SLOPE RELIABILITY
MBTC FR 1014
Sam I. Thornton
DISCLAIMER
The
contents of this report reflect the views of the authors, who are responsible
for the facts and accuracy of the information presented herein. This document is disseminated under the
sponsorship of the Department of Transportation, University Transportation
Centers Program, in the interest of information exchange. The
FINAL REPORT
Slope Reliability
Submitted
to
Mack-Blackwell
National Rural
and
Prepared
by
Sam I. Thornton
Civil Engineering Department
June 1995
SLOPE
RELIABILITY
SUMMARY
Analysis
methods for slope stability are routinely applied by geotechnical engineers.
Slope designs, however, are usually based on a "safety factor" which
does not account for soil variability (soil variability is due to actual
in-place conditions and not due to sampling procedures and/or testing
methods). As a result, the true safety
of a slope is unknown.
A
reliability approach, using probability calculations which account for the
variability in soil strength, is superior to the factor of safety
approach. The method is based on the
point estimate method and allows engineers to calculate a probability of
failure for the slope. Knowing the probability
of failure improves engineering judgement by providing a rational basis for
making a safe and economical slope design.
Examples
show how soil variability affects slope reliability and how the method is
applied. The factor of safety is 1.30
in the first two examples. In the first
example, the soil deposits are uniform and the probability of failure is
acceptable; In the second example, the soils have more soil strength variation
and the probability of failure is higher than recommended.
1
INTRODUCTION
Geotechnical
engineers routinely calculate a factor of safety (FS) to evaluate the stability
of earth slopes. The Simplified Bishop
method (Wright, et al, 1973) is a popular basis for computer analysis programs. A minimum FS of 1.3 is commonly considered as
the design basis for most slopes.
Failure is assumed to occur when the FS is less than 1.0.
Because
the FS analysis does not have a way to consider the variability of the soil
strength, the true safety of a slope is unknown. A reliability approach, where a probability
of failure is calculated, is a better
method for slope design because it accounts for variability in soil
strengths. Other factors, like an
inadequate field investigation, missing a critical geologic detail (Christian,
et, al., 1994) or progressive slope failures (Chowdhury, R,. N., Sept. 1994)
are not included in the method described in this report.
The
probability of slope failure method is based on the "Point Estimate
Method" (PEM) which was developed by Rosenblueth (1975 and 1981) and
described by Harr (1987). In the PEM
method, a distribution of the variable must be found or assumed. If a normal distribution is assumed, the
problem is simplified. Details of the
PEM method and a discussion of other distributions are contained in a thesis by
Garrett (1989) and a paper by McGuffy, Iori, Kyfor and Grivas (1981).
2
APPLICATION OF THE POINT ESTIMATE METHOD TO
SLOPE STABILITY
2.1
MEAN AND STANDARD DEVIATION
To
apply the PEM, the mean and standard deviation of the soil strength in each
layer must be found. Soil strength may
be cohesion, C, and/or internal friction, φ. Between layers, strength parameters are
considered independent. Within a soil
layer, however, the cohesion may be correlated to the internal friction.
![]()
(Eqn.
1)
![]()
(Eqn.
2)
where, x = the C or φ values in the layer
n
= the number of C or φ (tests performed) values in
the layer
2.2 CORRELATION COEFFICIENT
For
a soil layer with C and φ, the correlation between C and φ, must be found. Correlations vary with the type of strength
test. For the consolidated undrained
triaxial test, Harr (1987) reports a correlation, r, of about +0.25. A positive correlation means the internal
friction increases when the cohesion increases.
The undrained triaxial test is the best predictor for quick failures
caused by earthquakes or the sudden drawdown of water at a levee or dam. Drained triaxial tests often have negative
correlations and are usually the best predictor of field performance. Wolff reported a drained triaxial correlation
of -0.47 (Harr, 1987). The correlation
coefficient, r, is calculated by the following:
![]()
(Eqn.
3)
where, N = the number of strength tests
2.3 HIGH AND LOW STRENGTH VALUES
Variation
in C and φ is accounted for by adding or
subtracting the standard deviation. For
example, a high cohesion, C+, is obtained by adding the standard deviation of
the cohesion to the mean. A low
cohesion, C-, is the mean less the standard deviation. In turn, φ+ and φ- is the mean internal friction + or - the standard deviation of
internal friction.
