstrain analysis at 3 h after start of rapid

    drawdown. Different effective stress at the right side of embank-ment is due to the different pore water pressure condition analyzedby the conventional and proposed method.

    Fig. 6 shows the safety factor of non-reinforced embankment

    and reinforced embankment analyzed by conventional andproposed method. Although all the reinforcing and rapid draw-down conditions are exactly the same in both analyses, theproposed complete method offered the highest safety factor. This

    highlights the benefit of accurately modeling both the

    reinforcement and drainage functions of needle-punchednonwoven geotextile as demonstrated in the proposed method.

    4. Conclusion and results

    Conventionalanalysesof a needle-punched nonwoven geotextile

    reinforced channel embankment which only considers the effect ofthe tensile stiffness and strength of the geotextile on embankmentstabilityunderestimated the stabilitycompared to analysesthat alsoconsidered the drainage function of the geotextile. The proposed

    analysis method which considers both functions provides a morerealistic methods of assessing the stability of needle-punchednonwoven geotextile reinforced channel embankments subjectedto

    rapid drawdown.

    Acknowledgements

    The first author would like to express his sincere appreciation toDavid Igoe, Tom Doyle and Paul Doherty PhD researchers fromUniversity College Dublin for their help in reviewing this paper.

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    Nomenclature

    Pa: strain energyE: elasticity modulusA: cross section areaEA: axial rigidityL: length of geotextileu: axial displacement along the geotextile

    x0: distance along the geotextileh: total hydraulic headkw: unsaturated hydraulic conductivitykx: unsaturated hydraulic conductivities in x-directionky: unsaturated hydraulic conductivities in y-directionmw: slope of the water volume characteristic curvegw: unit weight of waterQ: volumetric water contentt: timen: porosityS: degree of saturation

    AEV: air-entry valueQr: residual water contentQs: saturated volumetric water contentJ: negative pore water pressurea, n, m: curve fitting parametersks: saturated hydraulic conductivityQp: volumetric water content at the halfway point of the volumetric water content

    function

    Jp: suction at the halfway point of the volumetric water content functionSp: slope of volumetric water content function at the halfway point

    A. Tolooiyan et al. / Geotextiles and Geomembranes 27 (2009) 399405 405

    http://www.ejge.com/2000/Ppr0013/Ppr0013.htmhttp://www.ejge.com/2000/Ppr0013/Ppr0013.htm