REGEO ‘2007 - 1 -
New Concepts in Geosynthetic-Reinforced Soil
Jorge G. Zornberg, Ph.D., P.E.
The University of Texas at Austin
ABSTRACT: Traditional soil reinforcing techniques involve the use of continuous geosynthetic
inclusions such as geogrids and geotextiles. The acceptance of geosynthetics in reinforced soil
construction has been triggered by a number of factors, including aesthetics, reliability, simple
construction techniques, good seismic performance, and the ability to tolerate large deformations
without structural distress. Following an overview of conventional reinforced soil applications, this
paper focuses on recent advances in reinforced soil technology. Examples include advances in
reinforced soil design for conventional loading (e.g. validation of analysis tools), advances in
design for unconventional loading (e.g., reinforced bridge abutments), and advances in
reinforcement materials (e.g., polymeric fiber reinforcements).
KEYWORDS: Soil Reinforcement, Shear Strength, Fiber-Reinforcement.
1 INTRODUCTION
Geosynthetic inclusions within a soil mass can
provide a reinforcement function by developing
tensile forces which contribute to the stability of
the geosynthetic-soil composite (a reinforced
soil structure). Design and construction of stable
slopes and retaining structures within space
constrains are aspects of major economical
significance in geotechnical engineering
projects. For example, when geometry
requirements dictate changes of elevation in a
highway project, the engineer faces a variety of
distinct alternatives for designing the required
earth structures. Traditional solutions have been
either a concrete retaining wall or a
conventional, relatively flat, unreinforced slope.
Although simple to design, concrete wall
alternatives have generally led to elevated
construction and material costs. On the other
hand, the construction of unreinforced
embankments with flat slope angles dictated by
stability considerations is an alternative often
precluded in projects where design is controlled
by space constraints.
Geosynthetics are particularly suitable for soil
reinforcement. Geosynthetic products typically
used as reinforcement elements are nonwoven
geotextiles, woven geotextiles, geogrids, and
geocells. Reinforced soil vertical walls generally
provide vertical grade separations at a lower cost
than traditional concrete walls. Reinforced wall
systems involve the use of shotcrete facing
protection or of facing elements such as precast
or cast-in-place concrete panels. Alternatively,
steepened reinforced slopes may eliminate the
use of facing elements, thus saving material
costs and construction time in relation to vertical
reinforced walls. As indicated in Figure 1 a
reinforced soil system generally provides an
optimized alternative for the design of earth
retaining structures.
A reduced scale geotextile-reinforced slope
model built using dry sand as backfill material.
The maximum slope inclination of an
unreinforced sand under its own weight is the
angle of repose of the sand, which is well below
the inclination of the slope face of the model.
Horizontal geotextile reinforcements placed
within the backfill provided stability to the steep
sand slope. In fact, not only the reinforced slope
model did not fail under its own weight, but its
failure only occurred after the unit weight of the
backfill was increased 67 times by placing the
model in a geotechnical centrifuge (Zornberg et
al., 1998).
The use of inclusions to improve the mechanical
properties of soils dates to ancient times.
However, it is only within the last quarter of
century or so (Vidal, 1969) that analytical and
Zornberg, J.G. (2007). “New Concepts in Geosynthetic-Reinforced Soil.” Keynote lecture, Proceedings of the Fifth Brazilian Symposium on
Geosynthetics, Geossinteticos 2007, and of the Sixth Brazilian Congress on Environmental Geotechnics, REGEO `2007, Recife, Brazil, 18-21
June, pp. 1-26 (CD-ROM).REGEO ‘2007 - 2 -
experimental studies have led to the
contemporary soil reinforcement techniques.
Soil reinforcement is now a highly attractive
alternative for embankment and retaining wall
projects because of the economic benefits it
offers in relation to conventional retaining
structures. Moreover, its acceptance has also
been triggered by a number of technical factors,
that include aesthetics, reliability, simple
construction techniques, good seismic
performance, and the ability to tolerate large
deformations without structural distress. The
design of reinforced soil slopes is based on the
use of limit equilibrium methods to evaluate
both external (global) and internal stability of
the structure. The required tensile strength of
the reinforcements is selected during design so
that the margins of safety, considering an
internal failure are adequate. Guidance in soil
reinforcement design procedures is provided
by Elias et al. (2001).
a) Concrete retaining b) Reinforced wall d) Unreinforced slope c) Reinforced slope
wall
Increasing construction cost
Increasing right-of-way
Figure 1. Reinforcement function of geosynthetics used to optimize the design of earth retaining structures.
2 VALIDATION OF DESIGN TOOLS
2.1 Overview
The use of inclusions to improve the mechanical
properties of soils dates to ancient times.
However, it is only within the last three decades
or so (Vidal 1969) that analytical and
experimental studies have led to the
contemporary soil reinforcement techniques.
Soil reinforcement is now a highly attractive
alternative for embankment and retaining wall
projects because of the economic benefits it
offers in relation to conventional retaining
structures. Moreover, its acceptance has also
been triggered by a number of technical factors,
which include aesthetics, reliability, simple
construction techniques, good seismic
performance, and the ability to tolerate large
deformations without structural distress. The
design of reinforced soil slopes is based on the
use of limit equilibrium methods to evaluate
both external (global) and internal stability.
After adopting the shear strength properties of
the backfill material, the required tensile strength
of the reinforcements can be defined in the
design so that the margin of safety is adequate.
Geosynthetics are classified as extensible
reinforcements. Consequently, the soil strength
may be expected to mobilize rapidly, reaching
its peak strength before the reinforcements
achieve their ultimate strength. This rationale
has led to some recommendations towards the
adoption of the residual shear strength for the
design of geosynthetic-reinforced slopes. This is
the case of commonly used design methods such
as those proposed by Jewell (1991) and
Leshchinsky and Boedeker (1989). SeveralREGEO ‘2007 - 3 -
agencies have endorsed the use of residual shear
strength parameters in the design of reinforced
soil structures, as summarized in Table 1.
Zornberg and Leshchinsky (2001) present a
review of current design criteria used by
different agencies for geosynthetic-reinforced
walls, geosynthetic-reinforced slopes, and
embankments over soft soils.
Table 1. Summary of Guidelines on Selection of Soil Shear Strength Parameters for Geosynthetic-Reinforced Soil
Design
Method/Agency Shear Strength
Parameters
Reference
Jewell’s Method Residual Jewell (1991)
Leshchinsky and Boedeker’s method Residual Leshchinsky and
Boedeker (1989)
Queensland DOT, Australia Residual RTA (1997)
New South Wells, Australia Residual QMRD (1997)
Bureau National Sols-Routes (draft French
Standard)
Residual Gourc et al. (2001)
Federal Highway Administration (FHWA),
AASHTO
Peak Elias et al. (2001),
AASHTO 1996
National Concrete Masonry Association Peak NCMA (1997, 1998)
GeoRio, Brazil Peak GeoRio (1989)
Canadian Geotechnical Society Peak Canadian Geotechnical
Society (1992)
German Society of Soil Mechanics and
Geotechnical Engineering
Peak EBGEO (1997)
Geotechnical Engineering Office, Hong
Kong
Peak GCO (1989), GEO (1993)
Public Works Research Center, Japan Peak Public Works Research
Center (2000)
British Standards, United Kingdom Peak British Standard
Institution (1995)
Leshchinsky’s hybrid method Hybrid Leshchinsky (2001)
The use of the peak friction angle has been
common practice in the US for the design of
geosynthetic-reinforced slopes. Guidance in soil
reinforcement design procedures has been
compiled by several federal agencies in the US,
including the American Association of State
Highway and Transportation Officials
(AASHTO 1996), and the Federal Highway
Administration (Elias et al. 2001). Design
guidance is also provided by the National
Concrete Masonry Association (NCMA 1997),
possibly the only industry manual of soil
reinforcement practice. The above mentioned
design guidance manuals recommend the use of
the peak friction angle in the limit equilibrium
analyses. Other agencies that have also endorsed
the use of peak shear strength parameters in the
design of reinforced soil structures are
summarized in Table 1.
A hybrid approach was recently proposed by
Leshchinsky (2000, 2001). Central to his
approach is the use of a design procedure in
which peak soil shear strength properties would
be used to locate the critical slip surface, while
the residual soil shear strength properties wouldREGEO ‘2007 - 4 -
subsequently be used along the located slip
surface to compute the reinforcement
requirements.