![]()
(Eqn.
4a)
![]()
(Eqn.
4b)
![]()
where,
![]()
(Eqn.
5a)
(Eqn.
5b)
![]()
where,
2.4
SLOPE SAFETY FACTORS
Safety
Factors must be found for all combinations of soil strength. The number of combinations is 2n,
where n is the number of variables (soil strengths). A slope with two layers, each layer with a C
and φ, has 24
or 16 combinations of soil strength. The
set of safety factors reflects the variation of soil strength. The symbol FS++++ is used for a slope
containing two soil layers with C+ and φ+ used for strength values in
both layers. FS-+++ is the symbol for
the FS when C- and φ+ are used for the first layer
and C+ and φ+ are used for the second
layer.
2.5 WEIGHING FUNCTIONS
Weighing
functions must be applied to the FS's.
The weighing functions are point estimates, p, of the distribution of
the FS's. The symbol p++++ is used for
the point applied to FS++++ as described in section 2.4. The sum of the p's is equal to 1.
2.51
Independent Layers
For
the case where each soil layer has only a C (a clay) or φ (a sand) the soil strengths are not correlated. If normal
distribution is assumed, the point estimates are:
p
= 1/2n (Eqn.
6)
where, n = the number of variables (layers when each
layer has only a C or φ).
The
points for two soil layers with C or φ are:
p++ = p+- =
p-+ = p-- = 1/4
For
three soil layers with C or φ, the points are:
p+++ = p++- = p+-+ = p-++ = p+-- =
p-+- = p--+ = p--- = 1/8
The
points for four soil layers are:
p++++ = p+++- = p++-+ = p+-++ =
p-+++ = p++-- =
p+--+ = p--++ = p+--- = p-+-- =
p--+- = p---+ = p-++- =
p+-+- = p---- = p-+-+ = 1/16
2.52 Correlated Layers
When
a slope has a single layer with both C and φ (two variables), the points
are:
p++ = p-- =
(1 + r)/4 (Eqn. 7a)
p+- = p-+ =
(1 - r)/4 (Eqn.
7b)
A
slope that has two soil layers, each with C and φ
(four variables), will have the following points:
p++++ = p---- = p++-- = p--++ = (1+r1+r2)/16 (Eqn.8a)
p+++- = p---+ = p++-+ = p--+- = (1+r1-r2)/16 (Eqn.8b)
p+--- = p-+++ = p+-++ = p--+- = (1-r1+r2)/16 (Eqn.8c)
p+-+- = p-+-+ = p+--+ = p-++- = (1-r1-r2)/16 (Eqn.8d)
2.53
Mixed Layers
For
the case where there are two layers of soil, one layer contains either C or φ and the other contains both C and φ,
the points are:
p+++ = p+-- = p--- =
p-++ = (1+r2)/8 (Eqn.9a)
p++- = p+-+ = p--+ =
p-+- = (1-r2)/8 (Eqn.9b)
2.6
STANDARD DEVIATION OF THE FS'S
The
expected value of the factor of safety, E[FS], and the expected value of the
squared FS's, must be found in order to calculate the standard deviation of the
FS, σ[FS].
2.61 Two Variables
For
a slope with two variables (either two layers with C or φ, or one layer with C and φ):
E[FS] = p++(FS++) +
p+-(FS+-)
+ p-+(FS-+) + p--(FS--) (Eqn.10a)
E[FS2] =
p++(FS++)2 + p+-(FS+-)2
+ p-+(FS-+)2 + p--(FS--)2 (Eqn.10b)
σ[FS] = (E[FS2]
- E[FS]2).5 (Eqn.11)
2.62 Three Variables
For
a slope with three variables (either three layers with C or φ, or two layers; one layer with C or φ,
and one layer with C and φ):
E[FS] = p+++(FS+++) +
p++-(FS++-)
+ p+--(FS+--) + p---(FS---)
+ p--+(FS--+) + p-++(FS--+)
+ p-+-(FS-+-) + p+-+(FS+-+) (Eqn.12a)
E[FS2] =
p+++(FS+++)2 + p++-(FS++-)2
+ p+--(FS+--)2 + p---(FS---)2
+ p--+(FS--+)2 + p-++(FS-++)2
+ p-+-(FS-+-)2 + p+-+(FS+-+)2 (Eqn.12b)
σ[FS] = (E[FS2]
- E[FS]2).5 (Eqn.11)
2.63
Four or More Variables
For
four or more variables, the expected FS, E[FS], is found by multiplying the
points, p, by their respective FS's and summing the products (see equations 10a
and 12a).
