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Risk Assessment in
Geotechnical Engineering
Presented by : Soumaya Addou スマイヤ アッドー
東北大学
1
References
This presentation is made based on the information provided by mainly these two books
2
3
Outline
I. Introduction of concepts
1) Uncertainty and risk in Geotechnical engineering
2) Probability Theory and Random Variables
3) Random Process Models
4) Definition of Risk
II. Uncertainty in Geotechnical Context
1) Site Characterization
2) Soil Variability
3) Spatial Variability within homogeneous Deposits
III.Reliability analysis Methods
1) Introduction: Steps and Approximations
2) Event Tree Analysis
3) First Order Second Moment Method (FOSM)
4) First Order Reliability Method (FORM)
5) Monte Carle Simulation
I. Introduction of concepts
Most of the early pioneers in Geotechnical Engineering were aware of the limitations of
purely rational, deductive approaches to the uncertain conditions that prevail in the
Geological world. Their later writings are full of warnings not to take the results of
laboratory tests and analytical calculations too literally
Recently, there has been a trend to apply the results of reliability theory to Geotechnical
engineering. The offshore and nuclear power are at the forefront for the use of these
approaches.
The variability inherent in soils and rocks suggests that geotechnical systems are highly
amenable to a statistical interpretation.
① Uncertainty and risk in Geotechnical engineering
4
Risk analysis
Natural
variability
Temporal Spatial
Knowledge
uncertainty
Model
Site
characterization
Parameters
Decision model
uncertainty
Objectives Values
Time
Preferences
I. Introduction of concepts
The types of uncertainties that arise in Engineering practice :
Engineering data on soil or rock mass properties are usually scattered
Usage of statistics and graphical and simple probabilistic methods
① Uncertainty and risk in Geotechnical engineering
5
I. Introduction of concepts
The mathematical theory of probability deals
with:
- Experiments “random process generating
specific and a priori unknown results”
- Their outcomes “sample space”
In Geotechnical Engineering, we mostly deal with probability as a density function and
Probability is found by integrating the probability mass over a finite region.
𝑃 𝐴 =
𝐴
𝑓𝑋 𝑥 𝑑𝑥
It is convenient sometimes to represent probability by their moments
𝐸 𝑥 𝑛
=
−∞
+∞
𝑥 𝑛
𝑓𝑋 𝑥 𝑑𝑥
The most common is the second central moment , called the variance
𝜎2
= 𝐸 𝑥 − 𝐸(𝑥) 2
𝐸 𝑥 is the arithmetic average called the mean.
② Probability Theory and Random Variables
6
I. Introduction of concepts
For an uncertain quantity , various forms for the Probability Functions have been suggested :
- Probability Mass Function (pmf) :
Binomial (success and failures) : 𝐹 𝑥 𝑛 = 𝑥
𝑛
𝑝 𝑥
(1 − 𝑝) 𝑛−𝑥
Poisson distribution : 𝑓 𝑥 λ =
λ 𝑥 𝑒−λ
𝑥!
….etc
- Probability Distribution Function (pdf):
Exponential distribution : 𝑓 𝑠 λ = λ𝑒−λ𝑠
The Normal Probability Distribution
….etc
http://slideplayer.com/slide/5710846/
③ Random Process Models
7
I. Introduction of concepts
The determinant of risk is the combination of uncertain event and the adverse
consequence
𝑅𝑖𝑠𝑘 = (𝑃𝑟𝑜𝑏𝑎𝑏𝑖𝑙𝑖𝑡𝑦, 𝐶𝑜𝑛𝑠𝑒𝑞𝑢𝑒𝑛𝑐𝑒)
④ Definition of Risk
Many approaches have been adopted to describe
risks.
They consist on plotting the exceedance
probability of risks against their associated
consequences.
Chart showing average annuals risks posed by a variety of
traditional civil facilities and other large structures .
