effect of geogrid geometry on interface resistance …...size. the geogrid with original aperture...
TRANSCRIPT
Effect of Geogrid Geometry on Interface Resistance in a Pullout Test
Jongwan Eun1, Ph.D., P.E.; Ranjiv Gupta2, Ph.D., P.E.; Jorge G. Zornberg3, Ph.D., P.E.
1Assistant Professor, Univ. of Nebraska-Lincoln, Lincoln, NE. E-mail: [email protected] 2Project Engineer, Geosyntec Consultants, Phoenix, AZ. E-mail: [email protected] 3Professor and W. J. Murray, Jr. Fellow in Engineering, Civil, Architectural & Environmental Engineering, Univ. of Texas at Austin, Austin, TX. E-mail: [email protected]
Abstract
This paper presents the effect of aperture size on the low displacement stiffness response of geogrids subjected to pullout loading. The aperture size of geogrid was varied by cutting ribs of geogrids in the pullout tests. Two types of geogrids were tested at two normal pressures (21 kPa and 35 kPa). The Soil-Geosynthetic Composite (SGC) model was used to compute the low displacement interface stiffness (KSGC) of the geogrids. Based on the analysis of laboratory tests using SGC model, the results showed response of geogrids was highly dependent on the aperture size. The geogrid with original aperture size showed the highest KSGC value. As the size of the aperture increased, the KSGC decreased possibly due to reduction in the passive resistance of transverse members and the loss of confinement at the junctions of the geogrid.
INTRODUCTION
Geogrids have been widely used in stabilization of pavements for several decades. The performance of reinforced flexible pavements is governed by the interaction mechanisms between soil and geosynthetic. The interaction of the geogrid with surrounding soils consists of the passive resistance due to the thickness of rib, the friction of the surface of rib and the confinement of soil in the aperture due to the rib. Generally, the interaction developed between the soil and the reinforcement is a function of soil type, reinforcement type and how they are linked with each other (Teixeira et al. 2007). Actually, these factors are interrelated, and the combined effect of these factors results in complex interactions. Hence, appropriate laboratory test incorporating these variables should be to quantify the interaction mechanisms between the soil and the reinforcement.
Previous studies have focused on investigating the performance of geogrid reinforcement in flexible pavements using laboratory confined tests (Sugimoto et al. 2001, Palmeira 2004, Bergado et al. 2008), because they can provide: (a) the ability to capture the mechanism of lateral restraint; (b) parameters for mechanistic-empirical design; (c) repeatability of test results; (d) a parameter that distinguishes between the performance of various geosynthetics; (e) sensitivity to low displacement
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© ASCE Eun, J., Gupta, R., and Zornberg, J.G. (2017). “Effect of Geogrid Geometry on Interface Resistance in a Pullout Test.” Proceedings of the Geotechnical Frontiers 2017 Conference, Geotechnical Special Publication (GSP) 280, Geo-Institute of ASCE, 12-15 March, Orlando, FL, pp. 236-246.