The
E[FS2] is found by multiplying the points, p, by their respective
squared FS's and summing the products (see equations 10b and 12b).
The
standard deviation is found from equation 11.
2.7 PROBABILITY OF FAILURE
For
normal distribution, the standardized variable Z is:
Z
= (FS - E[FS])/σ[FS] (Eqn. 13)
where, FS = the cutoff value to be evaluated (FS = 1)
E[FS]
and σ[FS] are found from section 2.6.
With
Z, the probability that the FS will be less than 1 can be found from the normal
distribution table in Appendix A.
3 ACCEPTABLE FAILURE PROBABILITIES
In
order to evaluate a design, the calculated probability of failure should be
compared to an acceptable probability. A
table of acceptable failure probabilities was proposed by Santamarina, et. al.
(1992). A partial listing of the table
is contained in Table 1.
TABLE 1. Slope Stability - Probability of Failure
|
CONDITIONS |
Pf |
|
Unacceptable
in most cases |
>0.1 |
|
Temporary
structures with low repair cost |
0.1 |
|
Low
consequences of failure repairs when time permits |
0.02 |
|
Existing
large cut on interstate highway |
0.01 |
|
Acceptable
in most cases except if lives may be lost |
0.001 |
|
Acceptable
for all slopes |
0.0001 |
|
Unnecessarily
low |
0.00001 |
4
EXAMPLES
4.1 CONVERSION FACTORS
SI to English English
to SI
1 m = 3.281 ft 1 ft = 0.3048 m
1 kN/m2 =
20.885 lb/ft2 1
lb/ft2 = 0.04788 kN/m2
1 kN/m3 =
6.361 lb/ft3 1
lb/ft3 = 0.1572 kN/m3
4.2 TWO LAYERS WITH EITHER C OR Φ
Two
examples using the slope in Figure 1 will show how the method is applied. The unit weight of both soil layers is 20
kN/m3

FIGURE 1
4.21 Example 1: Slope with Uniform Soils
The
internal friction, φ, and cohesion, C, from tests
for the soil in Figure 1 are:
SAND CLAY
φE C (kN/m2)
33.5 60
36.5 63
35.5 64
34.5 58
35.1 62.5
34.9
The
mean (Eqn.1) and standard deviation (Eqn.2) are as follows:
SAND CLAY
mean φ = 35E mean C = 61.5 kN/m2
σ (φ) = 1E σ (C) = 2.45
The
high and low strength values (Eqn. 4a, 4b, 5a, and 5b) used to determine
slope stability factors of safety are:
φ+ = 36E C+ = 63.95 kN/m2
φ- = 34E C- = 59.05 kN/m2
The
strength combinations for slope stability analysis are:
++ Sand φ = 36E Clay
C = 63.95 kN/m2
+- Sand φ = 36E Clay
C = 59.05 kN/m2
-+ Sand φ = 34E Clay
C = 63.95 kN/m2
-- Sand φ = 34E Clay
C = 59.05 kN/m2
The
resulting factors of safety from the computer program PCSTABL5 (Bishop
Method) are:
++ FS =
1.350
+- FS =
1.248
-+ FS =
1.348
-- FS = 1.246
The
weighing functions (Eqn. 6) for two soil types with 1 strength parameter
per layer is:
p++ = p+- =
p-+ = p-- = 0.25
The
expected FS (Eqn. 10a) is:
E[FS] = 0.25(1.350) +
0.25(1.248) + 0.25(1.348) +0 .25(1.246)
= 1.298
The
expected FS2 (Eqn. 10b) is:
E[FS2] =
0.25(1.350)2 + 0.25(1.248)2 + 0.25(1.348)2 +
0.25(1.246)2
= 1.6874
The
standard deviation of the FS's (Eqn. 11) is:
σ [FS] = [(1.687) - (1.298)2)].5
= 0.051
The
standardized variable (Eqn. 13) is:
Z = (1-1.298)/0.051 =
-5.84
For
a FS = 1, where failure is assumed to occur, the probability of failure,
Pf , is (Appendix A):
Pf
< 0.0000001
This
probability of failure, according to Table 1, is unnecessarily low.