In order to address the controversial issue
regarding selection of shear strength properties
in reinforced soil design, this paper presents
experimental evidence on failed reinforced
slopes. Specifically, the experimental
information obtained from centrifuge modeling
supports the use of peak shear strength
parameters in the design of geosyntheticreinforced soil structures. The perceived
conservatism in design is also not supported by
the generally observed good performance of
monitored reinforced soil structures.
2.2 Centrifuge Testing Program
Limit equilibrium analysis methods have been
traditionally used to analyze the stability of
slopes with and without reinforcements.
However, to date, limit equilibrium predictions
of the performance of geosynthetic-reinforced
slopes have not been fully validated against
monitored failures. This has led to a perceived
overconservatism in their design.
Consequently, an investigation was undertaken
to evaluate design assumptions for
geosynthetic-reinforced slopes (Zornberg et al.
1998a, 2000). The results of centrifuge tests
provide an excellent opportunity to examine
the validity of various assumptions typically
made in the analysis and design of reinforced
soil slopes. This paper presents the aspects of
that study aimed at evaluating the shear
strength properties governing failure of
reinforced soil slopes.
All reinforced slope models in the
experimental testing program had the same
geometry and were built within the same
strong box. A transparent Plexiglas plate was
used on one side of the box to enable side view
of the models during testing. The other walls of
the box were aluminum plates lined with
Teflon to minimize side friction. The overall
dimensions of the geotextile-reinforced slope
models are as shown in Figure 2 for a model
with nine reinforcement layers. Displacement
transducers are also indicated in the figure.
Figure 2. Typical centrifuge model.
The number of reinforcement layers in the
models ranged from six to eighteen, giving
reinforcement spacing ranging from 37.5 mm
to 12.5 mm. All models used the same
reinforcement length of 203 mm. The use of a
reasonably long reinforcement length was
deliberate, since this study focused on the
evaluation of internal stability against breakage
of the geotextile reinforcements. In this way,
external or compound failure surfaces were not
expected to develop during testing. As shown
in the figure, the geotextile layers were
wrapped at the slope facing in all models.
Green colored sand was placed along the
Plexiglas wall at the level of each
reinforcement in order to identify the failure
surface. In addition, black colored sand
markers were placed at a regular horizontal
spacing (25 mm) in order to monitor lateral
displacements within the backfill material.
The variables investigated in this study were
selected so that they could be taken into
account in a limit equilibrium framework.
Accordingly, the selected variables were:
Vertical spacing of the geotextile
reinforcements: four different
reinforcement spacings were adopted;
soil shear strength parameters: the same
sand at two different relative densities was
used; and
ultimate tensile strength of the
reinforcements: two geotextiles with
H = 228 mm
L = 203 mm
LP1
LP2
LP3
LP4
LP5
LP6
LVDT1 LVDT2REGEO ‘2007 - 5 -
different ultimate tensile strength were
selected.
Of particular relevance, for the purpose of the
issues addressed in this paper, is the fact that
that the same sand placed at two different
relative densities was used as backfill material
for the centrifuge models. The backfill material
at these two relative densities has different
peak shear strength values but the same
residual shear strength.
The model slopes were built using Monterey
No. 30 sand, which is a clean, uniformly
graded sand classified as SP in the Unified Soil
Classification System (Zornberg et al. 1998b).
The particles are rounded to subrounded,
consisting predominantly of quartz with a
smaller amount of feldspars and other
minerals. The average particle size for the
material is 0.4 mm, the coefficient of
uniformity is 1.3, and the coefficient of
curvature is about 1.1. The maximum and
minimum void ratios of the sand are 0.83 and
0.53, respectively. To obtain the target dry
densities in the model slopes, the sand was
pluviated through air at controlled
combinations of sand discharge rate and
discharge height. The unit weights for the
Monterey No. 30 sand at the target relative
densities of 55% and 75% are 15.64 kN/m3 and
16.21 kN/m3, respectively.
Two series of triaxial tests were performed to
evaluate the friction angle for the Monterey
No. 30 sand as a function of relative density
and of confining pressure. The tests were
performed using a modified form of the
automated triaxial testing system developed by
Li et al. (1988). The specimens had nominal
dimensions of 70 mm in diameter and 150 mm
in height and were prepared by dry tamping.
Figure 3 shows the stress strain response
obtained from the series of tests conducted to
evaluate the behavior of Monterey No. 30 sand
as a function of relative density. All tests
shown in the figure were conducted using a
confining pressure of 100 kPa. As can be
observed in the figure, while the sand shows a
different peak shear strength for different
relative densities, the shear stress tends to a
single residual shear strength for large strain
conditions. Figure 4 shows the increase in peak
friction angle with increasing relative density
at a confining pressure of 100 kPa. Of
particular interest are the friction angles
obtained at relative densities of 55% and 75%,
which correspond to the relative density of the
backfill material in the models. The estimated
triaxial compression friction angles (tc) at
these relative densities are 35° and 37.5°,
respectively. Although the tests did not achieve
strain values large enough to guarantee a
critical state condition, the friction angles at
large strains appear to converge to a residual
value (r) of approximately 32.5°. This value
agrees with the critical state friction angle for
Monterey No. 0 sand obtained by Riemer
(1992). As the residual friction angle is mainly
a function of mineralogy (Bolton 1986),
Monterey No. 0 and Monterey No. 30 sands
should show similar r values. The effect of
confining pressure on the frictional strength of
the sand was also evaluated. The results
showed that the friction angle of Monterey
No. 30 decreases only slightly with increasing
confinement. The fact that the friction angle of
this sand does not exhibit normal stress
dependency avoids additional complications in
the interpretation of the centrifuge model tests.
Scale requirement for the reinforcing material
establish that the reinforcement tensile strength
in the models be reduced by N. That is, an
Nth-scale reinforced slope model should be
built using a planar reinforcement having 1/N
the strength of the prototype reinforcement
elements (Zornberg et al. 1998a). Two types of
nonwoven interfacing fabrics, having mass per
unit area of 24.5 g/m2 and 28 g/m2, were
selected as reinforcement. Unconfined ultimate
tensile strength values, measured from widewidth strip tensile tests ASTM D4595, were
0.063 kN/m and 0.119 kN/m for the weaker
and stronger geotextiles, respectively.
Confined tensile strength values, obtained from
backcalculation of failure in the centrifuge
slope models, were 0.123 kN/m and 0.183
kN/m for the weaker and stronger geotextiles,
respectively (Zornberg et al. 1998b). Confined
tensile strength values were used for estimatingREGEO ‘2007 - 6 -
the factor of safety of the models analyzed in
this study under increasing g-levels.
Figure 3. Stress strain behavior of Monterey No. 30 sand
pluviated at different relative densities and tested in
triaxial compression under the same confinement
Figure 4. Friction angle for Monterey No. 30 sand
obtained from triaxial testing at different relative
densities.
2.3 Typical Centrifuge Test Results
The models were subjected to a progressively
increasing centrifugal acceleration until failure
occurred. A detailed description of the
characteristics of the centrifuge testing
program is presented by Zornberg et al.
(1998a). The centrifuge tests can be grouped
into three test series (B, D, or S). Accordingly,
each reinforced slope model in this study was
named using a letter that identifies the test
series, followed by the number of
reinforcement layers in the model. Each test
series aimed at investigating the effect of one
variable, as follows:
Baseline, B-series: Performed to
investigate the effect of the reinforcement
vertical spacing.
Denser soil, D-series: Performed to
investigate the effect of the soil shear
strength on the stability of geosyntheticreinforced slopes. The models in this series
were built with a denser backfill sand but
with the same reinforcement type as in the
B-series.
Stronger geotextile, S-series: Performed to
investigate the effect of the reinforcement
tensile strength on the performance of
reinforced slopes. The models in this series
were built using reinforcements with a
higher tensile strength than in the B-series
but with the same backfill density as in that
series.
The history of centrifugal acceleration during
centrifuge testing of one of the models is
indicated in Figure 5. In this particular test, the
acceleration was increased until sudden failure
occurred after approximately 50 min of testing
when the acceleration imparted to the model
was 76.5 times the acceleration of gravity.
Settlements at the crest of the slope, monitored
by LVDTs, proved to be invaluable to
accurately identify the moment of failure.
