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Publication Number:  FHWA-HRT-14-094    Date:  February 2015
Publication Number: FHWA-HRT-14-094
Date: February 2015

 

Synthesis of Geosynthetic Reinforced Soil (GRS) Design Topics

CHAPTER 6. W EQUATION

The W equation is used to estimate the vertical capacity of footings on a GRS wall and was first published by Pham in his Ph.D. thesis entitled Investigating Composite Behavior of Geosynthetic Reinforced Soil (GRS) Mass.(85) In this equation, the W term accounts for the fact that an increase in the reinforcement strength does not have the same effect as a proportional decrease in the reinforcement spacing, as has been traditionally assumed in simplified GMSE design. This is a significant difference between GMSE and GRS design. Results of mini-pier experiments performed by Adams, Adams et al., and Elton and Patawaran, and plane strain tests on GRS performed by Pham, showed that the contributions of the reinforcement spacing to the strength of the GRS is much greater than that of the reinforcement strength. (See references 86, 6, 87 through 91, and 85.) The various terms in the W equation and previous research and theory leading to its development are discussed. The reliability of this equation is demonstrated based on load test results from the literature.

W EQUATION

In reality, the capacity of a GRS is related to the effects of confinement (due to CISs and the lateral restraint offered by the reinforcement internally, and confining stress at the facing), reinforcement spacing, strength and stiffness, shape and location of the failure surface, stress-strain behavior of the soil, and degree of mobilization of shear resistance along an assumed failure plane. The W equation was derived using limit equilibrium analysis. This type of analysis assumes a linear failure surface, assumes a rigid-plastic soil behavior, neglects soil-reinforcement stiffness, and assumes full mobilization of shear strength along the failure surface. Despite the many assumptions that may not reflect reality, limit equilibrium analysis is popular among practitioners because it provides a solution that is simple and easy to use.

The W equation can be derived by first considering the Mohr-Coulomb failure envelope and the Mohr circle at failure for an unreinforced cohesionless soil (figure 45).

This figure shows two  Mohr circles plotted in shear stress-normal stress space. The smaller Mohr circle  is for an unreinforced soil while the larger circle is for the same soil but  reinforced. The reinforced soil Mohr circle is shifted to the right of the  unreinforced circle, suggesting that the reinforcement adds lateral confinement  to the soil. The reinforced soil Mohr circle is larger than the unreinforced circle,  suggesting that the reinforcement increases the strength of the unreinforced  soil. This plot assumes that the friction angles for the reinforced and  unreinforced soils are identical.
Figure 45. Drawing. Mohr circles for unreinforced and reinforced soil.

If the soil friction angle is φ, the equation in figure 46 shows that at failure:

The equation  calculates sigma subscript one as equal to sigma subscript three times the  quotient of one plus sin phi divided by one minus sin phi. The equation is also  expressed as sigma subscript one equals sigma subscript three times Kappa  subscript p.
Figure 46. Equation. Major principal stress σ subscript 1.

σ1 and σ3 are the major and minor principal stresses respectively, and Kp equals the Rankine passive earth pressure coefficient. If the soil were reinforced, Yang indicated that the friction angle of the reinforced soil is approximately the same as the unreinforced soil if no slippage occurs between the soil and reinforcement.(64) A GRS is stronger than the unreinforced soil, and hence the major principal stress at failure is higher than σ1, say σ1R in figure 45.

For this to occur, the confining stress in the soil must effectively increase due to the presence of the reinforcement as shown in the equation in figure 47:

The equation  calculates sigma subscript 3R as equal to sigma subscript three plus Delta  sigma subscript three.
Figure 47. Equation. Confining stress due presence of reinforcement, σ subscript 3R.

The reinforcement restrains lateral movement of the soil. Thus, Δσ3 represents the additional confining stress that is imposed due to the reinforcement. Therefore, the capacity of the GRS can be expressed as the equation in figure 48:

The equation calculates sigma subscript one R as equal to sigma subscript three R times Kappa subscript p. The equation  is also expressed as sigma subscript one R equals Kappa subscript p times the sum of sigma subscript three plus Delta  sigma subscript three.
Figure 48. Equation. Capacity of the GRS,σ subscript 1R.

Δσ3 is analogous to a prestress in the reinforced soil equal to the frictional force developed between the soil and the reinforcement with a maximum value determined by the tensile strength of the reinforcing material. At failure, this prestress will be at its maximum and is related to the reinforcement tensile strength per unit wall length (Tf). If it is assumed that one-dimensional expansion in the horizontal direction occurs over a tributary area of reinforcement equal to spacing Sv per unit wall length, then Δσ3 can be expressed as shown in figure 49:(92)

The equation calculates Delta  sigma subscript three as equal to T subscript F divided by S subscript v.
Figure 49. Equation. Additional confining stress as a function of reinforcement tensile strength divided by the reinforcement spacing Δ σ subscript 3.