magnitudes; and (f) convenience to conduct in the laboratory. Based on these advantages, a pullout test in a confined soil with monotonic loading has been used to reduce the variability in test results and to allow for the realistic measurement of the interface mechanisms. The geogrid geometry is a significant factor influencing pullout behavior of geogrid embedded in soils. Geogrid with comparatively large apertures, unlike other reinforcements (e.g. geotextiles) can sustain outer loading by providing both passive and frictional resistance components by transverse and longitudinal members (Teixeira et al. 2007, and Palmeira et al. 2004, 2008). Stress distribution between transverse and longitudinal members of the geogrid is affected by the geogrid geometry. However, there is much uncertainty about the complex influence of geogrid geometry. This research evaluated the effect of the geogrid geometry associated with various factors on the pullout behavior by using pullout stiffness at the interface between the geogrid and soil. The Soil-Geosynthetic Composite (SGC) model was used to illustrate analytically the interfacial mechanism governing reinforced soil with geogrid. The interface stiffness (KSGC) obtained from the model was evaluated to quantify the effect of the geogrid. A series of pullout tests was conducted to examine the pullout behavior of the geogrid in a confined soil and to determine the stiffness. Based on the results, the combined effects of the geogrid geometry associated with the type of the reinforcement, the confining pressure on the specimen, and the orientation of the specimen on the pullout behavior were investigated. SOIL-GEOSYNTHETIC COMPOSITE (SGC) MODEL Geosynthetic load-strain relationship. A load-transfer mechanism of geosynthetic in a confined soil demands to properly simulate the shear stress generated at the interface between the geosynthetic and the soil. To model the mechanism, an infinitesimal geosynthetic element subjected to force (F) in the pullout direction and to the shear stresses (τ) along both surfaces of the geosynthetic element of length (dx) surrounded soil mass can be assumed (Figure 1). Then, the force equilibrium can be given in differential form as follows: ( ) − ( ) − ( ) = 2 ( ) (1)
( ) = ( ) (2)
On the other hand, assuming that strain ε(x) develops in the dx due to the
change in confined force between two points in the element, the confined force and strain are related through confined stiffness (Jc) of the geosynthetic and is given as:
( ) = ∙ ( ) = ( ) (3)
Because the strain developed in the dx can then be related, the F can be
described as a differential form.
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Sub
soilal. the elem Figtest Intprodispintoelem
whlenparbouto tdetval
geothe
bstituting Eq
The abol-geosynthet2009). The soil-geosyn
ment of leng
gure 1. Freet.
terface stiffoposed to placement ao Eq. 3 withment, the for
If the se
ere τy is thegth of geosy
rameters deteundary condthe right termailed derivaidated in Gu
To reaosynthetic at
displaceme
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( )ove expresstic interface equation ass
nthetic interfgth dx in the
e body diag
fness (KSGC
describe that the soil-geh the assumrce at x was (econd partial(e yield shearynthetic andermined by ition in the tm of Eq. 7 aation and thupta (2009). alistically ct low displacents are bein
( ) = (2 gives, = ( ) =ion is a secbehavior du
sociates the face in termpullout test
grams for g
C). The Soilhe relationseosynthetic
mption of theobtained as ) = ( )
l derivative e) =r stress. The
d independensolving the test (Gupta 2as incorporahe determin
capture the cement magnng measured
) = (
( )
cond-order during the puldisplacemens of confine(Gupta 2009
geosynthetic
l-Geosyntheship betweeinterface (Ge constant sfollow. =
equation, Eq=e τy is consisnt of the dissecond deriv2009, Zornb
ating the givnation of th
interactionnitudes, it isd during the
)
differential ellout test (Gnt, w(x) withed stiffness J9, Zornberg
c element of
etic Composen the con
Gupta 2009)shear stress
q. 5 is solved= ( )
stent at a posplacement. vative equatberg et al. 20ven constanthe paramete
ns developes necessary t pullout test
equation govGupta 2009, Z
h the τ(x) dJc, for the get al. 2009)
f length dx
site (SGC) nfined force. As substitualong the g
d, the w(x) is
oint along thC1 and C2 ation with the009). The ws and conditer was des
ed betweento compute ft. Eqs. 6 an
(4)
(5)
verning the Zornberg et eveloped at
geosynthetic.