Figure 6 shows the increasing settlements at
the top of a reinforced slope model during
centrifuge testing. The sudden increase in the
monitored settlements indicates the moment of
failure when the reinforced active wedge slid
along the failure surface. Figure 7 shows a
typical failure surface as developed in the
centrifuge models. As can be seen, the failure
surface is well defined and goes through the
toe of the reinforced slope.
0
50
100
150
200
250
300
350
0 2 4 6 8 10 12 14 16 18 20
Axial strain (%)
D
r
=52.7%
D
r
=83.3%
D
r
=74%
D
r
=68%
D
r
=57.5%
D
r
=37%
=100 kPa
25
30
35
40
45
20 40 60 80 100
Peak Friction Angle (deg)
Relative Density (%)
Confining stress: 100 kPatime (min)
g-level (N)
0
10
20
30
40
50
60
70
80
0 10 20 30 40 50 60
Failure
Figure 5. G-level (N) versus time during centrifuge
testing.
g-level (N)
Vertical displacement (mm) .
5 0
10
15
20
25
30
35
40
0 10 20 30 40 50 60 70 80
LVDT1
LVDT2
Failure
Figure 6. Settlements at the crest of a reinforced slope
model.
Figure 7. Failed geotextile-reinforced slope model.
Following the test, each model was carefully
disassembled in order to examine the tears in
the geotextile layers. Figure 8 shows the
geotextiles retrieved after centrifuge testing of
a model reinforced with eighteen geotextile
layers. The geotextile at the top left corner of
the figure is the reinforcement layer retrieved
from the base of the model. The geotextile at
the bottom right corner is the reinforcement
retrieved from the top of the model. All
retrieved geotextiles show clear tears at the
location of the failure surface. The pattern
observed from the retrieved geotextiles shows
that internal failure occurred when the tensile
strength on the reinforcements was achieved.
The geotextile layers located towards the base
of the slope model also showed breakage of the
geotextile overlaps, which clearly contributed
to the stability of the slope. No evidence of
pullout was observed, even on the short
overlapping layers.
Figure 8. Geotextile reinforcements retrieved after
testing.
2.4 Effect of Backfill Shear Strength on the
Experimental Results
The criteria for characterizing reinforcements
as extensible or inextensible has been
established by comparing the horizontal strain
in an element of reinforced backfill soil
subjected to a given load, to the strain required
to develop an active plastic state in an element
of the same soil without reinforcement
(Bonaparte and Schmertmann 1987).
Accordingly, reinforcements have been
typically classified as:
extensible, if the tensile strain at failure in
the reinforcement exceeds the horizontal
extension required to develop an active
plastic state in the soil; or as
inextensible, if the tensile strain at failure
in the reinforcement is significantly less
than the horizontal extension required to
develop an active plastic state in the soil.REGEO ‘2007 - 8 -
The geotextiles used to reinforce the centrifuge
model slopes are extensible reinforcements.
The effect of reinforcement spacing on the
stability of the reinforced slope models, as
indicated by the measured g-level at failure Nf,
is shown in Figure 9. The number of
reinforcement layers n in the figure includes
the total number of model geotextiles
intersected by the failure surface (i.e. primary
reinforcements and overlaps intersected by the
failure surface). The overlaps intersected by
the failure surface developed tensile forces and
eventually failed by breakage and not by
pullout. The figure shows that a well-defined
linear relationship can be established between
the number of reinforcement layers and the glevel at failure. As the fitted lines for each test
series passes through the origin, the results in
each test series can be characterized by a single
n/ Nf ratio.
Figure 9. G-level at failure for the centrifuge models.
Models in the B- and D-series were reinforced
using the same geotextile reinforcement, but
using sand backfill placed at two different
relative densities (55 and 75%). As mentioned,
the Monterey sand at these two relative
densities has the same soil residual friction
angle (32.5°) but different peak friction angles
(35° and 37.5°). As shown in Figure 9, models
in the D-series failed at higher g-levels than
models in the B-series built with the same
reinforcement spacing and reinforcement type.
Since the backfill soil in models from the Dand B-series have the same residual soil shear
strength, the higher g-level at failure in the
D-series models is due to the higher peak soil
shear strength in this test series.
Analysis of the data presented in this figure
emphasizes that the use of a single residual
shear strength value, common to the two
backfill materials used in the test series, can
not explain the experimental results. Instead,
the experimental results can be explained by
acknowledging that the stability models
constructed with the same reinforcement layout
and the same sand backfill, but placed at
different densities, is governed by different
shear strength values. Indeed, limit equilibrium
analyses (Zornberg et al. 1998b) indicated that
the shear strength value that should be used in
the analysis of these slope failures is the plain
strain peak shear strength of the backfill.
The experimental results indicate that the
stability of structures with extensible
reinforcements is governed by the peak shear
strength and not by the residual shear strength
of the backfill soil. A plausible explanation of
these experimental results is that, although the
soil shear strength may have been fully
mobilized along certain active failure planes
within the reinforced soil mass, shear
displacements have not taken place along these
failure surfaces. That is, although the soil may
have reached active state due to large
horizontal strains because of the extensible
nature of the reinforcements, large shear
displacements (and drop from peak to residual
soil shear strength) only take place along the
failure surface during final sliding of the active
reinforced wedge (Zornberg et al. 1998b).
An additional way of evaluating these
experimental results is by using dimensionless
coefficients, which have been used in order to
develop design charts for geosyntheticreinforced soil slopes (Schmertmann et al.
1987, Leshchinsky and Boedeker 1989, Jewell
1991). The validity of the proposed
5 0
10
15
20
25
0 10 20 30 40 50 60 70 80
G-level at Failure (Nf)
B6
B 9
B 12
B18
D6
S6
S9
D12REGEO ‘2007 - 9 -
normalization can be investigated from the
centrifuge results of this study. For a reinforced
slope model that failed at an acceleration equal
to Nf times the acceleration of gravity, a
dimensionless coefficient K can be estimated
as follows:
1 N
.
2 H
K = n T .
f
ult 2
(1)
where n is the number of reinforcements, Tult is
the reinforcement tensile strength, H is the
slope height, Nf is the g-level at failure from
the centrifuge test, and is the sand unit
weight. The value of n used in Equation 1
includes the number of overlaps that were
intersected by the failure surface in the
centrifuge slope models in addition to the
number of primary reinforcement layers. The
coefficient K is a function of the shear strength
of the soil and of the slope inclination. [i.e. K =
K(,)]. All centrifuge slope models were built
with the same slope inclination .
Consequently, validation of the suggested
normalization requires that a single coefficient
K(,) be obtained for all models built with the
same backfill. If the soil shear strength
governing failure of the models is the residual
strength, a single coefficient K(,) should be
obtained for all models. On the other hand, if
the soil shear strength governing failure is the
peak shear strength, a single coefficient should
be obtained for those models built with sand
placed at the same relative density.
Figure 10 shows the centrifuge results in terms
of (n Tult) (2 / H2) versus the g-level at failure
Nf . The results in the figure show that a linear
relationship can be established for those
models built with sand placed at the same
relative density. As inferred from Equation 1,
the slope of the fitted line corresponds to the
dimensionless RTS coefficient K = K(,).
The results obtained using the centrifuge
models from the B- and S-series, built using
Monterey sand placed at 55% relative density,
define a normalized coefficient K(,) = KB =
KS = 0.084. Similarly, centrifuge results from
the D-series models, built using Monterey sand
at 75% relative density, define a normalized
coefficient K(,) = KD = 0.062. These results
provide sound experimental evidence
supporting the use of charts based on
normalized coefficients for preliminary design
of geosynthetic-reinforced slopes. If failure of
reinforced soil slopes were governed by the
residual soil shear strength, the results of all
centrifuge tests should have defined a single
line. However, as can be observed in the
figure, different normalized coefficients are
obtained for different soil densities. This
confirms that the normalization should be
based on the peak shear strength and not on the
residual shear strength of the backfill material.
Figure 10. Normalized Reinforcement Tension
Summation (RTS) values from centrifuge test results.