8
II. Uncertainty in Geotechnical Context
① Site Characterization
Concerns information about the geometry and material properties of local geological formations,
mainly :
 The geological nature of deposits and formations
 Location, thickness and material composition
 Engineering properties of formations
 Ground water level and its fluctuations
The random process models
used are usually models of
“Spatial variation”
Probability is in the model not the ground 9
II. Uncertainty in Geotechnical Context
② Soil Variability
The variability of elementary soil properties concerns various categories of physical properties :
- Index and classification properties : bulk properties, classification properties, …etc
- Consolidation properties: 𝐶𝑐, 𝐶𝑟, 𝑐 𝑣…etc
- Permeability: hydraulic conductivity
- Strength Properties: CPT, SPT parameters, effective friction angle, …etc
Variability in soil properties is inextricably related to the particular site
and to a specific regional geology
Parameter Soil Recorded COV (%) Source
𝐶𝑐, 𝐶𝑟
𝑐 𝑣
Bangkok Clay
Various
Dredge Spoils
Gulf of Mexico Clay
Ariake Clay
Singapore Clay
Bangkok clay
20
25-50
35
25-28
10
17
16
Zhu et al. (2001)
Lumb (1974)
Thevanayagam et al (1996)
Baecher and Ladd (1997)
Tanaka et al. (2001)
Tanaka et al. (2001)
Tanaka et al. (2001)
Values of the variability in consolidation parameter, expressed as Coefficient of Variation
10
II. Uncertainty in Geotechnical Context
3) Spatial Variability within homogeneous Deposits
 Describing the variation of soil properties in space requires additional tools
 In order to characterize the spatial variation of a soil deposit, a large number of tests is required
Use of a model 𝑧(𝑥) = 𝑡 𝑥 + 𝑢(𝑥)
Soil property
at location x
Trend at x
deterministic
residual variation at x
“random variable”
Estimate the trend by fitting well-
defined mathematical functions to
data points
Use of methods like “Regression
analysis”
Fitting the same data with a line versus a curve changes the residual variance11
II. Uncertainty in Geotechnical Context
3) Spatial Variability within homogeneous Deposits
The spatial association of residuals off the trend is expressed by a mathematical function that
describes the correlation of two residuals separated by a distance 𝛿, this description is called the
autocorrelation function.
𝑅 𝑧(𝛿) =
𝐶𝑜𝑣(𝑢(𝑥𝑖), 𝑢(𝑥𝑗))
𝑉𝑎𝑟 𝑢(𝑥)
𝑉𝑎𝑟 𝑢(𝑥) : The variance of the residuals across the site
Autocorrelation of rock fracture density in a copper porphyry deposit
12
III. Reliability analysis Methods
① Introduction: Steps and Approximations
Reliability analysis deals with the relation between the loads “Q” a system carry, and its ability to
carry those loads “R”.
The goal of the analysis is to estimate the probability of failure 𝒑 𝒇, the steps are :
1. Establish an analytical model
2. Estimate statistical descriptions of the parameters
3. Calculate statistical moments of the performance function
4. Calculate the reliability index
5. Compute the probability of failure
I. First Order Second Moment Method (FOSM)
II. First Order Reliability Method (FORM)
III. Monte Carle Simulation
…..etc 13
III. Reliability analysis Methods
② Event Tree Analysis
A graphical representation of the many chains of events that might result from some initiating event.
Its objective is to provide the Probability of system failure.
Example of event tree of the probability of embankment breach of a dam due to liquefaction
The event tree
begins with an
accident initiating
event : Earthquake,
flood,….etc
A joint probability is obtained by multiplying the conditional event probabilities along the chain
14
III. Reliability analysis Methods
③ First Order Second Moment Method (FOSM)
It uses the first terms of a Taylor series expansion of the performance function “F” to estimate the
expected value and variance of the performance function. When the variables are uncorrelated
Example : The James Bay Dikes
“Reliability Applied to Slope Stability Analysis” John T. Christian; Charles C. Ladd, and Gregory B. Baecher, 1994.