Implied in the equation in figure 49 is that a GRS with reinforcement strength Tf at spacing Sv will have the same capacity as a GRS with reinforcement strength 2Tf at spacing 2Sv, which has been shown to be untrue by Adams, Adams et al., Elton and Patawaran, Ziegler et al., and Pham. (See References 86, 6, 87 through 91, 93, and 85.) Instead, Sv has a bigger influence on the capacity than Tf. This led Pham to propose a modified version of the equation in figure 49 as shown in figure 50:


The equation calculates Delta  sigma subscript three as equal to W multiplied by the quotient of T subscript F divided by S subscript v.
Figure 50. Equation. Modified version of equation in figure 49 for additional confining stress, Δ σ subscript 3 imposed with the W factor.

W is the factor that amplifies the contribution of Sv to the GRS capacity. The W factor was semi-empirically derived and is calculated using the equation in figure 51:

The equation calculates W as equal to 0.7 with an exponent term  that is the quotient of S subscript v divided by six D subscript max. (W is  the factor that amplifies the contribution of S subscript v to the geosynthetic  reinforced soil capacity.)
Figure 51. Equation. W factor.

Dmax is the maximum particle size of the GRS backfill used as a normalizing parameter to make the exponent dimensionless. Note that the 0.7 factor in figure 51 was theoretically derived while the exponent was empirically derived. Using the concept of "average stresses" proposed by Ketchart and Wu to estimate the average and maximum forces in a reinforcement, Pham showed, based on a load-transfer analysis, that the average reinforcement force is about 70 percent of the maximum reinforcement tensile strength; hence the 0.7 factor in figure 51.(62,85) For details on this derivation, refer to Pham.(85)

The exponent of figure 51 is a function of Sv and Dmax. Because the base term is less than unity, W, and hence the capacity, increases with decreasing Sv and increasing Dmax. This is logical because one would expect a GRS with closer reinforcement spacing and larger maximum aggregate size to have a higher capacity.

Therefore, combining the equations in figure 48, figure 50, and figure 51, the capacity of the GRS can be expressed as the equation in figure 52:

The equation  calculates sigma subscript one R as equal  to the product of Kappa subscript p and the sum of sigma subscript three plus the product of two terms. The first  term is 0.7 with an exponent that is the quotient of S subscript v divided by  six D subscript max. The second term  is the quotient of T subscript F divided by S subscript v.
Figure 52. Equation. Capacity of the GRS, σ subscript 1R.

If the soil has cohesion, c, then the equation in figure 52 can be expanded to the equation in figure 53:

The equation calculates sigma subscript  one R as equal to the sum of 2c times the square root of Kappa  subscript pplus the equation from  Figure 52, which is the product of Kappa subscript p and the sum of sigma subscript three plus the product of two  terms. The first term is 0.7 with an exponent that is the quotient of S subscript v divided by six D subscript max. The second term is the quotient of T subscript F divided by S subscript v.
Figure 53. Equation. Expansion of the equation in figure 52 for the capacity of the GRS, σ subscript 1R, to include cohesion.

According to Pham, for a GRS wall with a dry stacked modular block facing, s3 equals the lateral stress exerted by the facing on the GRS mass, which is γbl times D times tan .(85) γbl equals the bulk unit weight of the facing block, which is the weight of block/volume of the block assuming it is not hollow. (For a 7.625- by 7.625- by 15.625-inch (19.368- by 19.368- by 39.688-cm) CMU block weighing 42 lbs (19.1 kg), bl equals 80 pcf). D equals the depth of the facing block perpendicular to the wall face. δ equals the friction angle between geosynthetic reinforcement and the top or bottom surface of the facing block. The equation in figure 53 can also be rearranged and solved for the required reinforcement strength (Tf,req) given the loads on the particular GRS composite for design.

RELIABILITY OF THE W EQUATION

A database consisting of 19 load tests on GRS from the literature (table 7) was used to examine the reliability of the W equation or the equation in figure 52. In addition to the references already cited in this synopsis, the table contains tests from Adams et al.(6) A plot of predicted versus measured capacities is shown in figure 54. It can be seen that overall, the coefficient of determination was 0.853 with a slope of 0.913 for this dataset when the regression line was forced through the origin. To illustrate the importance of the W term, a plot of predicted versus measured capacities is shown in figure 55 with the W term eliminated from the equation in figure 53. It is apparent that the capacities are severely overpredicted with a less than desirable fit. This validates the necessity of the W term in the equation in figure 53.

Table 7 . Prediction data for large-scale tests.

No.