2.5 Final Remarks on Validation of Design
Tools
The selection of the backfill shear strength
properties in the design of geosyntheticreinforced soil structures is an issue over which
design guidelines disagree. The main debate
has been over whether the peak or the residual
shear strength of the backfill material should
be adopted for design. The use of residual
shear strength values in the design of
geosynthetic reinforced slopes while still using
peak shear strength in the design of
unreinforced embankments could lead to
7 6 5 4 3 2 1 0
0 10 20 30 40 50 60 70 80
G-level at Failure (Nf)
B6
B9
B12
B18
D6
S6
S9
D12
55% Relative
Density
75% Relative Density
1
K
D
1
K
B = KSREGEO ‘2007 - 10 -
illogical comparisons of alternatives for
embankment design. For example, an
unreinforced slope that satisfies stability
criteria based on a factor of safety calculated
using peak strength, would become
unacceptable if reinforced using inclusions of
small (or negligible, for the purposes of this
example) tensile strength because stability
would be evaluated in this case using residual
soil shear strength values. The main purpose of
this investigation was to provide experimental
evidence addressing this currently unsettled
issue.
The experimental results presented herein
indicate that the soil shear strength governing
the stability of geosynthetic-reinforced soil
slopes is the peak shear strength. A centrifuge
experimental testing program was undertaken
which indicated that reinforced slopes
constructed with the same reinforcement layout
and the same backfill sand, but using different
sand densities failed at different centrifuge
accelerations. That is, nominally identical
models built with backfill material having the
same residual shear strength but different peak
shear strength did not have the same factor of
safety. Since the residual shear strength of the
sand backfill is independent of the relative
density, these results indicate that the soil shear
strength governing stability is the peak shear
strength of the backfill material.
Several design guidance manuals have
implicitly recommended the selection of the
peak shear strength for the design of reinforced
soil slopes. Considering the current debate over
the selection of the soil shear strength in design
and the experimental results presented herein,
design manuals should explicitly endorse
selection of peak shear strength values for the
design of reinforced soil structures. This
approach would not only be consistent with the
observed experimental centrifuge results, but
also with the US practice of using peak shear
strength in the design of unreinforced slopes.
3 GEOSYNTHETIC-REINFORCED
BRIDGE ABUTMENTSF
3.1 Overview
The technology of geosynthetic-reinforced soil
(GRS) systems has been used extensively in
transportation systems to support the selfweight of the backfill soil, roadway structures,
and traffic loads. The increasing use and
acceptance of soil reinforcement has been
triggered by a number of factors, including cost
savings, aesthetics, simple and fast
construction techniques, good seismic
performance, and the ability to tolerate large
differential settlement without structural
distress. A comparatively new use of this
technology is the use of GRS systems as an
integral structural component of bridge
abutments and piers. Use of a reinforced soil
system to directly support both the bridge (e.g.
using a shallow foundation) and the
approaching roadway structure has the
potential of significantly reducing construction
costs, decreasing construction time, and
smoothing the ride for vehicular traffic by
eliminating the “bump at the bridge” caused by
differential settlements between bridge
foundations and approaching roadway
structures.
The most prominent GRS abutment for bridge
support in the U.S. is the recently-opened-totraffic Founders/Meadows Parkway bridge,
which crosses I-25 approximately 20 miles
south of downtown Denver, Colorado (Figure
11). Designed and constructed by the Colorado
Department of Transportation (CDOT), this is
the first major bridge in the United States to be
built on footings supported by a geosyntheticreinforced system, eliminating the use of
traditional deep foundations (piles) altogether.
Phased construction of the almost 9-m high,
horseshoe-shaped abutments, located on each
side of the highway, began July 1998 and was
completed twelve months later. Significant
previous research by FHWA and CDOT on
GRS bridge abutments, which has
demonstrated their excellent performance and
high load-carrying capacity, led to the
construction of this unique structure.REGEO ‘2007 - 11 -
Figure 11. View of the Founders/Meadows GRS bridge abutments near Denver, Colorado.
The performance of bridge structures
supported by GRS abutments has not been
tested under actual service conditions to merit
acceptance without reservation in highway
construction. Consequently, the
Founders/Meadows structure was considered
experimental and comprehensive material
testing, instrumentation, and monitoring
programs were incorporated into the
construction operations. Design procedures,
material characterization programs, and
monitoring results from the preliminary (Phase
I) instrumentation program are discussed by
Abu-Hejleh et al. (2000). Large-size direct
shear and triaxial tests were conducted to
determine representative shear strength
properties and constitutive relations of the
gravelly backfill used for construction. Three
sections of the GRS system were instrumented
to provide information on the structure
movements, soil stresses, geogrid strains, and
moisture content during construction and after
opening the structure to traffic.
3.2 Past experiences in GRS bridge
abutments
Although the Founders/Meadows structure is a
pioneer project in the U.S. involving
permanent GRS bridge abutments for highway
infrastructure, significant efforts have been
undertaken in Japan, Europe and Australia
regarding implementation of such systems in
transportation projects. Japanese experience
includes preloaded and prestressed bridge piers
(Tatsuoka et al. 1997, Uchimura et al. 1998)
and geosynthetic-reinforced wall systems with
continuous rigid facing for railway
infrastructure (Kanazawa et al. 1994, Tateyama
et al. 1994). European experience includes
vertically loaded, full-scale tests on
geosynthetic reinforced walls constructed in
France (Gotteland et al. 1997) and Germany
(Brau and Floss 2000). Finally, Won et al.
(1996) reported the use of three terraced
geogrid-reinforced walls with segmental block
facing to directly support end spans for a major
bridge in Australia.
The experience in the U.S. regarding
geosynthetic-reinforced bridge abutments for
highway infrastructure includes full-scale
demonstration tests conducted by the Federal
Highway Administration (FHWA) (e.g. Adams
1997, 2000) and by CDOT (e.g. Ketchart and
Wu 1997). In the CDOT demonstration project,
the GRS abutment was constructed with
roadbase backfill reinforced with layers of a
woven polypropylene geotextile placed at a
spacing of 0.2 m. Dry-stacked hollow-cored
concrete blocks were used as facing. A vertical
surcharge of 232 kPa was applied to the 7.6 m
high abutment structure. The measured
immediate maximum vertical and lateral
displacements were 27.1 mm and 14.3 mm,
respectively. The maximum vertical and lateral
creep displacements after a sustained vertical
surcharge pressure of 232 kPa, applied duringREGEO ‘2007 - 12 -
70 days, were 18.3 mm and 14.3 mm,
respectively. The excellent performance and
high loading capacity demonstrated by these
geosynthetic-reinforced soil abutments with
segmental block facing convinced CDOT
design engineers to select GRS walls to
support the bridge abutment at the
Founders/Meadows structure.
3.3 Description of the GRS bridge abutment
The Founders/Meadows bridge is located 20
miles south of Denver, Colorado, near Castle
Rock. The bridge carries Colorado State
Highway 86, Founders/Meadows Parkway,
over U.S. Interstate 25. This structure,
completed by CDOT in July of 1999, replaced
a deteriorated two-span bridge structure. In this
project, both the bridge and the approaching
roadway structures are supported by a system
of geosynthetic-reinforced segmental retaining
walls. Figure 12 shows a picture of one of the
segmental retaining wall systems, located at
the east side of the bridge. This figure shows
the bridge superstructure supported by the
“front MSE wall,” which extends around a 90-
degree curve into a “lower MSE wall”
supporting the “wing wall” and a second tier,
“upper MSE wall”.
Photo 12. View of the Southeast side of the completed Founders/Meadows bridge abutment.
Each span of the new bridge is 34.5 m long and
34.5 m wide, with 20 side-by-side prestressed
box girders. The new bridge is 13 m longer and
25 m wider than the previous structure,
accommodating six traffic lanes and sidewalks
on both sides of the bridge. A typical
monitored cross-section through the “front
MSE wall” and “abutment wall” transmits the
load through abutment walls to a shallow strip
footing placed directly on the top of a geogridreinforced segmental retaining wall. The
centerline of the bridge abutment wall and
edge of the foundation are located 3.1 m and
1.35 m, respectively, from the facing of the
front MSE wall. A short reinforced concrete
abutment wall and two wing walls, resting on
the spread foundation, confine the reinforced
backfill soil behind the bridge abutment and
support the bridge approach slab. The bridge is
supported by central pier columns along the
middle of the structure, which in turn are
supported by a spread footing founded on
bedrock at the median of U.S. Interstate 25.