4.22 Example 2: Slope with Variable Clay
Strength
test results for the soil in Figure 1 are as follows:
Sand Clay
φE C(kN/m2)
36.5 55
34 50
34.5 71
35.5 82
34.5 53
58
The
mean (Eqn. 1) and standard deviation (Eqn. 2) are as follows:
Sand Clay
mean φ = 35E mean
C = 61.5 kN/m2
σ (φ) = 1E σ (C) = 12.4 kN/m2
The
high and low strength values (Eqn. 4a, 4b, 5a, and 5b) used to determine
slope stability factors of safety are:
φ+ = 36E C+ = 73.9 kN/m2
φ- = 34E C- = 49.1 kN/m2
The
strength combinations for slope stability analysis are:
++ Sand φ = 30E Clay C = 73.9 kN/m2
+- Sand φ = 36E Clay
C = 49.1 kN/m2
-+ Sand φ = 34E Clay
C = 73.9 kN/m2
-- Sand φ = 34E Clay
C = 49.1 kN/m2
The
factors of safety from the computer program PCSTABL5 (Bishop Method)
are:
++ FS =
1.556
+- FS =
1.040
-+ FS =
1.554
-- FS =
1.039
The
expected FS (Eqn. 10a) is:
E[FS]
= 1.297
The
standard deviation of the FS's (Eqn. 11) is:
σ [FS] = 0.2578
The
standardized variable (Eqn. 13) and the probability of failure
(Appendix A) are:
Z =
(1-1.297)/0.2578 = -1.1637
Pf =
0.125
This
probability of failure, according to Table 1 is too high, even for temporary
structures with low repair costs.
4.23 Example Comparison
The
probability that the slopes in the two examples would fail is greatly
different; less than 0.00001% for the
first example vs. 12.5% for the second example.
This difference is surprising because the geometry unit weight, and
average strength of the soil layers within the slopes are the same. The reason for the difference in probability
of failure is the variability in cohesion of the clay layer. In the uniform clay layer (section 4.11) the
standard deviation of the cohesion is 2.45 kN/m2 or 4% of the
average cohesion. The variable clay layer
(section 4.12) has a standard deviation
of 12.4 kN/m2 or 20% of the average cohesion.
4.3 EXAMPLE 3: THREE LAYERS WITH EITHER C OR Φ
The
figure below is a slope on Interstate 40 near

FIGURE 2
In
this example, the only strength parameter in each layer is cohesion. From the strength tests, the mean and
standard deviation of each layer obtained from Eqn. 1 and 2 are:
|
LAYER
NO. |
MEAN STRENGTH |
STANDARD DEVIATION |
|
1 |
180 lb/ft2 |
16 lb/ft2 |
|
2 |
410 lb/ft2 |
54 lb/ft2 |
|
3 |
600 lb/ft2 |
138 lb/ft2 |
The
high and low values (Eqn. 4a and 4b) for cohesion in lb/ft2
are:
Layer 1
Layer 2
Layer 3
C1+ = 196 C2+ = 464 C3+ = 738
C1 - = 164 C2
- = 356 C3
- = 462
The
next step is putting together the strength combinations. In this case, since there are 3 strength
parameters, the are 23, or 8 strength combinations.
The
strength combinations and factors of safety from the computer
program PCSTABL5 (Bishop Method) for each combination are as follows:
|
COMBINATION |
C1 |
C2 |
C3 |
FS |
|
+++ |
196 |
464 |
738 |
1.466 |
|
++- |
196 |
464 |
462 |
1.293 |
|
+-+ |
196 |
356 |
738 |
1.145 |
|
-++ |
164 |
464 |
738 |
1.452
|
|
+-- |
196 |
356 |
462 |
1.131 |
|
-+- |
164 |
464 |
462 |
1.285 |
|
--+ |
164 |
356 |
738 |
1.145 |
|
--- |
164 |
356 |
462 |
1.131 |
The
next step is the calculation of the expected FS (Eqn. 12a), expected
value of the squared FS's (Eqn. 12b),
and standard deviation of the FS's (Eqn. 11):
E[FS] = 1.256
E[FS2]
= 1.595
σ[FS] = 0.1326
Then
the standardized variable (Eqn. 13) is found for a FS = 1.