in pullout
model was e and the uting Eq. 5
geosynthetic
(6)
s given,
(7)
he confined are constante initial and
w(x) is equal tions. More scribed and
n soil and force where nd 7 can be
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used to determine the response of geosynthetic for given displacement increment. This can then be translated to quantify the soil-geosynthetic response to obtaining a measurement for a lateral restraint mechanism developed in the reinforced flexible pavements by using pullout test data. Thus, the equations were solved to obtain the relation between confined force and displacement in terms of model parameters as shown below. ( ) = 4 ∙ ∙ ( ) = ∙ ( ) (8)
The force and displacement at any given point x throughout the geosynthetic can be related by model parameters i.e., the yield shear stress (τy) and confined stiffness (Jc) of the soil-geosynthetic system. A coefficient of interface stiffness (KSGI) enables to evaluate soil-geosynthetic interaction (Gupta 2009, Zornberg et al. 2009). MATERIALS AND METHODS
Geogrid. Two different geogrid products, GG1 and GG2 were used as a reinforcement for the pullout test series (Figure 2). GG1 is comprised of knitted polypropylene (PP) yarns, crafted into a stable, interlocking pattern, and then coated for protection from installation damage. On the other hand, GG2 is an integrally formed, punched-and-drawn polypropylene (PP) grid featuring raised protrusions at each rib intersection to provide a structural abutment when placed between soil layers. The properties of GG1 and GG2 were listed in Table 1. The geogrids were prepared with dimensions of 0.6 m length and 0.45 m width for pullout test (ASTM D6706). Four different geometries―the original geogrid, the geogrid with only half of the transverse members, the geogrid with a doubled opening size and the geogrid with only longitudinal members―were used in this study. The designated specimen was prepared by cutting transverse members using pliers. The GG2 with half transverse members was not tested due to its large aperture size. LVDT. Five LVDTs were used to measure displacements at locations with a horizontal spacing of 100, 200, 300, 450, and 600 mm from the front end of the specimen, named LVDT 1 to 5. The displacement profile throughout the length of the geogrid could be monitored by installing LVDTs at various locations. The displacement rate of testing was set to 1mm/min, (ASTM D6706). The displacement of the specimen occurred as the specimen started to move due to pullout force. Soil. Monterey No. 30 sand was used as the backfill material for pullout testing. Monterey No. 30 sand is a clean and poorly graded, which was classified as SP according to the Unified Soil Classification System (USCS) (Zornberg et al. 1998). The test was conducted at the relative density of 50%.
Pullout test. The pullout test equipment consisted of a steel box (1.5 m × 0.6 m × 0.3 m), reaction frame, and applying pullout system (Figure 3a). The front end of the box had an opening of 50 mm and had two sleeves of 75 mm length to minimize the influence of the frontal box wall on pullout test results. In the front of the pullout box, the roller grips and its support trolley were designed to avoid stress concentration at
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the geosynthetic reinforcement. In the pullout box, the steel plates were used as the reaction frame system with wooden boards (Figure 3b). Six air cylinders were used for applying normal pressure on the surface of soils. The reaction frame system is a reliable way to apply a constant confining pressure on top of the geosynthetic specimen. Two hydraulic pistons were attached to the both side of the pullout box to apply pullout force on the specimen. The electric pump enabled better control over the rate of testing, since it could be independently controlled using the flow valve attached to it. The displacement transducers were attached to the system enabling faster data acquisition.
Table 1. Properties of geogrids used in the study.
Property Test method Units GG1 GG2
Rib shape Observation - Rectangular Rectangular
Rib Thickness Calipers mm 0.5 0.76
Norminal Apeture size
Calipers mm 15 × 15 25 × 33
Junction efficiency GRI-GG2-87 % - 93
Flexural Rigidity ASTM D1388-
96 mg-cm 100,000 250,000
Aperture Stability modulus
Kinney (2001) m-N/deg 0.44 0.32
Minimum true initial modulus ASTM D6637-
01
kN/m 250 250
MD kN/m 350 400
XD Tensile strength at
2% strain ASTM D6637-01
kN/m 5 4.1
MD kN/m 7 6.6
XD
Figure 2. Geogrid used for a pullout test: (a) GG1; and (b) GG2.