When compared to typical systems involving
the use of deep foundations to support bridge
structures, the use of geosynthetic-reinforced
systems to support both the bridge and the
approaching roadway structures has the
potential to alleviate the “bump at the bridge”
Upper
MSE
Wall
Girder Wing Wall
Front MSE Wall
Lower
MSE
Wall
Instrumentation BoxREGEO ‘2007 - 13 -
problem caused by differential settlements
between the bridge abutment and approaching
roadway. In addition, this approach also allows
for construction in stages and comparatively
smaller construction working areas. Several of
the common causes for development of bridge
bumps were addressed in the design of the
Founders/Meadows structure. The main cause
of uneven settlements in typical systems is the
use of different foundation types. That is, while
the approaching roadway structure is typically
constructed on compacted backfill soil
(reinforced or not), the bridge abutment is
typically supported on stronger soils by deep
foundations. The roadway approach
embankment and the bridge footing were
integrated at the Founders/Meadows structure
with an extended reinforced soil zone in order
to minimize uneven settlements between the
bridge abutment and approaching roadway. A
second cause of differential settlements can be
attributed to erosion of the fill material around
the abutment wall induced by surface water
runoff. Several measures were implemented in
this project to prevent that surface water, as
well as groundwater, reach the reinforced soil
mass and the bedrock at the base of the fill
(e.g. placement of impervious membranes with
collector pipes). Finally, a third potential cause
of differential settlements is the thermally
induced movements, i.e., expansion and
contraction of bridge girders strongly attached
to the abutment wall (integral abutment). A
compressible 75 mm low-density expanded
polystyrene sheet was placed between the
reinforced backfill and the abutment walls. It
was expected that this system would
accommodate the thermally induced
movements of the bridge superstructure
without affecting the retained backfill.
The backfill soil used in this project includes
fractions of gravel (35%), sand (54.4%), and
fine-grained soil (10.6%). The liquid limit and
plasticity index for the fine fraction of the
backfill are 25% and 4 %, respectively. The
backfill soil classifies as SW-SM per ASTM
2487, and as A-1-B (0) per AASHTO M 145.
The backfill met the construction requirements
for CDOT Class 1 backfill. A friction angle of
34o and zero cohesion were assumed in the
design of the GRS walls. To evaluate the
suitability of these design parameters,
conventional direct shear tests and large size
direct shear and triaxial tests were conducted.
In the conventional tests, the 35% gravel
portion was removed from the specimens, but
in the large-size triaxial and direct shear tests,
the backfill soil specimens included the gravel
portion. The results of conventional direct
shear tests and large size direct shear and
triaxial tests indicate that assuming zero
cohesion in the design procedure and removing
the gravel portion from the test specimens lead
to significant underestimation of the actual
shear strength of the backfill.
The geogrid reinforcements used in this project
were manufactured by the Tensar Corporation.
Three types of geogrid reinforcements were
used: UX 6 below the footing, and UX 3 and
UX 2 behind the abutment wall. The longterm-design-strength (LTDS) of these
reinforcements is 27 kN/m, 11 kN/m, and 6.8
kN/m, respectively. CDOT specifications
imposed a global reduction factor of 5.82 to
determine the long-term design strength
(LTDS) of the geogrid reinforcements from
their ultimate strength. This global reduction
factor accounts for reinforcement tensile
strength losses over the design life period due
to creep, durability, and installation damage. It
also includes a factor of safety to account for
uncertainties.
3.4 Performance
The instrumentation program was conducted in
two phases (Phases I and II), which
correspond, respectively to the construction of
two phases of the GRS bridge abutment
structure. A pilot instrumentation plan was
conducted during construction of the Phase I
structure in order to obtain information that
will tailor the design of a more comprehensive
monitoring program to be implemented during
Phase II. The Phase I instrumentation program
included survey targets, pressure cells,
jointmeters, and inclinometer. The more
comprehensive Phase II instrumentation
program included monitoring using survey
targets, digital road profiler, pressure cells,REGEO ‘2007 - 14 -
strain gauges, moisture gauges, and
temperature gauges. A view of the
instrumentation plan for Phase II is shown in
Figure 13. The figure shows the four critical
locations that were instrumented in Phase II:
(i) Location A, close to the facing. Data
collected at this location is particularly
useful for guiding the structural design
of the facing and of the connection
between facing and reinforcements.
(ii) Locations B and C along the center and
interior edge of the abutment
foundation. Information collected at
these locations is relevant for the design
of the reinforcement elements.
(iii) Location D, behind the bridge
foundation, and horizontal plane at the
base of the fill. Data measured at these
locations is useful to estimate the
external forces acting behind and below
the reinforced soil mass.
Figure 13. Instrumentation plan of Phase II structure.
A comprehensive discussion of the
instrumentation results, the collection and
analysis of which is under progress, is beyond
the scope of this paper. Results of the
preliminary Phase I instrumentation program
have been reported by Abu-Hejleh et al.
(2000). Some of the relevant findings obtained
based on the information collected so far are
the following:
The measured response from both the
pressure cells and strain gauges correlates
well with the applied loads during the
construction stages.
The maximum geogrid strains experienced
during construction are comparatively very
small (approximately 0.45 %).
Horizontal earth pressures collected at the
facing and of the reinforcement maximum
tensile strains are well below design values.
19
18
17
16
15
29
28 14
27
26 13
25
24 12
23
22 11
21
20 10
19
18 9
17
16 8
15
14 7
13
12 6
11
10 5
98
4
76
3
54
2
32
1
1
Strain Gage Pressure Cell Survey Point Moisture Gage Temperature Gage
Bridge Foundation
Concrete Approach Slab Concrete Roadway
Girder
Bridge Deck
Location A Location B Location C Location D
Bedrock
Two
Gages
Two
Gages
Fi 9 I i L S i 800 (Ph II)
Geogrid Layer #
Front GRS WalllREGEO ‘2007 - 15 -
Most of the straining of the geogrid
reinforcements occurred during
construction of the wall and not during
placement of the bridge surcharge load.
This can be explained by the effect of
compaction operations and presence of
slacks in the geogrid reinforcements. Strain
gauge monitoring results collected so far
suggest that approximately 50% of the total
recorded strains occurred during placement
and compaction of a few lifts of soil above
the geogrid layers (e.g. approximately 2 m
of soil or 40 kPa). The maximum measured
front wall outward displacement induced
by wall construction (before placement of
the bridge superstructure) was 12 mm,
which corresponds to 0.20 % of the wall
height.
The maximum outward displacement
induced by placement of the bridge
superstructure was additional 10 mm,
which corresponds to 0.17% of the wall
height. The maximum settlement of the
bridge footing due to placement of the
bridge superstructure was 13 mm.
The maximum outward displacements
induced after opening the structure to
traffic and until June 2000 (18 months) was
13 mm. These movements correspond to
0.22 % of the wall height. The measured
settlement of the leveling pad supporting
the front wall facing was approximately 5
mm. However, it is important to emphasize
that these movements took place only
during the initial 12 months of service
(until January 2000). Lateral and vertical
movements have been negligible from
January to June 2000.
Elevation profiling and surveying results
show no signs of development of the
“bump at the bridge” problem.
Overall, the performance of the
Founders/Meadows bridge structure, based on
the monitored behavior recorded so far,
showed excellent short- and long-term
performance. Specifically, the monitored
movements were significantly smaller than
those expected in design or allowed by
performance requirements, there were no signs
for development of the “bump at the bridge”
problem or any structural damage, and postconstruction movements became negligible
after an in-service period of 1 year.
4 ADVANCES IN FIBER-REINFORCED
SOIL DESIGN
4.1 Overview
Fiber reinforcement has become a promising
solution to the stabilization of thin soil veneers
and localized repair of failed slopes. Randomly
distributed fibers can maintain strength
isotropy and avoid the existence of the
potential planes of weakness that can develop
parallel to continuous planar reinforcement
elements. The design of fiber-reinforced soil
slopes has typically been performed using
composite approaches, where the fiberreinforced soil is considered a single
homogenized material. Accordingly, fiberreinforced soil design has required nonconventional laboratory testing of composite
fiber-reinforced soil specimens which has
discouraged implementation of fiberreinforcement in engineering practice.