Uncertainties
in soil
properties
Scatter
- Spatial Variability
- noise
𝛼𝑐 𝑢 𝐹𝑉 = 𝑐 𝑢 + 𝑐 𝑒
Systematic
error
- Limited number of tests
- Bias :
Ex : The factor α is a
function of the plasticity
index. It is taken 𝛼 = 1
𝑐 𝑒 is a random experimental error.
Should not be included in stability analysis
to be found by “Autocovariance function” 15
Identify all
the variables
Determine the best
estimate of each
variable (The mean)
and the best estimate
of the factor of Safety
Estimate the
uncertainty
(the
variance)
Calculate the
partial
derivatives
∆𝐹
∆𝑋𝑖
Obtain
𝑉𝑎𝑟 𝐹
Calculate 𝛽
then
Probability
of failure 𝑝 𝑓
III. Reliability analysis Methods
③ First Order Second Moment Method (FOSM)
FOSM Calculations
The variance 𝜎 𝐹
2
= 𝑖=1
𝑛
𝑗=1
𝑛 𝜕𝐹
𝜕𝑋 𝑖
𝜕𝐹
𝜕𝑋 𝑗
𝜌 𝑋 𝑖 𝑋 𝑗
𝜎 𝑋𝑖
𝜎 𝑋 𝑗
Reliability index 𝛽 =
𝐸 𝐹 −1
𝜎 𝐹
• Factor of Safety
• Soil Profile and fill Properties
• Shear strength of foundation
clay
𝑝 𝑓 were computed on the assumption that F is normally distributed
16
 The selected 𝑝 𝑓 was selected smaller
for higher embankments
 Based on the revised target probabilities,
one obtains the consistent, desired
factors of safety.
III. Reliability analysis Methods
④ First Order Reliability Method (FORM)
This method, developed by Hasofer and Lind (1974) addressed some concerns about some
assumptions involved in the FOSM method.
For each variable 𝑥𝑖, we define 𝑥′
𝑖 having a mean value of zero and unit standard deviation.
𝑥′
𝑖 =
𝑥𝑖 − 𝜇 𝑥𝑖
𝜎𝑥𝑖
17
Limit state function
𝑔 𝑥′
1, 𝑥′
2, … , 𝑥′
𝑛 = 0
Safe and unsafe regions (Du. 2005)
 Reliability index is interpreted geometrically as
the distance between the point defined by the
expected values of the variables and the closest
point on the failure criterion.
 The probability of failure is the volume of the
hill on the failure side.
III. Reliability analysis Methods
④ First Order Reliability Method (FORM)
Lagrange’s multipliers is used to
find the minimum distance as :
𝛽 = 𝑑 𝑚𝑖𝑛 = −
𝑥′∗
𝑖
𝜕𝑔
𝜕𝑥′ 𝑖 ∗
𝜕𝑔
𝜕𝑥′ 𝑖 ∗
2
The design point in the reduced
coordinate is :
𝑥′∗
𝑖 = −𝛼𝑖 𝛽
With 𝛼𝑖=
𝜕𝑔
𝜕𝑥′ 𝑖
𝜕𝑔
𝜕𝑥′ 𝑖 ∗
2
18
1. Define the limit state equation
2. Assume initial values of 𝑥′𝑖 and obtain reduced variables
𝑥′
𝑖 =
𝑥 𝑖−𝜇 𝑥 𝑖
𝜎 𝑥 𝑖
3.Evaluate 𝜕𝑔
𝜕𝑥′𝑖
and 𝛼𝑖 at 𝑥′
𝑖∗
4.Obtain the new design point 𝑥′
𝑖∗ in terms of 𝛽
5. Substitute the new 𝑥′
𝑖∗ in the limit state equation 𝑔(𝑥′
𝑖∗)=0
and solve for 𝛽
6. Using the 𝛽 value obtained in step 5, re-evaluate
𝑥′∗
𝑖 = −𝛼𝑖 𝛽
7.Repeat steps 3 through 6 until 𝛽 converges
Rackwitz algorithm
19
III. Reliability analysis Methods
⑤ Monte Carlo Simulation Methods
Example :
A system has 2 random inputs 𝑍1 and 𝑍2, the response is a random function 𝑔(𝑍1, 𝑍2)
System failure occurs if 𝑔(𝑍1, 𝑍2) > 𝑔 𝑐𝑟𝑖𝑡
We want to find 𝑝 𝑓 = 𝑃 𝑔(𝑍1, 𝑍2) > 𝑔 𝑐𝑟𝑖𝑡
𝑍1 and 𝑍2 follow a certain probability distribution, so the 𝑝 𝑓 can be expressed in terms of the
joint probability density function
𝑝 𝑓 =
𝑧2∈𝐹 𝑧1∈𝐹
𝑓𝑧1 𝑧2
𝑧1, 𝑧2 𝑑𝑧1 𝑑𝑧
F: the failure region
This kind of integrals can be evaluated in most cases numerically
Monte Carlo Simulation
20
III. Reliability analysis Methods