Z =
(1-1.256)/0.1326 = 1.93
By using this Z and the probability
chart in Appendix A, the probability of failure for this slope is 2.68%.
4.4
EXAMPLE 4: FOUR LAYERS WITH C OR Φ
The example for four layers of soil
is taken from the thesis at the

FIGURE 3
In this example, the first and third
layers are clay and the second and fourth layers are sand. From the strength tests, the mean (Eqn.1)
and standard deviation (Eqn. 2) of strengths are:
LAYER MEAN STRENGTH STANDARD DEVIATION
1
3500 lb/ft2 200 lb/ft2
2
27E 5E
3
2000 lb/ft2 300 lb/ft2
4
32E 2.5E
The high and low strength values
(Eqn. 4a, 4b, 5a, and 5b) are:
LAYER HIGH STRENGTH LOW STRENGTH
1 3700
lb/ft2 3300
lb/ft2
2 32E 22E
3 2300
lb/ft2 1700
lb/ft2
4 34.5E 29.5E
The strength combinations and
factors of safety from the computer program PCSTABL5 (Bishop Method) for
each combination are:
|
COMBINATION |
C1 lb/ft2 |
φ2 E |
C3 lb/ft2 |
φ4 E |
FS |
|
++++ |
3700 |
32 |
2300 |
34.5 |
1.4024 |
|
+++- |
3700 |
32 |
2300 |
29.5 |
1.1966 |
|
++-- |
3700 |
32 |
1700 |
29.5 |
1.1428 |
|
+--- |
3700 |
22 |
1700 |
29.5 |
1.1239 |
|
---- |
3300 |
22 |
1700 |
29.5 |
1.1235 |
|
-+-- |
3300 |
32 |
1700 |
29.5 |
1.1424 |
|
-++- |
3300 |
32 |
2300 |
29.5 |
1.1966 |
|
-+++ |
3300 |
32 |
2300 |
34.5 |
1.4021 |
|
--+- |
3300 |
22 |
2300 |
29.5 |
1.1798 |
|
--++ |
3300 |
22 |
2300 |
34.5 |
1.3786 |
|
---+ |
3300 |
22 |
1700 |
34.5 |
1.1798 |
|
-+-+ |
3300 |
32 |
1700 |
34.5 |
1.3352 |
|
+-+- |
3700 |
22 |
2300 |
29.5 |
1.1798 |
|
+--+ |
3700 |
22 |
1700 |
34.5 |
1.3130 |
|
+-++ |
3700 |
22 |
2300 |
34.5 |
1.3790 |
|
++-+ |
3700 |
32 |
1700 |
34.5 |
1.3356 |
The expected FS, expected value
of the squared FS's, and standard deviation of the FS's are found
per article 2.63:
E[FS]
= 1/16 [l.4024 + 1.1966 + 1.1428 + 1.1239 + 1.1235 + 1.1424 + 1.1966 + 1.4021 + 1.1798 + 1.3786 + 1.3126 +
1.3352 +
1.1798 +1.3130 + 1.3790 + 1.3356]
= 1.2590
E[FS2]
= 1/16 [l.40242 + 1.19662 + 1.14282 + 1.12392
+ 1.12352 + 1.14242+
1.19662+ 1.40212 +
1.17982 + 1.37862 + 1.31262 + 1.33522
+ 1.17972 + 1.31302 +
1.37902 + 1.33562]
= 1.5958
σ[FS] = (l.5958 - 1.25902).5
= 0.1035
Then the standardized variable
is found for a FS = 1.
Z
= (1.0 - 1.2590)/0.1305
= 2.50
Using the probability chart in
Appendix A, the probability of failure is 0.62%.
4.5
EXAMPLE 5: ONE SOIL WITH TWO VARIABLES
This example is taken from a paper
by Verduin and Lovell (1988). The
embankment is 40 feet high and is built on a slope of two horizontal to one
vertical (Figure 4). The soil has a unit
weight of 140 lb/ft3.