Test

Test Results

Facing

Reinforcement

Aggregate

Geometry

Reference

qult,emp
(kPa)

qult calc
(kPa)

σc
(kPa)

Block
Type

Sv
(m)

Tf
(kN/m)

Dmax
(m)

c
(kPa)

φtest
(degrees)

φ
 Method

Kp

1

GSGC 2

3,400

2,182

34

N/A

0.2

70

0.0330

70

50

TX

7.55

PS

85
(Pham (2009))

2

GSGC 3

2,040

1,615

34

N/A

0.4

140

0.0330

70

50

TX

7.55

PS

3

GSGC 4

1,785

936

34

N/A

0.4

70

0.0330

70

50

TX

7.55

PS

4

GSGC 5

2,034

1,925

0

None

0.2

70

0.0330

70

50

TX

7.55

PS

5

Elton 1

230

133

0

None

0.15

9

0.0127

28

40

DS

4.60

Cylindrical

91
(Elton and Patawaran (2005))

6

Elton 2

129

33

0

None

0.3

9

0.0127

28

40

DS

4.60

Cylindrical

7

Elton 3

306

207

0

None

0.2

14

0.0127

28

40

DS

4.60

Cylindrical

8

Elton 4

292

222

0

None

0.2

15

0.0127

28

40

DS

4.60

Cylindrical

9

Elton 5

402

281

0

None

0.2

19

0.0127

28

40

DS

4.60

Cylindrical

10

Elton 6

397

296

0

None

0.2

20

0.0127

28

40

DS

4.60

Cylindrical

11

Elton 7

459

370

0

None

0.2

25

0.0127

28

40

DS

4.60

Cylindrical

12

NCHRP 1

420

275

0.97

CMU

0.2

21

0.0254

0

36.5

LSDS

3.94

PS

94
(Wu et al. (2006))

13

NCHRP 2

850

908

0.97

CMU

0.2

70

0.0254

0

36.5

LSDS

3.94

PS

14

Defiance 1

542

580

0.97

CMU

0.2

35

0.0127

0

50.7

LSDS

7.84

Column

89
(Adams et al. (2007))

15

Defiance 2

1,213

1,153

0.97

CMU

0.2

70

0.0127

0

50.7

LSDS

7.84

Column

16

Vegas

1,008

1,231

2.35

SRW

0.2

35

0.0254

70

50

TX

7.55

Column

88
(Adams et al. (2002))

17

MP A

225

284

0

None

0.6

70

0.0254

0

53.5

LSDS

9.20

Column

89
(Adams et al. (2007))

18

MP B

170

671

0

None

0.4

70

0.0254

0

53.5

LSDS

9.20

Column

19

MP C

460

634

0

None

0.2

21

0.0254

0

53.5

LSDS

9.20

Column

GSGC =Generic Geosynthetic Soil Composite 
NCHRP = National Cooperative Highway Research Program
MP = Mini-Pier
TX = Triaxial
DS = Direct Shear
LSDS = Large-Scale Direct Shear
PS = Plane Strain
1 kPA = 20.89 psf
1 m = 3.28 ft
1 kN/m = 68.6 lb/ft

This chart plots the predicted versus measured capacities from full-scale geosynthetic  reinforced solid (GRS) load tests. The x-axis is Measured Capacity in  kilopascals and ranges from 0 to 3,500. The y-axis is Predicted Capacity in  kilopascals and ranges from 0 to 3,500. The predicted capacity is obtained  using the equation in figure 52. That equation was semi-empirically derived and  contains a W-term that amplifies the  contribution of the reinforcement spacing and downplays the contribution of the  reinforcement strength to the GRS capacity. For the data used, the slope of the  predicted versus measured capacities is 0.91 with a coefficient of  determination of 0.85. (1 kPA = 20.89 psf.)
1 kPA = 20.89 psf
Figure 54. Chart. Predicted versus measured capacity of large-scale GRS tests using the equation in figure 52.


This chart plots the predicted versus measured  capacities from full-scale geosynthetic reinforced soil (GRS) load tests. The x-axis  is Measured Capacity in kilopascals and ranges from 0 to 3,500. The y-axis is  Predicted Capacity in kilopascals and ranges from 0 to 3,500. The predicted capacity  is obtained using the equation in figure 52 without the W term. The equation in  figure 52 was semi-empirically derived and contains a W-term that amplifies the  contribution of the reinforcement spacing and downplays the contribution of the  reinforcement strength to the GRS capacity. For the data used, the slope of the  predicted versus measured capacities is 1.38 with a coefficient of  determination of 0.61. 1 kPA = 20.89 psf.)
1 kPA = 20.89 psf
Figure 55. Chart. Predicted versus measured capacity of large-scale GRS tests using the equation in figure 52 without the W term.

 

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