⑤ Monte Carlo Simulation Methods
After simulating the random realizations of 𝑍1 and 𝑍2, 𝑔(𝑍1, 𝑍2) is evaluated for each.
we check if 𝑔(𝑍1, 𝑍2) > 𝑔 𝑐𝑟𝑖𝑡
𝐼𝑖 =
1 if 𝑔(𝑧𝑖1, 𝑧𝑖2) > 𝑔 𝑐𝑟𝑖𝑡
0 𝑜𝑡ℎ𝑒𝑟𝑤𝑖𝑠𝑒
The estimate of the probability is 𝑝 𝑓 =
1
𝑛 𝑖=1
𝑛
𝐼𝑖
Thank you for your attention
ご清聴ありがとうございました
21

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Risk Assessment in Geotechnical Engineering

  • 1. Risk Assessment in Geotechnical Engineering Presented by : Soumaya Addou スマイヤ アッドー 東北大学 1
  • 2. References This presentation is made based on the information provided by mainly these two books 2
  • 3. 3 Outline I. Introduction of concepts 1) Uncertainty and risk in Geotechnical engineering 2) Probability Theory and Random Variables 3) Random Process Models 4) Definition of Risk II. Uncertainty in Geotechnical Context 1) Site Characterization 2) Soil Variability 3) Spatial Variability within homogeneous Deposits III.Reliability analysis Methods 1) Introduction: Steps and Approximations 2) Event Tree Analysis 3) First Order Second Moment Method (FOSM) 4) First Order Reliability Method (FORM) 5) Monte Carle Simulation
  • 4. I. Introduction of concepts Most of the early pioneers in Geotechnical Engineering were aware of the limitations of purely rational, deductive approaches to the uncertain conditions that prevail in the Geological world. Their later writings are full of warnings not to take the results of laboratory tests and analytical calculations too literally Recently, there has been a trend to apply the results of reliability theory to Geotechnical engineering. The offshore and nuclear power are at the forefront for the use of these approaches. The variability inherent in soils and rocks suggests that geotechnical systems are highly amenable to a statistical interpretation. ① Uncertainty and risk in Geotechnical engineering 4
  • 5. Risk analysis Natural variability Temporal Spatial Knowledge uncertainty Model Site characterization Parameters Decision model uncertainty Objectives Values Time Preferences I. Introduction of concepts The types of uncertainties that arise in Engineering practice : Engineering data on soil or rock mass properties are usually scattered Usage of statistics and graphical and simple probabilistic methods ① Uncertainty and risk in Geotechnical engineering 5
  • 6. I. Introduction of concepts The mathematical theory of probability deals with: - Experiments “random process generating specific and a priori unknown results” - Their outcomes “sample space” In Geotechnical Engineering, we mostly deal with probability as a density function and Probability is found by integrating the probability mass over a finite region. 𝑃 𝐴 = 𝐴 𝑓𝑋 𝑥 𝑑𝑥 It is convenient sometimes to represent probability by their moments 𝐸 𝑥 𝑛 = −∞ +∞ 𝑥 𝑛 𝑓𝑋 𝑥 𝑑𝑥 The most common is the second central moment , called the variance 𝜎2 = 𝐸 𝑥 − 𝐸(𝑥) 2 𝐸 𝑥 is the arithmetic average called the mean. ② Probability Theory and Random Variables 6