FIGURE 4
The mean and standard
deviation of the soil strength are:
mean
C = 200 lb/ft2 σ(C) = 80 lb/ft2
mean
φ = 25E σ(φ) = 2.5°
The correlation coefficient
(Eqn. 3) as determined from laboratory tests is +0.25.
The high and low strength values
(Eqn 4a, 4b, 5a, and 5b) used to determine slope stability factors of safety
are:
φ+ = 25 + 2.5 = 27.5E C+ = 200 +
80 = 280 lb/ft2
φ- = 25 - 2.5 = 22.5E C- = 200 - 80
= 120 lb/ft2
The slope factors of safety
from the computer program PCSTABL5 (Bishop Method) are:
FS++
= 1.685
FS+- = 1.454
FS-+ = 1.373
FS-- = 1.140
The weighing functions (Eqn.
7a and 7b) are:
p++
= p-- = 0.25(1+0.25) = 0.3125
p+- = p-+ = 0.25(1-0.25) = 0.1875
The expected FS (Eqn. 10a), expected
value of the squared FS's (Eqn.10b), and standard deviation of the FS's
(Eqn. 11) are:
E[FS]
= 0.3125(1.685) + 0.1875(1.454) +
0.1875(1.373) + 0.3125(1.140)
= 1.413
E[FS2]
= 0.3125(1.685)2 + 0.1875(1.454)2 +
0.1875(1.373)2 + 0.3125(1.140)2
= 2.043
σ[FS] = (2.043 - (1.413)2).5
= 0.216
The standardized variable (Eqn.
13) and probability of failure (Appendix A) are:
Z
= (1.0 - 1.413)/0.216 = -1.91
Pf
= 2.8%
4.6
TWO SOIL LAYERS WITH TWO VARIABLES EACH

FIGURE
5
Unit
Weight Layer 1 = 110 lb/ft3
Unit
Weight Layer 2 = 120 lb/ft3
The mean (Eqn. 1) and
standard deviation (Eqn. 2) of the soil strength are:
First Layer
Second Layer
C
(lb/ft2) φE C
(lb/ft2) φE
200 31 150 27
180 33 110 30
210 28 240 24
230 27 220 25
160 34 120 32
Layer
1 mean C = 196 lb/ft2 σ(C) = 27
lb/ft2
mean
φ = 30.6E σ(φ) = 3.05°
Layer
2 mean C = 168 lb/ft2 σ(C) =
58.9 lb/ft2
mean
φ = 27.6E σ(φ) = 3.36°
The correlation coefficients
(Eqn. 3) are -0.964 for layer 1 and -0.927 for layer 2.
The high and low strength values
(Eqn. 4a, 4b, 5a, and 5b) are:
C1+
= 223 lb/ft2 φ1+ = 33.65E
C1- = 169 lb/ft2 φ1- = 27.55E
C2+
= 226.9 lb/ft2 φ2+ = 30.96E
C2- = 109.1 lb/ft2 φ2- = 24.24E
The slope factors of safety
from the computer program PCSTABL5 (Bishop Method) are:
FS++++
= 1.6235
FS+++- = 1.3798
FS++-- = 1.2123
FS+--- = 1.1714
FS---- = 1.1413
FS---+ = 1.3573
FS--++ = 1.5226
FS-+++ = 1.5897
FS-+-+ = 1.4579
FS+-+- = 1.3295
FS+--+ = 1.3977
FS-++- = 1.3527
FS++-+ = 1.4560
FS--+- = 1.3014
FS+-++ = 1.5595
FS-+-- = 1.1873
The weighing functions (Eqn.
