Title: WP 3 : DESIGN TOOLS
1- WP 3 DESIGN TOOLS
- PART 1 USE OF FINITE ELEMENT METHOD
- IN GEOTECHNICAL DESIGN
- Overview of the basic document
2- WP 3 DESIGN TOOLS
- PART 1 USE OF FINITE ELEMENT METHOD
- IN GEOTECHNICAL DESIGN
- Overview of the basic document
- Choice of soil model, parameters and initial
stresses
3- WP 3 DESIGN TOOLS
- PART 1 USE OF FINITE ELEMENT METHOD
- IN GEOTECHNICAL DESIGN
- Overview of the basic document
- Choice of soil model, parameters and initial
stresses - Proposal of future actions
4 OVERVIEW OF THE BASIC
DOCUMENT New version will be soon
available on the website
5- Different types of numerical methods
- Value of numerical methods
- Fundamental principles of FEM
- Approach for the user
- FEM for different types of construction
- Inventory of ressources
- List of references
6- Different types of numerical methods
- Value of numerical methods
- Fundamental principles of FEM
- Approach for the user
- FEM for different types of construction
- Inventory of ressources
- List of references
7Value of numerical methods
- When analytical methods are insufficient or
impossible - Complex geometry
- Soil-structure interaction
- Settlements
8Value of numerical methods
- When analytical methods are insufficient or
impossible - Complex geometry
- Soil-structure interaction
- Settlements
- To
- Calculate stresses and deformations and compare
them to allowable values - Parameter studies
9Value of numerical methods
- Tool for Observational Method
- To identify representative and critical locations
for installation of measuring apparatus - Measurements during early stages ? calibration of
the model ? better prediction of final situation
? possibility of early intervention
10Approach for the user sources of uncertainties
- Numerical aspects
- convergence,
- discretisation,
11Approach for the user Sources of uncertainties
- Numerical aspects
- convergence,
- discretisation,
- Models
- geometry,
- soil,
- structural elements,
- interfaces,
- construction stages
12Approach for the user Sources of uncertainties
- Numerical aspects
- convergence,
- discretisation,
- Type of analysis
- drained/undrained/consolidation,
- initial stresses,
- water condition
- Models
- geometry,
- soil,
- structural elements,
- interfaces,
- construction stages
13Approach for the user Sources of uncertainties
- Numerical aspects
- convergence,
- discretisation,
- Type of analysis
- drained/undrained/consolidation,
- initial stresses,
- water condition
- Models
- geometry,
- soil,
- structural elements,
- interfaces,
- construction stages
- Model parameters
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15Approach for the user Sources of uncertainties
- Numerical aspects
- convergence,
- discretisation,
- Type of analysis
- drained/undrained/consolidation,
- initial stresses,
- water condition
- Models
- geometry,
- soil,
- structural elements,
- interfaces,
- construction stages
- Model parameters
16 CHOICE OF SOIL MODEL, PARAMETERSAND INITIAL
STRESSES
17Choice of soil model
- Because of none of the currently availabe soil
constitutive models can reproduce all of the
aspects of real soil behaviour, one have to make
a choice, taking into account - the nature of the subsoil,
18Choice of soil model
- Because of none of the currently availabe soil
constitutive models can reproduce all of the
aspects of real soil behaviour, one have to make
a choice, taking into account - the nature of the subsoil,
- the soil features that govern te behaviour of a
particular geotechnical problem stiffness,
strength,
19Choice of soil model
- Because of none of the currently availabe soil
constitutive models can reproduce all of the
aspects of real soil behaviour, one have to make
a choice, taking into account - the nature of the subsoil,
- the soil features that govern te behaviour of a
particular geotechnical problem stiffness,
strength, - the availability of soil data
20Choice of soil model
- Elastic material models
- Elasto-plastic material models
- Different programming codes of essentially the
same material model may lead to different answers
!!! - Strain hardening and strain softening material
models - Stress history
- Real soil behaviour strongly depends on previous
and current stress paths, stress history. This
may be described by introducing several moving
yield surfaces or "history surfaces"
21Choice of soil model
22Choice of soil model
- Example Tests on shallow foundation at Labenne
(sand) - Mestat, Berthelon
- In general better results with the Nova model
(elasto-plastic with hardening) than with the MC
model
23Choice of soil model
- LSD 2000 International Workshop on Limit State
Design in Geotechnical Engineering - Melbourne, Australia, 18 November 2000