  • 7. I. Introduction of concepts For an uncertain quantity , various forms for the Probability Functions have been suggested : - Probability Mass Function (pmf) : Binomial (success and failures) : 𝐹 𝑥 𝑛 = 𝑥 𝑛 𝑝 𝑥 (1 − 𝑝) 𝑛−𝑥 Poisson distribution : 𝑓 𝑥 λ = λ 𝑥 𝑒−λ 𝑥! ….etc - Probability Distribution Function (pdf): Exponential distribution : 𝑓 𝑠 λ = λ𝑒−λ𝑠 The Normal Probability Distribution ….etc http://slideplayer.com/slide/5710846/ ③ Random Process Models 7
  • 8. I. Introduction of concepts The determinant of risk is the combination of uncertain event and the adverse consequence 𝑅𝑖𝑠𝑘 = (𝑃𝑟𝑜𝑏𝑎𝑏𝑖𝑙𝑖𝑡𝑦, 𝐶𝑜𝑛𝑠𝑒𝑞𝑢𝑒𝑛𝑐𝑒) ④ Definition of Risk Many approaches have been adopted to describe risks. They consist on plotting the exceedance probability of risks against their associated consequences. Chart showing average annuals risks posed by a variety of traditional civil facilities and other large structures . 8
  • 9. II. Uncertainty in Geotechnical Context ① Site Characterization Concerns information about the geometry and material properties of local geological formations, mainly :  The geological nature of deposits and formations  Location, thickness and material composition  Engineering properties of formations  Ground water level and its fluctuations The random process models used are usually models of “Spatial variation” Probability is in the model not the ground 9
  • 10. II. Uncertainty in Geotechnical Context ② Soil Variability The variability of elementary soil properties concerns various categories of physical properties : - Index and classification properties : bulk properties, classification properties, …etc - Consolidation properties: 𝐶𝑐, 𝐶𝑟, 𝑐 𝑣…etc - Permeability: hydraulic conductivity - Strength Properties: CPT, SPT parameters, effective friction angle, …etc Variability in soil properties is inextricably related to the particular site and to a specific regional geology Parameter Soil Recorded COV (%) Source 𝐶𝑐, 𝐶𝑟 𝑐 𝑣 Bangkok Clay Various Dredge Spoils Gulf of Mexico Clay Ariake Clay Singapore Clay Bangkok clay 20 25-50 35 25-28 10 17 16 Zhu et al. (2001) Lumb (1974) Thevanayagam et al (1996) Baecher and Ladd (1997) Tanaka et al. (2001) Tanaka et al. (2001) Tanaka et al. (2001) Values of the variability in consolidation parameter, expressed as Coefficient of Variation 10
  • 11. II. Uncertainty in Geotechnical Context 3) Spatial Variability within homogeneous Deposits  Describing the variation of soil properties in space requires additional tools  In order to characterize the spatial variation of a soil deposit, a large number of tests is required Use of a model 𝑧(𝑥) = 𝑡 𝑥 + 𝑢(𝑥) Soil property at location x Trend at x deterministic residual variation at x “random variable” Estimate the trend by fitting well- defined mathematical functions to data points Use of methods like “Regression analysis” Fitting the same data with a line versus a curve changes the residual variance11