8a, 8b, 8c, and 8d) are:
p++++
= p---- = p++-- = p--++ = (1-0.964-0.927)/16
= -0.05569
p+++-
= p---+ = p++-+ = p--+- = (1-0.964+0.927)/16 = 0.0602
p+---
= p-+++ = p+-++ = p-+-- = (1+0.964-0.927)/16 = 0.0648
p+-+-
= p-+-+ = p+--+ = p-++- = (1+0.964+0.927)/16 = 0.1807
The expected FS, expected value
of the squared FS's, and standard deviation of the FS's are:
E[FS] = -0.05569(1.6235) +
0.0602(1.333798) + -0.05569(1.2123)
+ 0.0648(1.1714) + -0.05569(1.1413) + 0.0602(1.3573)
+ -0.05569(1.5226) + 0.0648(1.5897) +
0.1807(1.4579)
+ 0.1807(1.3527) + 0.1807(1.3977) +
0.0602(1.4560)
+ 0.0602(1.3014) + 0.1807 (1.3295) +
0.0648(1.5595)
+ 0.0648(1.1873)
=
1.3821
E[FS2] = -0.05569(1.62352) +
0.0602(1.37982) + -0.05569(1.21232)
+
0.0648(1.17142) + -0.05569(1.14132) + 0.0602(1.35732)
+
-0.05569(1.52262) + 0.0648(1.58972) + 0.1807(1.45782)
+
0.1807(1.35272) + 0.1807(1.39772) + 0.0602(1.45602)
+ 0.0602(1.30142)
+ 0.1807(1.32952) + 0.0648(1.55952)
+
0.0648(1.18732)
=
1.9136
σ[FS] = (1.9136 - 1.38212).5
= 0.05798
The standardized variable
(Eqn. 13) is:
Z
= (1.0 - 1.382)/0.058
= -6.59
The probability of failure
(Appendix A) is less than .003%.
5
Two
sites were selected by the
5.1
The
embankment at
SOIL
1 SOIL 2
φE φE
Mean
37.9 30.5
Std. Deviation 2.84 1.26
φ+ 40.74 31.76
φ- 35.06 29.24
The
resulting factors of safety from the computer program PCSTABL5 are:
FS++ = 2.763
FS+- = 2.658
FS-+ = 2.384
FS-- = 2.315
The
functions (Eqn. 6) for two soil types with 1 strength parameter per
layer is:
p++ = p+- = p-+ = p-- = 0.25
The
expected FS (Eqn.10a) is:
E[FS] = 0.25(2.763) + 0.25(2.658) +
0.25(2.384) +0 .25(2.315)
= 2.53
The
expected FS2 (Eqn. 10b) is:
E[FS2] = 0.25(2.763)2
+ 0.25(2.658)2 + 0.25(2.384)2 + 0.25(2.315)2
= 6.43
The
standard deviation of the FS's (Eqn. 11) is:
σ [FS] = [(6.34) - (2.53)2)].5
= 0.1859
The
standardized variable (Eqn. 13) is:
Z = (1-2.53)/0.1859 = -8.23
For
a FS = 1, where failure is assumed to occur, the probability of failure,
Pf , is (Appendix A):
Pf < 0.0002
This
probability of failure, according to Table 1, is acceptable for this slope.
5.2
MORRILTON
The
Morrilton site, based on the strength data supplied by the
6 CONCLUSION
The
reliability approach to slope stability is superior to the safety factor
approach because it accounts for variability in soil strength.
7 REFERENCES
Chowdhury,
R. N., Sept. 1994, "Decisions On Landslides Based on Risk
Assessment", International Conference on Landslides, Slope Stability and
the Safety of Infrastructures,
Christian,
John T., Charles C. Ladd, and Gregory B. Baecher, Dec. 1994, "Reliability
Applied to Slope Stability Analysis", Jour. of Geotechnical Engineers,
American Society of Civil Engineers, p 2181.
Garrett,
Steven Ray, 1988, Slope Failure Probability In Layered Soils, Master's
Thesis,
Harr,
M. E., 1987, Reliability Based Design in Civil Engineering, McGraw-Hill,
Inc., pp. 205-220.
McGuffey,
V., Z. Iori, Z. Kyfor, and D. Athanasoiu-Grivas, 1981, "Use of Point
Estimates for Probability Moments in Geotechnical Engineering", Transportation
Research Record 809, TRB, National Research Council, Washington D. C.
Rosenblueth,
Rosenblueth,
Santamarina,
J.C., A.G. Altschaeffl, and J.L. Chameau, Jan 1992, Reliability of Slopes,
Transportation Research Board, Paper #920569, Washington D. C.
Wright,
Stephen G., Fred H. Kulhaway, and James M. Duncan, Oct 1973, "Accuracy of
Equilibrium Slope Stability Analysis", Jour. Soil Mechanics and
Foundations, Amer. Soc. of Civil Engineers,
APPENDIX
A
NORMAL
DISTRIBUTION CURVE AREAS