Several composite models have been proposed
to explain the behavior of randomly distributed
fibers within a soil mass (Maher and Gray,
1990, Michalowski and Zhao, 1996, Ranjan et
al., 1996). The mechanistic models proposed
by Gray and Ohashi (1983) and Maher and
Gray (1990) quantify the “equivalent shear
strength” of the fiber-reinforced composite as a
function of the thickness of the shear band that
develops during failure. Information needed to
characterize shear band development for these
models is, however, difficult to quantify
(Shewbridge and Sitar, 1990). Common
findings from the various testing programs
implemented to investigate composite models
include: (i) randomly distributed fibers provide
strength isotropy in a soil composite; (ii) fiber
inclusions increase the “equivalent” shear
strength within a reinforced soil mass; and (iii)
the “equivalent” strength typically shows a
bilinear behavior, which was experimentally
observed by testing of comparatively weak
fibers under a wide range of confining stresses.REGEO ‘2007 - 16 -
A discrete approach for the design of fiberreinforced soil slopes was recently proposed to
characterize the contribution of randomly
distributed fibers to stability (Zornberg, 2002).
In this approach, fiber-reinforced soil is
characterized as a two-component (soil and
fibers) material. Fibers are treated as discrete
elements that contribute to stability by
mobilizing tensile stresses along the shear
plane. Consequently, independent testing of
soil specimens and of fiber specimens, but not
of fiber-reinforced soil specimens, can be used
to characterize fiber-reinforced soil
performance.
This paper initially reviews the main concepts
of the discrete approach and subsequently
validates the framework for design purposes.
4.2 Discrete frame work for fiber
reinforcement
The volumetric fiber content, , used in the
proposed discrete framework is defined as:
V V
=
f
(1)
where Vf is the volume of fibers and V is the
control volume of fiber-reinforced soil.
The gravimetric fiber content, w, typically
used in construction specifications, is defined
as:
f s
w
W W
=
(2)
where Wf is the weight of fibers and Ws is the
dry weight of soil.
The dry unit weight of the fiber-reinforced soil
composite, d , is defined as:
V
W W
=
f s
d
(3)
The contribution of fibers to stability leads to
an increased shear strength of the
“homogenized” composite reinforced mass.
However, the reinforcing fibers actually work
in tension and not in shear. A major objective
of the discrete framework is to explicitly
quantify the fiber-induced distributed tension,
t, which is the tensile force per unit area
induced in a soil mass by randomly distributed
fibers.
Specifically, the magnitude of the fiberinduced distributed tension is defined as a
function of properties of the individual fibers.
In this way, as in analysis involving planar
reinforcements, limit equilibrium analysis of
fiber-reinforced soil can explicitly account for
tensile forces.
The interface shear strength of individual fibers
can be expressed as:
f f = ci,c c ci, tan n,ave (4)
where c and are the cohesive and frictional
components of the soil shear strength and n,ave
is the average normal stress acting on the
fibers. The interaction coefficients, ci,c and ci,,
commonly used in soil reinforcement literature
for continuous planar reinforcement, is adopted
herein to relate the interface shear strength to
the shear strength of the soil. The interaction
coefficients are defined as:
ac
c =
i,c
(5)
tan
tan
,
c =
i
(6)
where a is the adhesive component of the
interface shear strength between soil and the
polymeric fiber, tan is the skin-frictional
component.
The pullout resistance of a fiber of length lf
should be estimated over the shortest side of
the two portions of a fiber intercepted by the
failure plane. The length of the shortest portion
of a fiber intercepted by the failure plane varies
from zero to lf /2. Statistically, the average
embedment length of randomly distributed
fibers, le,ave, can be analytically defined by:
, 4
f
e ave
l
l = (7)
where lf is total length of the fibers.
The average pullout resistance can be
quantified along the average embedment
length, le,ave , of all individual fibers crossing a
soil control surface A. The ratio between the
total cross sectional area of the fibers Af and
the control surface A is assumed to be defined
by the volumetric fiber content . That is:
A A
=
f
When failure is governed by the pullout of the
fibers, the fiber-induced distributed tension, tp,
is defined as the average of the tensile forcesREGEO ‘2007 - 17 -
inside the fibers over the control area A.
Consequently, tp can be estimated as:
t p = ci,c c ci, tan n,ave (9)
where is the aspect ratio defined as:
=
lfdf
(10)
where df is the equivalent diameter of the fiber.
When failure is governed by the yielding of the
fibers, the distributed tension, tt , is determined
from the tensile strength of the fiber:
tt = f ,ult (11)
where f,ult is the ultimate tensile strength of
the individual fibers.
The fiber-induced distributed tension t to be
used in the discrete approach to account for the
tensile contribution of the fibers in limit
equilibrium analysis is:
t = mint p ,tt (12)
The critical normal stress, n,crit , which defines
the change in the governing failure mode, is
the normal stress at which failure occurs
simultaneously by pullout and tensile breakage
of the fibers. That is, the following condition
holds at the critical normal stress:
tt t p (13)
An analytical expression for the critical normal
stress can be obtained as follows:
, tan
, ,
,
i
f ult i c
n crit
c
c c (14)
As in analyses involving planar inclusions, the
orientation of the fiber-induced distributed
tension should also be identified or assumed.
Specifically, the fiber-induced distributed
tension can be assumed to act: a) along the
failure surface so that the discrete fiberinduced tensile contribution can be directly
“added” to the shear strength contribution of
the soil in a limit equilibrium analysis; b)
horizontally, which would be consistent with
design assumptions for reinforced soil
structures using planar reinforcements; and c)
in a direction somewhere between the initial
fiber orientation (which is random) and the
orientation of the failure plane.
This equivalent shear strength of fiberreinforced specimens can be defined as a
function of the fiber-induced distributed
tension t, and the shear strength of the
unreinforced soil, S:
S = S t c t
eq n tan (15)
where is an empirical coefficient that
accounts for the orientation of fiber and the
efficiency of the mixing of fibers. is equal to
1, if the fibers are randomly distributed and
working with 100% efficiency, otherwise
should be smaller than 1.
Depending on whether the mode of failure is
fiber pullout or yielding, the equivalent shear
strength can be derived by combining (9) or
(11) with (15). It should be noted that the
average normal stress acting on the fibers,
n,ave, does not necessarily equal the normal
stress on the shear plane n . For randomly
distributed fibers, n,ave could be represented by
the octahedral stress component. However, a
sensitivity evaluation undertaken using typical
ranges of shear strength parameters show that
n,ave can be approximated by n without
introducing significant error.
Accordingly, the following expressions can be
used to define the equivalent shear strength
when failure is governed by fiber pullout:
S eq, p = ceq, p tan eq, p n (16)
ceq, p = 1 ci,c c (17)
tan eq, p = 1 ci, tan (18)
Equivalently, the following expressions can be
obtained to define the equivalent shear strength
when failure is governed by tensile breakage of
the fibers:
S eq,t = ceq,t tan eq,t n (19)
ceq,t = c f ,ult (20)
tan eq,t = tan (21)
The above expressions yield a bilinear shear
strength envelope, which is shown in Figure
14.REGEO ‘2007 - 18 -
Figure 14 Representation of the equivalent shear
strength according to the discrete approach
4.2 Experimental validation
A triaxial compression testing program on
fiber-reinforced soil was implemented to
validate the proposed discrete framework. Both
cohesive and granular soils were used in the
testing program, and the soil properties were
summarized in Table 2.
Table 2 Summary of soil properties
Soil type Soil 1 Soil 2
USCS
classification
SP CL
LL % - 49
PL % - 24
IP % - 25
% Fines 1.4 82.6
The tests were conducted using commercially
available polypropylene fibers, and the
properties of fibers were summarized in Table
3. A series of tensile test were performed in
general accordance with ASTM D2256-97 to
evaluate the ultimate tensile strength of fibers.
The average tensile strength of the fibers was
approximately 425,000 kPa.
The triaxial testing program involved
consolidated drained (CD) tests for SP soils
and consolidated undrained (CU) tests for CL
soils. The specimens have a diameter of 71 mm
and a minimum length-to-diameter ratio of 2.
The CU tests were performed in general
accordance with ASTM D4767, and the
specimens were back pressure saturated and
the pore water pressure was measured. The
unreinforced tests of SP soil yielded an
effective shear strength envelope defined by
cohesion of 6.1 kPa and friction angle of 34.3°,
while the cohesion and friction angle of CL
soil were 12.0 kPa and 31.0° respectively.
Table 3 Summary of fiber properties
SP tests CL tests
Linear density (denier) 1000 & 360 2610
Fiber content (%) 0.2 & 0.4 0.2 & 0.4
Length of fibers (mm) 25 & 51 25 & 51
Type of fiber fibrillated &
tape
fibrillated
The governing failure mode for the polymeric
fibers used in this investigation is pullout
because of the comparatively high tensile
strength and short length of the fibers.