- Some Considerations on the Use of Finite
Element Methods in Ultimate Limit State Design - C. Bauduin
- Besix, Brussels Brussels University
- M. De Vos
- Belgian Building Research Institute, Brussels
- B. Simpson
- Arup Geotechnics, London
24Choice of soil model
- Examples, using MC and hardening model
- seems to be no significant effect on the ULS of
the soil - more significant role on the ULS in structural
elements, especially for stiff, brittle
structures ? advanced model may be needed
25Choice of soil model
- Empfehlungen des Arbeitskreises Numerik in der
Geotechnik - Although a linear elastic model is a very
simplified way to represent soil behaviour, it
gives often a good estimation (bearing capacity,
forces, soil-structure interaction,)
26Choice of soil model
- David M Potts and Lidjia Zdravkovic, 2001
-
- Soil dilation can have a dominant effect on pile
behaviour and consequently care must be exercised
when selecting an appropriate constitutive model
and its parameters
27Choice of soil model
- Guidelines are sometimes confusing
- more detailed analysis is needed
28Input parameters
- Measured values of soil properties can be
greatly affected by factors such as sampling,
handling and preparation, precision of testing
technique, -
- Confining pressure the stress-strain behaviour
of soil is nonlinear. For all cases except
saturated soil under undrained conditions, the
stress strain behaviour of soil depends on
confining pressure. - Preliminary design values from litterature,
experience - Design values from tests if necessary,
perform a calculation with upper and lower limit
of parameter values
29Input parameters
- Tests for parameter determination
- Laboratory tests
- Field tests
- Correlations with index property values
- Calibration studies
30Input parameters
- Calibration studies
- In many cases, designers have experience with
local soils and are skilled at calculating 1-D
consolidation settlements using conventional
procedures. It is good practice in such cases to
develop a 1-D column of finite elements that
models the soil profile at the site of interest.
The 1-D column can be loaded and the resulting
settlements compared to those calculated using
conventional procedures. The material property
values for the finite element analyses can be
adjusted until a match is obtained. Similarly, if
an independent estimate of the lateral load
response, i.e., the Poisson effect, can be made,
the material property values can be adjusted
until the 1-D column results match the
independent estimate. Ideally, one set of
material property values would be found that
provides a match to both the compressibility and
the lateral load response over the range of
applied loads in the problem to be analysed.
31Input parameters
- Illustration with case studies
- Limelette
- Sint Katelijne Waver
32Limelette site
Input parameters
33CPTs (qc) Limelettedynamic field static field
Input parameters
34Sint Katelijne Waver site
Input parameters
35CPTs (qc) Sint Katelijne Waver
Input parameters
36Strength parameter F ( Limelette )
Input parameters
- Application of correlations established for
sands from in situ tests to the sandy layer in
Limelette (8,2m 16m) - From CPTs
- Robertson Campanella, 1983
- Meyerhoff, 1956
- Olsen Farr, 1986
- From SPTs
- Stroud, 1989 (OCR 3)
- Peck et al, 1974
- Terzaghi Peck, 1967
- From DMTs
- Durgonoglu Mitchell (OCR 3)
37Static field
Input parameters
38Dynamic field
Input parameters
39Strength parameter F ( Limelette )
Input parameters
- Application of correlations established for
silts from in situ tests to the silty layer in
Limelette (2,2m 6,2m) - From SPTs
- Terzaghi Peck, 1967
- From DMTs
- Durgunoglu Mitchell
40Static field
Input parameters
41Dynamic field
Input parameters
42Summary ? Sand Limelette
Input parameters
- Static field
- 8,2-10,2m
- From CPTs Fpeak 41 47
- From SPTs Fpeak 35 38
- From DMTs Fpeak 40
- 10,2-16m
- From CPTs Fpeak 38 44
- From SPTs Fpeak 35 38
- From DMTs Fpeak 40
- Triaxial tests Fpeak 35
- Dynamic field
- 8,2-10,2m
- From CPTs Fpeak 41 46
- From SPTs Fpeak 35 38
- From DMTs Fpeak 40
- 10,2-12,2m
- From CPTs Fpeak 40 44
- From SPTs Fpeak 35 38
- From DMTs Fpeak 40
- 12,2-16m
- From CPTs Fpeak 38 42,5
- From SPTs Fpeak 34 37
- From DMTs Fpeak 40
- Triaxial tests Fpeak 35
43Summary ? Silt Limelette
Input parameters
- Static field
- From SPTs Fpeak 31 35
- From DMTs Fpeak 35
- Triaxial tests Fpeak 35
- Dynamic field
- From SPTs Fpeak 31 35
- From DMTs Fpeak 35
- Triaxial tests Fpeak 35
44 Conclusions determination of F
(Sand Silt Limelette)
Input parameters
- CPTs correlations are established mainly for
sandy soils. When applicated to the sandy layer