(b)(a)
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A tserithre
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ULLOUT BE
gure 4a showertures) and ording of theth increasingcurred first, a
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VDT 1 is the
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EHAVIOR
ws the frontathe displace
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ersus the dishe results flg the test. Also increaseid started tohighest. The
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OF GEOGR
al pullout foement obtains started aftedisplacemenreasing rate oT 5 located adisplacementdent on the ullout box we, but the ithe failure (t
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o be generate initial pull
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RID IN CO
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rate of the VDT placedce increasedld decrease
finishing the ement, w(x) ee Figure 1
the front of testing. The and geogrid
the frontal een the soil lacement at roached the
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platdecgiv
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PUTY
Figusinorigthe wasmemmemwitforcthe pulincrcleafor lessthe 35 apebropregeoin b
teau after thcreased with ven test was
Figure 4. Frofunction o
ULLOUT BYPE, CONFI
gure 5a presng GG1 witginal geogrihighest valu
s similar to mbers that mmbers. Signth double apce with timetensile stren
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DIFFERENTAND ORIEN
f the frontalt LVDT 2 wgeometry anThe force of G1 because ere not elimie pullout resdinal membeand GG2 at as very simil
milar results2. The ultimbtained for G1 might be hginal GG1. Fnder two difent. Unfortue was not obrred. The pnder low cobjected to thith changing
f frontal pulmaximum pul
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T GEOMENTATIONS
l pullout forwith time. Tnd the half trf GG1 with h
both the frinated by re
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mate pullout sGG1 was hihigher due toFigure 5c shfferent confi
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pullout forceonfining preshe high presg the geome
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ETRIES, GS OF GEOG
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cause the spee under highssure. The essure. The puetry. In Figu
ignificantly value for the
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GEOGRID GRID
me obtained force of the
members arese membersthe bearing f transverse
for the GG1 ntal pullout
d. Although ondition, the f the GG1 s not shown hat obtained ore ribs and mparison of ures (21 and
for doubleecimen was h confiningeffect of the ullout forceure 5d, the
(b)
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fronAltpulidenapeforcdireMDmemthe
Fig
(pre PU In geobe forc
ntal pullout though the pllout resistanntical result
erture shape ce in the maection (XD).D in the casmbers. The specimen.
gure 5. Com(aperture) oessure of 21
ULLOUT BE
the SGC osynthetic inobtained froce (Eq. 8) a
(a)
(c)
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achine direct. However, tse using the reason is du
mparison of of GG1 (b) g and 35 kPa
EHAVIOR A
model, an nteraction waom a slope inand displace
ime using a of transverseing to the
the stress cimen. In thetion (MD) isthe pullout fo
geogrid incue to the con
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AT SMALL
interface sas defined an the plot ofement as sho
different orie and longitorientationwas distribe case of uss slightly higforce of the Xcluding doubnfinement o
lout force ce of GG1 anifferent orie
L DISPLAC
tiffness parat low displaf the relationown in Figu
ientation of ttudinal memof the spe
buted differesing originalgher than thXD becomesble aperture
of the soil in
curves for: (nd GG2; (c)entation of
CEMENT R
rameter (KS
acement (< 2nship betweeure 6. The s
(b)
the GG2 wambers are id
cimen doesently accordl specimen, at in the cros higher thane and only ln the square
(a) different) different cGG2 for M
RANGE
SGC) to qua2.5 mm). Then the squareslope can be
as compared.dentical, the s not show ding to the the pullout
oss machine n that of the longitudinalaperture of
t geometry onfining
MD and XD.
antify soil-he KSGC can ed confined e computed
(d)
.
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fromfonthe of gpretest Effobtloncasgeoonlthatpul EffcomKSG
diffcasgeoto tresuresi
Fty
pre
Effcomof b
G
m the regrental pullout f
plot of KSG
geogrid geomssure on theting data in a
fect of geogtained for Gngitudinal on
es involvingogrid is highly longitudint of GG2. Gllout force di
fect of geomparison of GC in high coference of Ke of the orig
ogrid includithe ribs is apults, the effistance when
Figure 6. Coype betweenessure betw
fect of geomparison of both the orig
GG1 (orig.)
GG2 (orig
GG1 (longi.)
ession analyforces (FiguC shows a remetry on pule specimen, all cases wer
grid geomeGG1 and GGnly membersg different g
her than that nal membersG1 has stronistributes mo
ogrid geomKSGI under
onfining preKSGC betweenginal geogriding longitudipplied stronfect of trann comparativ
omparison on GG1 and Geen 21 and
MD and
ogrid geomKSGC for dif
ginal and the
g.)
GG2 (longi.)