  • 12. II. Uncertainty in Geotechnical Context 3) Spatial Variability within homogeneous Deposits The spatial association of residuals off the trend is expressed by a mathematical function that describes the correlation of two residuals separated by a distance 𝛿, this description is called the autocorrelation function. 𝑅 𝑧(𝛿) = 𝐶𝑜𝑣(𝑢(𝑥𝑖), 𝑢(𝑥𝑗)) 𝑉𝑎𝑟 𝑢(𝑥) 𝑉𝑎𝑟 𝑢(𝑥) : The variance of the residuals across the site Autocorrelation of rock fracture density in a copper porphyry deposit 12
  • 13. III. Reliability analysis Methods ① Introduction: Steps and Approximations Reliability analysis deals with the relation between the loads “Q” a system carry, and its ability to carry those loads “R”. The goal of the analysis is to estimate the probability of failure 𝒑 𝒇, the steps are : 1. Establish an analytical model 2. Estimate statistical descriptions of the parameters 3. Calculate statistical moments of the performance function 4. Calculate the reliability index 5. Compute the probability of failure I. First Order Second Moment Method (FOSM) II. First Order Reliability Method (FORM) III. Monte Carle Simulation …..etc 13
  • 14. III. Reliability analysis Methods ② Event Tree Analysis A graphical representation of the many chains of events that might result from some initiating event. Its objective is to provide the Probability of system failure. Example of event tree of the probability of embankment breach of a dam due to liquefaction The event tree begins with an accident initiating event : Earthquake, flood,….etc A joint probability is obtained by multiplying the conditional event probabilities along the chain 14
  • 15. III. Reliability analysis Methods ③ First Order Second Moment Method (FOSM) It uses the first terms of a Taylor series expansion of the performance function “F” to estimate the expected value and variance of the performance function. When the variables are uncorrelated Example : The James Bay Dikes “Reliability Applied to Slope Stability Analysis” John T. Christian; Charles C. Ladd, and Gregory B. Baecher, 1994. Uncertainties in soil properties Scatter - Spatial Variability - noise 𝛼𝑐 𝑢 𝐹𝑉 = 𝑐 𝑢 + 𝑐 𝑒 Systematic error - Limited number of tests - Bias : Ex : The factor α is a function of the plasticity index. It is taken 𝛼 = 1 𝑐 𝑒 is a random experimental error. Should not be included in stability analysis to be found by “Autocovariance function” 15
  • 16. Identify all the variables Determine the best estimate of each variable (The mean) and the best estimate of the factor of Safety Estimate the uncertainty (the variance) Calculate the partial derivatives ∆𝐹 ∆𝑋𝑖 Obtain 𝑉𝑎𝑟 𝐹 Calculate 𝛽 then Probability of failure 𝑝 𝑓 III. Reliability analysis Methods ③ First Order Second Moment Method (FOSM) FOSM Calculations The variance 𝜎 𝐹 2 = 𝑖=1 𝑛 𝑗=1 𝑛 𝜕𝐹 𝜕𝑋 𝑖 𝜕𝐹 𝜕𝑋 𝑗 𝜌 𝑋 𝑖 𝑋 𝑗 𝜎 𝑋𝑖 𝜎 𝑋 𝑗 Reliability index 𝛽 = 𝐸 𝐹 −1 𝜎 𝐹 • Factor of Safety • Soil Profile and fill Properties • Shear strength of foundation clay 𝑝 𝑓 were computed on the assumption that F is normally distributed 16  The selected 𝑝 𝑓 was selected smaller for higher embankments  Based on the revised target probabilities, one obtains the consistent, desired factors of safety.