Accordingly, the triaxial testing program
conducted in this study focuses only on the
first portion of the bilinear strength envelope
shown in Figure 14.
Figure 15 shows the stress-strain behavior of
SP soil specimens reinforced with 360 denier
fibers, and placed at gravimetric fiber contents
of 0, 0.2 and 0.4 %. Specimens were tested
under confining pressure of 70 kPa. The peak
deviator stress increases approximately linearly
with increasing fiber content, which is
consistent with the discrete framework (see
equation (9)). The post-peak shear strength loss
is smaller in the reinforced specimens than in
the unreinforced specimens. However, the
initial portions of the stress-strain curves of the
reinforced and unreinforced specimens are
approximately similar. Accordingly, the soil
appears to take most of the applied load at
small strain levels, while the load resisted by
the fibers is more substantial at higher strain
level. The larger strain corresponding to the
peak deviator stress displayed by the fiberreinforced specimens suggests that fibers
increase the ductility of the reinforced soil
specimen. These findings are confirmed in
Figure 16, which shows the test results
obtained under higher confining stress (140
kPa).
Se =S+t
1
tan
n
c
S
n,cri
S tREGEO ‘2007 - 19 -
Figure 15. Stress-strain behavior of specimens prepared
using w =0, 0.2 and 0.4% with lf =25 mm fibers (360
denier), 70 kPa, Soil 1
Figure 16 Stress-strain behavior of specimens prepared
using w =0, 0.2 and 0.4% with lf =25 mm fibers (360
denier), 140 kPa, Soil 1
The effect of fiber length on the stress-strain
behavior is shown in Figure 17. The specimens
were prepared using fibers with a different
fiber type (1000 denier) than that used in the
tests shown in Figures 15 and 16. The
specimens were prepared using the same
gravimetric fiber content, but with varying
fiber length. The specimens reinforced with
longer (50 mm) fibers displayed higher shear
strength. The peak deviator stress increases
linearly with increasing aspect ratio, which is
also consistent with the trend indicated by
equation (9). The strain corresponding to the
peak strength increases with increasing fiber
length. When the governing failure mode is
pullout, the fiber-induced distributed tension
reaches its peak when the pullout resistance is
fully mobilized. For longer fibers, it usually
requires a larger interface shear deformation to
fully mobilize the interface strength.
Consequently, the macroscopic axial strain at
peak stress should be larger for specimen
reinforced with longer fibers. Figure 18 shows
a similar trend for the case of tests conducted
under higher confining pressures.
Figure 17 Stress-strain behavior of specimen prepared
using w=0.2 %, with lf=25 mm and 50 mm fibers (1000
denier), =70 kPa, Soil 1
Figure 18 Stress-strain behavior of specimen prepared
using w=0.2 %, with lf=25 mm and 50 mm fibers (1000
denier), =140 kPa, Soil 1
Figure 19 compares the stress-strain behavior
of both unreinforced and fiber-reinforced
specimen using soil 2. The reinforced
specimen were prepared at w=0.2%, using 2-
inch long 2610 denier fibers. Both specimens
were compacted at optimum moisture content
to 90% of the maximum dry density achieved
in the standard Proctor test as specified in
ASTM D 698, and tested under confining
pressure =98 kPa. Due to the undrained test
condition, the effective confining stress
changes with the excess pore water pressure
induced in the process of shearing. The peak
shear strength was selected in terms of the
maximum value of (’/’). The increment of
deviator stress due to fiber addition is not as
obvious as in the case of SP sand. However,
the pore water pressure generated during
shearing is larger for reinforced specimen than
for unreinforced specimen (see Figure 20).
Consequently the effective confining stress
0
50
100
150
200
250
300
350
400
450
500
0 5 10 15 20 25
Axial strain (%)
Deviator stress (kPa)
w=0%
w=0.2%
w=0.4%
0
100
200
300
400
500
600
700
800
900
1000
0 5 10 15 20 25
Axial strain (%)
Deviator stress (kPa)
w=0%
w=0.2%
w=0.4%
0
50
100
150
200
250
300
350
0 5 10 15 20 25
Axial strain (%)
Deviator stress (kPa)
unreinforced
l f=25 mm
l f=50 mm
0
100
200
300
400
500
600
0 5 10 15 20 25
Axial strain (%)
Deviator stress (kPa)
unreinforced
l f=25 mm
l f=50 mmREGEO ‘2007 - 20 -
inside the reinforced specimen is smaller than
that inside the unreinforced specimen. The
fiber-reinforced specimen achieved equal or
higher peak deviator stress than the
unreinforced specimen under a lower effective
confining stress. This shows that the addition
of fibers increases the shear strength of the
reinforced specimen. Since positive water
pressure is associated with the tendency of
volume shrinkage, this observation shows that
fiber reinforcement restrains the dilatancy of
the reinforced soil. Other researchers
(Michalowski and Cermak, 2003, Consoli et
al., 1998) reported that fiber-reinforced
specimens displayed smaller volume dilatation
than unreinforced specimen in consolidated
drained (CD) test. This observation confirms
their findings in a different test condition.
Figure 19 Stress-strain behavior of specimens prepared
using w=0, 0.2 %, with lf=50 mm fibers (2610 denier),
=98 kPa, Soil 2
Figure 20 Excess pore water pressure of specimens
prepared using w=0, 0.2 %, with lf=50 mm fibers (2610
denier), =98kPa, Soil 2
Similar observation can be made from Figures
21 and 22, which shows the stress-strain
behavior and the pore water pressure evolution
obtained using 25-mm fibers placed at 0.2%
and 0.4% gravimetric fiber contents. As the
fiber content increases, the pore water pressure
generated during undrained shearing also
increases.
Figure 21 Stress-strain behavior of specimens prepared
using w=0.2, 0.4%, with lf=25 mm fibers (2610 denier),
=116 kPa, Soil 2
Figure 22 Excess pore water pressure of specimens
prepared using w =0.2, 0.4 %, with lf=25 mm fibers
(2610 denier), =116kPa, Soil 2
Equations (16) through (18) were used to
predict the equivalent shear strength for fiberreinforced specimens. Interaction coefficients
(ci,c and ci,) of 0.8 are assumed in the analyses
conducted in this study. The interface shear
strength obtained from pullout test results
conducted on woven geotextiles was
considered representative of the interface shear
strength on individual fibers. For practical
purposes, interaction coefficients can be
selected from values reported in the literature
for continuous planar reinforcements. This is
because pullout tests conducted using a variety
of soils and planar geosynthetics have been
reported to render interaction coefficient values
falling within a narrow range (Koutsourais et
0
20
40
60
80
100
0 5 10 15 20
Axial strain (%)
Deviator stress (kPa)
w=0.2%
w=0%
-20
0
20
40
60
80
100
120
0 5 10 15 20
Axial strain (%)
Pore water pressure (kPa)
w=0.2%
w=0%
0
20
40
60
80
100
120
140
0 5 10 15 20
Axial strain (%)
Deviator stress (kPa)
w=0.2%
w=0.4%
-20
0
20
40
60
80
100
120
0 5 10 15 20
Axial strain (%)
Pore water pressure (kPa)
w=0.2%
w=0.4%REGEO ‘2007 - 21 -
al., 1998, Michalowski and Cermak, 2003).
is assumed to be 1.0 for randomly distributed
fibers. Table 4 summarized the values of
parameters used in the analyses.
Table 4 Summary of parameters used in the prediction
The effect of fiber content on shear strength is
shown in Figure 23, which compares the
experimental data and predicted shear strength
envelopes obtained from Soil 1 using 25 mm
fibers with linear density of 360 denier placed
at fiber contents of 0.0%, 0.2%, and 0.4%. The
experimental results show a clear increase in
equivalent shear strength with increasing fiber
content. No major influence of fibrillation is
perceived in the results of the testing program.
The shear strength envelope for the
unreinforced specimens was defined by fitting
the experimental data. However, the shear
strength envelopes shown in the figure for the
reinforced specimens were predicted
analytically using the proposed discrete
framework. A very good agreement is
observed between experimental data points and
predicted shear strength envelopes. As
predicted by the discrete framework, the
distributed fiber-induced tension increases
linearly with the volumetric fiber content.