of the Limelette site, the differences between
the different correlations arein the range of 5. - SPTs correlations are established for silty and
sandy soils. When applicated to the sandy layer
of the Limelette site, the differences are in the
range of 3. - DMTs correlations are established for silty and
sandy soils. - Comparison between the Fpeak value deduced from
CPTs, SPTs, DMTs and triaxial tests - Fpeak,triaxial Fpeak, DMT lt Fpeak,SPT lt
Fpeak, CPT
45Strength parameter cu ( Sint Katelijne Waver )
Input parameters
- Application of correlations established for
clays from in situ tests to the stiff
overconsolidated tertiary clay of Sint Katelijne
Waver - From CPTs
- Carpentier, 1970
- Marsland Quaterma, 1982
- From SPTs
- Stroud, 1989
- From DMTs
- Marchetti, 1980
46Input parameters
47Summary cuTertiary Overconsolidated Clay Sint
Katelijne Waver
Input parameters
- From CPT (Carpentier) cu (kPa) 8,22 z (m)
65 - From CPT (Marsland and Quaterma) cu (kPa)
5,01 z (m) 46 - From SPT (Stroud) cu (kPa) 5,18 z (m) 47
- From DMT (Marchetti) cu (kPa) 12,26 z (m)
50 - UU triaxial tests cu (kPa) 11,3 z (m) 34
48Deformation parameter Eoed ( Limelette )
Input parameters
- Application of correlations from in situ tests
to the site of Limelette - From CPTs
- Sanglerat, 1972
- From PMTs
- Nuyens
- From DMTs
- Totani, Marchetti, Monaco Calabrese
49Static field
Input parameters
50Dynamic field
Input parameters
51Deformation parameter Eoed ( Sint Katelijne
Waver )
Input parameters
- Application of correlations established for
clays from in situ tests to the stiff
overconsolidated tertiary clay of Sint Katelijne
Waver - From CPTs
- Sanglerat, 1972
- From PMTs
- Nuyens
52Input parameters
53Input parameters
- Example Tests on shallow foundation at Labenne
(sand) - Mestat, Berthelon
- Vertical displacements are largely underestimated
(soil model MC). - The causes of this may be
- Fluctuation of the water level, capillary
cohesion, no-representativity of the laboratory
tests, simplicity of the MC model, local
heterogeneities - Mostly wrong estimation of the Young modulus.
From laboratory test initial modulus, more
realistic lower modulus, for example from in
situ pressiometric tests (contrary to the
simulation of other constructions where the
values of laboratory tests gave acceptable
results).
54Input parameters
- importance of calibration studies
- be careful with correlations
- more information needed more specific per
region/country ? - deformation parameters from in situ tests
better from PMT ? - taking into account the soil model used
55Initial stresses
- Empfehlungen des Arbeitskreises Numerik in der
Geotechnik - initial stress state often an important
factor - The initial stress state depends on
- soil density
- soil shear strength characteristics
- load history (geology, consolidation)
- la yers in rock
- sliding surfaces
- water flow
56Initial stresses
- Empfehlungen des Arbeitskreises Numerik in der
Geotechnik - initial stress state often an important
factor - The initial stress state depends on
- soil density
- soil shear strength characteristics
- load history (geology, consolidation)
- la yers in rock
- sliding surfaces
- water flow
-
- ? difficult to predict with precision
57Initial stresses
- perform different calculations with different
initial stresses - include the history in the first calculation step
- impose displacements of nodes
- first, perform a calculation with a large soil
volume, - then, perform a calculation with a smaller soil
volume for which the bounderies are taken from
the first calculation
58Initial stresses
- LSD 2000 International Workshop on Limit State
Design in Geotechnical Engineering - Melbourne, Australia, 18 November 2000
- Some Considerations on the Use of Finite
Element Methods in Ultimate Limit State Design - C. Bauduin
- Besix, Brussels Brussels University
- M. De Vos
- Belgian Building Research Institute, Brussels
- B. Simpson
- Arup Geotechnics, London
59Initial stresses
Design Characteristic value
value Soil strength parameters Init.
stresses M d1, Ad1 Stage
1 Md2, Ad2 Stage 2
Stage 3 Final situation Time
(stage)
60Initial stresses
- NC soils MC or hardening model
- no significant effect of initial stress field
(characteristic or design) on ultimate state of
the soil - may be very important, when looking to ULS in
structural elements
61 PROPOSAL OF FUTURE ACTIONS
62Future actions
- add other available information (Cost C7,
benchmarks,), with special attention to - soil models
- (initial stresses)
- parameter determination strength / deformation
- others ?
- summary of benchmarks
- (new benchmarks)
63Future actions
- application of safety factors
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