)
(a)
sis with leaure 5c) decreelatively linellout behaviothe geogrid
re interpreted
etry and gG2 with the
. The slope ogeometries. obtained for, the value o
nger longitudore to the lon
metry and different co
essure was hn high and ld without alinal only megly when th
nsverse memvely high con
of KSGC of diGG2 in 21 k35 kPa of Gd XD in 21
metry and fferent orien
e double aper
35 kPa
21 kPa (
ast square meased with iear slope witor as well as
d orientationd.
eogrid typeoriginal witof the GG1 iThe KSGC o
r GG2 by apof KSGC of Gdinal membengitudinal m
confiningonfining prehigher than tlow confininltering the apembers. Thishe transversember contribnfining pres
ifferent geokPa of confiGG1; and (ckPa of conf
geogrid orntation of gerture size. Th
a (orig.)
21 kPa (orig
35 kPa (lo
longi.)
method. The increasing dthin 2.5 mms other factorn, and the ge
e. Figure 5thout alterinis stiffer thaobtained forpproximatelyGG1 is arouners than tran
members in G
pressure. essure such athat in low cng pressure waperture thans was becaue members abutes much ssure is appli
ograid geomining pressuc) the orientfining pressu
rientation. eogrid combihe GG2 was
g.)
ongi.)
(b)
increasing displacement
m. To quantifrs such as theogrid type,
5a comparedng the apertuan that of ther GG1 for ty 50%. Hownd six times nsverse memGG1 than GG
Figure 6b as 21 and 3confining prwas much la
n that in the use the confinare present.
more to toied to the ge
metry: (a) theure; (b) the tation of GGure.
Figure 6c ined with ths tested unde
XD (orig.)
MD (orig.)
XD (
M
rate of the t. However, fy the effect he confining
the pullout
d the KSGC
ure and the e GG2 in all the original
wever, in the higher than
mbers, so the G2.
shows the 35 kPa. The ressure. The arger in the case of the
nement due From these
otal pullout ogrid.
e geogrid confining
G2 between
shows the he geometry er 21 kPa of
XD (doub.)
long.)
MD (doub.)
MD (long.)
(c)
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confining pressure. The area of transverse ribs in the original case without altering the aperture was increased if the specimen was tested in the MD instead of the XD. However, as the number of transverse member decreases and the area of aperture increases in other cases to control the geometry, the values of KSGC are reduced rapidly in the MD, because the confinement due to transverse members for passive resistance is less than in the XD. As in the previous case, the confinement due to ribs was found to strongly influence the KSGC. CONCLUSIONS This paper presents the effect of geogrid geometry, geogrid type, confining pressure, and geogrid orientation on the pullout behavior of geogrid reinforced soil. Based on results of a series of pullout tests, the interface stiffness (KSGC) was evaluated at small displacement range (< 2.5 mm). The value of KSGC was found to decrease with increasing aperture size of the geogrid specimen. This was to the reduction in the passive resistance of transverse members of the geogrid and loss of confinement at the junctions. The difference of KSGC between high and low confining pressure was much larger in the case of the original geogrid than that in the case of the geogrid with only longitudinal member. The values of KSGC are reduced rapidly in the MD because the confinement due to transverse members for passive resistance is less than in the XD Based on the results obtained in this study, it was found that geogrid geometry strongly influences the pullout behavior of geogrids under small displacements. REFERENCES Bergado, D.T., Teerawattanasuk, C., (2008), “2D and 3D numerical simulations of
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Sugimoto, M., Alagiyawanna, A.N.M. and Kadoguchi, K. (2001), “Influence of rigid and flexible face on geogrid pullout tests”, Geotextiles and Geomembranes, Vol. 19, No.5, 257-277.
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Zornberg, J.G., Ferreira, J.A.Z., Gupta, R.V., Joshi, R.V., and Roodi, G.H. (2009). Geosynthetic-Reinforced Unbound Base Courses: Quantification of the Reinforcement Benefits. Center for Transportation Research (CTR), Report No. FHWA/TX-10/5-4829-1, Austin, Texas, December 2009, Revised February 2012, 170 p.
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