Similar observation can be made in Figure 24,
which shows the results obtained from Soil 2
using 50- mm-long fibers with linear density of
2610 denier.
The effect of fiber aspect ratio on shear
strength is shown in Figure 25, which
compares the experimental and predicted shear
strength envelopes of specimens of Soil 1
placed at w=0.2%, with 25 and 50 mm-long
fibers. As predicted by the discrete framework,
increasing the fiber length increases the pullout
resistance of individual fibers, and results in a
higher fiber-induced distributed tension.
Consequently, for the same fiber content,
specimens reinforced with longer fibers will
have higher equivalent shear strength. This
trend agrees well with the experimental data.
Similar observation can be made from Figure
26, which shows the results obtained from Soil
2 using 25 mm and 50 mm-long fibers and
placed at w =0.4%.
Figure 23 Comparison between predicted and
experimental shear strength results for specimens
reinforced at w =0, 0.2%, 0.4% with 25 mm-long fibers
(360 denier), Soil 1
Figure 24 Comparison between predicted and
experimental shear strength results for specimens
reinforced at w=0, 0.2%, 0.4% with 50 mm-long fibers
(2610 denier), Soil 2
Additional insight into the validity of the
proposed discrete approach can be obtained by
comparing the results obtained for specimens
reinforced with 50 mm-long fibers placed at a
fiber content of 0.2% with those obtained for
specimens reinforced with 25 mm-long fibers
placed at a fiber content of 0.4%. That is
specimens with a constant value of (w· As
inferred from inspection of equation (9) the
fiber-induced distributed tension is directly
proportional to both the fiber content and the
fiber aspect ratio. Consequently, the predicted
equivalent shear strength parameters for the
above combinations of fiber length and fiber
° c
(kPa)
ci,c ci,
Soil 1 1.0 34.3 6.1 0.8 0.8
Soil 2 1.0 31.0 12.0 0.8 0.8
0
100
200
300
400
0 100 200 300 400
' (kPa)
(kPa)
Exp. data, 0% fibers
Stren. envelope, 0% fibers (best fit)
Exp. data, 0.2% fibers (fibr.)
Exp. data, 0.2% fibers (tape)
Stren. envelope, 0.2% fibers (predicted)
Exp. data, 0.4% fibers (fibr.)
Exp. data, 0.4% fibers (tape)
Stren. envelope, 0.4% fibers (predicted)
0
20
40
60
80
100
0 20 40 60 80 100
' (kPa)
(kPa)
Exp. data, 0% fibers
Stren. envelope, 0% fibers(best fit)
Exp. data, 0.2% fibers
Stren. envelope, 0.2% fibers(predicted)
Exp. data, 0.4% fibers
Stren. envelope, 0.4% fibers(predicted)REGEO ‘2007 - 22 -
content are the same. Figures 27 and 28
combine these experimental results.
Figure 25 Comparison between predicted and
experimental shear strength results for specimens
reinforced at w =0.2%, with 25 mm-long and 50 mm-long
fibers (1000 denier), Soil 1
Figure 26 Comparison between predicted and
experimental shear strength results for specimens
reinforced at w =0.4%, with 25 mm-long and 50 mm-long
fibers (2610 denier), Soil 2
The good agreement between experimental
results and predicted values provides additional
evidence of the suitability of the proposed
discrete approach. From the practical
standpoint, it should be noted that using 50
mm-long fibers placed at a fiber content of
0.2% corresponds to half the reinforcement
material than using 25 mm-long fibers placed
at a fiber content of 0.4%. That is, for the same
target equivalent shear strength the first
combination leads to half the material costs
than the second one. It is anticipated, though,
that difficulty in achieving good fiber mixing
may compromise the validity of the
relationships developed herein for
comparatively high aspect ratios (i.e.
comparatively long fibers) and for
comparatively high fiber contents. The fiber
content or fiber length at which the validity of
these relationships is compromised should be
further evaluated. Nonetheless, good mixing
was achieved for the fiber contents and fiber
lengths considered in this investigation, which
were selected based on values typically used in
geotechnical projects.
Figure 27 Consolidated shear strength results for
specimen reinforced with 50 mm-long fibers (1000
denier) placed at w =0.2% and 25 mm fibers placed at
w =0.4%, Soil 1
Figure 28 Consolidated shear strength results for
specimen reinforced with 50 mm-long fibers (2610
denier) placed at w=0.2% and 25 mm fibers placed at w
=0.4%, Soil 2
Figure 29 shows the stress-strain behavior of
specimen reinforced with 50 mm fibers placed
at w =0.2% and 25 mm fibers placed at w
=0.4%. While the discrete approach was
developed only to predict the shear strength
response, the results in the figure show that
fiber-reinforced specimens prepared using a
constant value display similar stress-strain
0
100
200
300
400
0 100 200 300 400
' (kPa)
(kPa)
Exp. data 0% fibers
Stren. envelope, 0% fibers (best fit)
Exp. data, 25mm (tape)
Exp. data, 25mm (fibr)
Stren. envelope, 25mm (predicted)
Exp. data 50mm (tape)
Exp. data 50mm (fibr)
Stren. envelope, 50mm (predicted)
0
20
40
60
80
100
0 20 40 60 80 100
' (kPa)
(kPa)
Exp. data, 0% fibers
Stren. envelope, 0% fibers (best fit)
Exp. data, 25mm fibers
Stren. envelope, 25mm fibers(predicted)
Exp. data, 50mm fibers
Stren. envelope,25mm fibers(predicted)
0
100
200
300
400
0 100 200 300 400
' (kPa)
(kPa)
Experimental data, 0% fibers
Stren. envelope, 0% fibers (best fit)
Exp. data, 0.2% fibers (fibr.), 50 mm
Exp. data, 0.2% fibers (tape), 50 mm
Exp. data, 0.4% fibers (fibr.), 25 mm
Exp. data, 0.4% fibers (tape), 25 mm
Stren. envelope, (predicted)
0
20
40
60
80
100
0 20 40 60 80 100
'(kPa)
(kPai)
Exp. data, 0% fibers
Stren. envelope, 0% fibers (best fit)
Exp. data, 0.2% fibers, 50 mm
Exp. data, 0.4% fibers, 25mm
Stren. envelope (predicted)REGEO ‘2007 - 23 -
behavior. This similar response is observed for
both fibrillated and tape fibers, suggesting that
the fibrillation procedure does not have a
significant impact on the mechanical response
of fiber-reinforced soil. The experimental
results suggest that the proportionality of shear
strength with the fiber content and fiber aspect
ratio predicted by the discrete framework can
be extrapolated to the entire stress-strain
response of fiber-reinforced specimens.
Figure 29 Comparison between stress-strain behavior for
specimen reinforced with 50mm fibers (1000 denier)
placed at w=0.2% and 25 mm fibers placed at w =0.4%,
=70 kPa
4.3 Remarks on Fiber Reinforced Soil
The discrete approach for fiber-reinforced soil
was validated in this investigation using
experimental data from a triaxial testing of
both sand and clay. The effect of fiber
reinforcement on stress-strain behavior and
shear strength was investigated and compared
with the analytical results of the discrete
approach. The main conclusions drawn from
this investigation are:
The addition of fibers can significantly
increase the peak shear strength and limit
the post peak strength loss of both cohesive
and granular soil. An increase in fiber
content leads to increasing strain at failure
and, consequently, to a more ductile
behavior.
The fiber reinforcement tends to restrain
the volume dilation of the soil in drained
condition, or equivalently, increase the
positive water pressure in undrained
condition.
The peak shear strength increases with
increasing aspect ratio. The strain at peak
deviator stress increases with increasing
fiber aspect ratio.
As predicted by the discrete framework, the
experimental results confirmed that the
fiber-induced distributed tension increases
linearly with fiber content and fiber aspect
ratio when failure is characterized by
pullout of individual fibers.
Experimental results conducted using
specimens with a constant (w·) value
show not only the same shear strength but
also display a similar stress-strain behavior.
If good mixing can be achieved, fibers with
comparatively high aspect ratio can lead to
lower fiber contents while reaching the
same target equivalent shear strength,
resulting in savings of reinforcement
material.
Overall, for both sand and clay specimens,
the discrete approach was shown to predict
accurately the shear strength obtained
experimentally using specimens reinforced
with polymeric fibers tested under
confining stresses typical of slope
stabilization projects.
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