Upload
alexjos1
View
223
Download
0
Embed Size (px)
Citation preview
7/23/2019 Lecture 4 - Cam Clay
1/43
Critical-State Soil Models
Department of Civil and Envir. Eng., Rensselaer Polytechnic Institute, Troy, NY
April, 2014
7/23/2019 Lecture 4 - Cam Clay
2/43
Critical-State Soil Mechanics
Developed by Roscoeand others at Cambridge inthe fifties
Some Useful Literature:
Schofield, A., & Wroth, P. (1968). Critical state soil mechanics.
Wood, D. (1990). Soil behaviour and critical state soil mechanics.Cambridge University Press.
Helwany, S. (2007).Applied soil mechanics with ABAQUS applications.John Wiley & Sons.
Is an effective stress framework for describing soilresponse
7/23/2019 Lecture 4 - Cam Clay
3/43
Critical-State Soil Mechanics
Critical State models tie together:
1. Behavior of confining pressure (p)2. Behavior of deviatoric stress (q)
3. Behavior of volume changes (e)
Introduce concept of critical state of soils:
State at which shear strains occur without furtherchanges in confining stress, deviatoric stress orvolume.
7/23/2019 Lecture 4 - Cam Clay
4/43
Critical-State Models Some Critical State Soil Models:
Granta Gravel
Cam Clay Modified Cam Clay
7/23/2019 Lecture 4 - Cam Clay
5/43
Prevosts Multi-surface Modified Cam-Clay
Prevosts Multi-surface Modified Cam-Clay
Kinematic hardening Isotropic hardening
Multiple yield surfaces Yield surface and Critical Statesurface
Yield surfaces not capped Capped yield surfaces
Yield surface size independent of e Dependency on e
Ignores OCR Accounts for OCR effect
7/23/2019 Lecture 4 - Cam Clay
6/43
Kinematic Hardening
xz
xyxy
xz
xy
7/23/2019 Lecture 4 - Cam Clay
7/43
Isotropic Hardening
b
a
7/23/2019 Lecture 4 - Cam Clay
8/43
Isotropic Hardening
7/23/2019 Lecture 4 - Cam Clay
9/43
Normal Consolidation Line and
UnloadingReloading Lines
7/23/2019 Lecture 4 - Cam Clay
10/43
Normal Consolidation Line and
UnloadingReloading Lines
7/23/2019 Lecture 4 - Cam Clay
11/43
Normal Consolidation Line and
UnloadingReloading Lines
7/23/2019 Lecture 4 - Cam Clay
12/43
Critical-State
Critical state: State at
which shear stress
application leads tono volume change as
the soil is continually
sheared.
7/23/2019 Lecture 4 - Cam Clay
13/43
Critical-State
p (kPa)
CSL M
7/23/2019 Lecture 4 - Cam Clay
14/43
Critical-State Line
Elastic Yielding
7/23/2019 Lecture 4 - Cam Clay
15/43
Critical-State Line in e-p-q space
3D Figure
7/23/2019 Lecture 4 - Cam Clay
16/43
Parameters for formulation
or
7/23/2019 Lecture 4 - Cam Clay
17/43
Parameters for formulation
7/23/2019 Lecture 4 - Cam Clay
18/43
Inside the field surface (Elastic state)
Elastic but
NOT linear
7/23/2019 Lecture 4 - Cam Clay
19/43
Soil Plasticity
Flow Rule: Describes the direction of the
vector of plastic strain increment
Hardening Law: Relates the magnitude of a
plastic strain to the magnitude of an
increment of stress as the stress traverses the
yield surface and the material hardens
7/23/2019 Lecture 4 - Cam Clay
20/43
Yield Surface
Yield Surface: Separates states of stress which cause only elastic
strains from states of stress that cause plastic (and elastic) strains
Preconsolidation Pressure
7/23/2019 Lecture 4 - Cam Clay
21/43
Plastic Strains
Definitions:
des:Deviatoric Elastic strain increment
dp
s:Deviatoric Plastic strain incrementds= d
es+ dps
dev:Volumetric Elastic strain incrementdpv: Volumetric Plastic strain increment
dv= dev+ d
pv
0
7/23/2019 Lecture 4 - Cam Clay
22/43
Volumetric Strains
Derived from isotropicconsolidation test:
also:
Differentiating:
Elastic Volumetric
Strains Plastic VolumetricStrains
Total Volumetric Strains
7/23/2019 Lecture 4 - Cam Clay
23/43
Deviatoric Plastic Strains Cam Clay Model assumes an associatedflow rule
controlled by the shape of the yield surface:
Stress increment has same direction as strain increment
These increments are perpendicular to the yield surface
(normality rule)
7/23/2019 Lecture 4 - Cam Clay
24/43
Deviatoric Plastic Strains
Yield surface:
Using:
Differentiating (dq/dp), we find normalof the yield surface (-dp/dq):
2 2
2
M
7/23/2019 Lecture 4 - Cam Clay
25/43
Deviatoric Plastic Strains
Normal of theyield surface
2 2
2PS Vd d
M
/P P
S S Vd d d dp dq
7/23/2019 Lecture 4 - Cam Clay
26/43
Plastic Strains (General)
d
7/23/2019 Lecture 4 - Cam Clay
27/43
Summary
Volumetric Strains:
Deviatoric Strains:
7/23/2019 Lecture 4 - Cam Clay
28/43
Critical-State Soil Models
Department of Civil and Envir. Eng., Rensselaer Polytechnic Institute, Troy, NY
April, 2014
7/23/2019 Lecture 4 - Cam Clay
29/43
Summary
p
(kPa)
CSL
M
7/23/2019 Lecture 4 - Cam Clay
30/43
Summary
7/23/2019 Lecture 4 - Cam Clay
31/43
Yield Surface
Yield Surface: Separates states of stress which cause only elastic
strains from states of stress that cause plastic (and elastic) strains
Preconsolidation Pressure
7/23/2019 Lecture 4 - Cam Clay
32/43
Summary
Volumetric Strains:
Deviatoric Strains:
G l F l i
7/23/2019 Lecture 4 - Cam Clay
33/43
General FormulationBorja, R. I., & Lee, S. R. (1990). Cam-clay plasticity, part I:
implicit integration of elasto-plastic constitutive relations.
Computer Methods in Applied Mechanics and
Engineering, 78(1), 49-72
G l F l i
7/23/2019 Lecture 4 - Cam Clay
34/43
General Formulation
7/23/2019 Lecture 4 - Cam Clay
35/43
Hardening Behavior
7/23/2019 Lecture 4 - Cam Clay
36/43
Hardening Behaviorq
P
e
Critical State
Line
State Boundary
Surface
NormalConsolidation
Line
7/23/2019 Lecture 4 - Cam Clay
37/43
Hardening Behaviorq
P
e
Critical State
Line
State Boundary
Surface
NormalConsolidation
Line
7/23/2019 Lecture 4 - Cam Clay
38/43
Softening Behavior
S f i B h i
7/23/2019 Lecture 4 - Cam Clay
39/43
Softening Behavior
q
P
e
Critical State
Line
State Boundary
Surface
NormalConsolidation
Line
7/23/2019 Lecture 4 - Cam Clay
40/43
Softening Behaviorq
P
e
Critical State
Line
State Boundary
Surface
NormalConsolidation
Line
NCL
CSL
e
P
d d l
7/23/2019 Lecture 4 - Cam Clay
41/43
Extended Cam Clay
d d C Cl
7/23/2019 Lecture 4 - Cam Clay
42/43
Extended Cam Clay
7/23/2019 Lecture 4 - Cam Clay
43/43
Effect of shape of Yield Function