  • 17. III. Reliability analysis Methods ④ First Order Reliability Method (FORM) This method, developed by Hasofer and Lind (1974) addressed some concerns about some assumptions involved in the FOSM method. For each variable 𝑥𝑖, we define 𝑥′ 𝑖 having a mean value of zero and unit standard deviation. 𝑥′ 𝑖 = 𝑥𝑖 − 𝜇 𝑥𝑖 𝜎𝑥𝑖 17 Limit state function 𝑔 𝑥′ 1, 𝑥′ 2, … , 𝑥′ 𝑛 = 0 Safe and unsafe regions (Du. 2005)  Reliability index is interpreted geometrically as the distance between the point defined by the expected values of the variables and the closest point on the failure criterion.  The probability of failure is the volume of the hill on the failure side.
  • 18. III. Reliability analysis Methods ④ First Order Reliability Method (FORM) Lagrange’s multipliers is used to find the minimum distance as : 𝛽 = 𝑑 𝑚𝑖𝑛 = − 𝑥′∗ 𝑖 𝜕𝑔 𝜕𝑥′ 𝑖 ∗ 𝜕𝑔 𝜕𝑥′ 𝑖 ∗ 2 The design point in the reduced coordinate is : 𝑥′∗ 𝑖 = −𝛼𝑖 𝛽 With 𝛼𝑖= 𝜕𝑔 𝜕𝑥′ 𝑖 𝜕𝑔 𝜕𝑥′ 𝑖 ∗ 2 18 1. Define the limit state equation 2. Assume initial values of 𝑥′𝑖 and obtain reduced variables 𝑥′ 𝑖 = 𝑥 𝑖−𝜇 𝑥 𝑖 𝜎 𝑥 𝑖 3.Evaluate 𝜕𝑔 𝜕𝑥′𝑖 and 𝛼𝑖 at 𝑥′ 𝑖∗ 4.Obtain the new design point 𝑥′ 𝑖∗ in terms of 𝛽 5. Substitute the new 𝑥′ 𝑖∗ in the limit state equation 𝑔(𝑥′ 𝑖∗)=0 and solve for 𝛽 6. Using the 𝛽 value obtained in step 5, re-evaluate 𝑥′∗ 𝑖 = −𝛼𝑖 𝛽 7.Repeat steps 3 through 6 until 𝛽 converges Rackwitz algorithm
  • 19. 19 III. Reliability analysis Methods ⑤ Monte Carlo Simulation Methods Example : A system has 2 random inputs 𝑍1 and 𝑍2, the response is a random function 𝑔(𝑍1, 𝑍2) System failure occurs if 𝑔(𝑍1, 𝑍2) > 𝑔 𝑐𝑟𝑖𝑡 We want to find 𝑝 𝑓 = 𝑃 𝑔(𝑍1, 𝑍2) > 𝑔 𝑐𝑟𝑖𝑡 𝑍1 and 𝑍2 follow a certain probability distribution, so the 𝑝 𝑓 can be expressed in terms of the joint probability density function 𝑝 𝑓 = 𝑧2∈𝐹 𝑧1∈𝐹 𝑓𝑧1 𝑧2 𝑧1, 𝑧2 𝑑𝑧1 𝑑𝑧 F: the failure region This kind of integrals can be evaluated in most cases numerically Monte Carlo Simulation
  • 20. 20 III. Reliability analysis Methods ⑤ Monte Carlo Simulation Methods After simulating the random realizations of 𝑍1 and 𝑍2, 𝑔(𝑍1, 𝑍2) is evaluated for each. we check if 𝑔(𝑍1, 𝑍2) > 𝑔 𝑐𝑟𝑖𝑡 𝐼𝑖 = 1 if 𝑔(𝑧𝑖1, 𝑧𝑖2) > 𝑔 𝑐𝑟𝑖𝑡 0 𝑜𝑡ℎ𝑒𝑟𝑤𝑖𝑠𝑒 The estimate of the probability is 𝑝 𝑓 = 1 𝑛 𝑖=1 𝑛 𝐼𝑖
  • 21. Thank you for your attention ご清聴ありがとうございました 21

Notes de l'éditeur

  1. Page 23 - 24 Natural : associated with inherent randomness of natural processes manifesting as variability over time and for phenomena that take time at a single location, or as variability over space for phenomena that take place at different locations but at single time or variability over both time and space Knowledge : attributed to lack of data, lack of information about events and processes or lack of understanding of physical laws that limits our ability to model the real world. - Site :subsurface geology resulting from data and exploration uncertainties - Model: the degree to which a mathematical model accurately mimics reality - Parameter: precision to which model parameters can be estimated - Inability to know social objectives, values and time preferences.
  2. Modeling site characterization involves the following steps: -Develop hypotheses about site geology Build a random process model based on the hypotheses Make observations in the field or laboratory Perform statistical analysis of the observations to draw inferences about the random process model Apply des\cision analysis to optimize the type, number and location of observations
  3. It is not wise to apply typical values of soil property variability from other sites in performing a reliability analysis. Cc: compression index, Cr: recompression index, cv: coefficient of consolidation
  4. So means and standard deviations are used to describe the variability in a set of soil property data. But they mask spatial information. The trend is determined by an equation and the residuals are characterized statistically by a random variable. Data are used to estimate a smooth trend, and remaining variations are described statistically, the variance of the residual reflects the uncertainty
  5. Since changing the trend changes Rz, the autocorrelation function reflects a modelling decision too.
  6. Both the loads and resistance may be uncertain. It means finding a way to compute the margin of safety, factor of safety or other measure of performance like a simple equation or a computational procedure. The parameters include the properties of geotechnical materials and also loads and geometry. Usually they are described by their means, variances and covariances. This usually means calculating the mean and variance of the performance function. Calculate calculate
  7. Provide insight into the functioning of a system and into the associated uncertainties about the way the system functions. The analysis attempts to generate all the subsequent events. The event outcomes are represented as branches issuing from the chance node representing a particular event. A conditional probability is associated with each event
  8. 𝜌 𝑋 𝑖 𝑋 𝑗 is the covariance between two variables - The James Bay project required the construction of 50 Km of dikes on soft sensitive clays. The method was used to evaluate the single or multi-stage construction of a typical dike whose cross section is the following. The goal of the analysis is to understand the relative safety of different designs, obtain insights about the influence of different parameters and establish consistent criteria for preliminary designs. The random experimental variations represented by 𝑐 𝑒 due to error in measurements and small scale fluctuations in soil must be eliminated to find the shear strength. Only the spatial variance represent a real effect that occurs in the field and needs to be taken into account. A limited number of tests is used and different set of measurements would yield a different estimate, the bias means that the experimental technique may not measure directly the quantity of interest
  9. 𝜎 𝐹 the variance. 𝐸 𝐹 the mean The function can be differentiated formally or numerically by divided differences Factor of safety : method of slices is used so numerical method is required to evaluate the variance Soil profile and fill properties : thickness of the crust, the depth to the till, unit weight, friction angle Shear strength : for single stage analyses, uncertainty in 𝑐 𝑢 is based on the field vane data. For multi stage case, shear strengths were established from a combination of undrained strength ratios and the in situ stress history To extrapolate the results there are two way, one could assume that the variance of F is constant or assume that the coefficient of variation is constant Conclusion : target probabilities are being selected based on reasons such as the relative contribution of different modes of failure. The target probability selection depends also on the costs of reconstruction ( The probability was reduced with the increase of the height of the embankment)
  10. The FOSM method involve some approximations that may not be acceptable : Suppose that the moments of the failure criterion can be estimated accurately enough by starting with the mean values of the variables and extrapolating linearly. The from of the distribution of F is known and can be used to compute 𝑝 𝑓 The objective from transforming the variables 𝑥 𝑖 into 𝑥 ′ 𝑖 is to obtain a standardized space of Normal variables to aid in the computation of reliability Index.
  11. Finally the reliability index is used to find the probability of failure