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Video Lecture for MCA 
By: 
video.edhole.com
Non-Linear Hyperbolic Model & 
Parameter Selection 
Short Course on Computational Geotechnics + Dynamics 
Boulder, Colorado 
January 5-8, 2004 
Stein Sture 
Professor of Civil Engineering 
University of Colorado at Boulder 
video.edhole.com
Contents 
Introduction 
Stiffness Modulus 
Triaxial Data 
Plasticity 
HS-Cap-Model 
Simulation of Oedometer and Triaxial Tests on 
Loose and Dense Sands 
Summary 
Computational Geotechnics Non-Linear Hyperbolic Model video.edhole.com & Parameter Selection
Introduction 
Hardening Soils 
Most soils behave in a nonlinear behavior soon after application of 
shear stress. Elastic-plastic hardening is a common technique, also 
used in PLAXIS. 
Usage of the Soft Soil model with creep 
Creep is usually of greater significance in soft soils. 
   
Rf = 
qf 
qa 
   
Eur=3E50 
Hyperbolic stress strain response curve of Hardening Soil model 
Computational Geotechnics Non-Linear Hyperbolic Model video.edhole.com & Parameter Selection
Stiffness Modulus 
Elastic unloading and reloading (Ohde, 1939) 
We use the two elastic parameters nur and Eur 
Definition of E50 in a standard drained triaxial experiment 
   
æ  
è  
ref ccotj -s3 
æ  
è  
ref s3 
ç  
E50 =E50 
m 
' +ccotj 
pref +ccotj 
ç  
m 
ö  
÷  
ø  
æ  
è  
ref s3 
=E50 
' sinj +ccosj 
pref sinj +ccosj 
ç  
ö  
ø  
m 
÷  
   
Eur 
' 
ccotj + pref 
ö  
÷  
ø  
Gur = 1 
2(1+n) 
Eur 
   
pref=100kPa 
Initial (primary) loading 
Computational Geotechnics Non-Linear Hyperbolic Model video.edhole.com & Parameter Selection
Stiffness Modulus 
Definition of the normalized oedometric stiffness 
Values for m from oedometer test versus initial porosity n0 
Normalized oedometer modulus versus initial porosity n0 
Oedometer tests 
   
ref 
Eoed 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Stiffness Modulus 
Normalized oedometric stiffness for various soil classed (von Soos, 1991) 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Stiffness Modulus 
Values for m obtained from triaxial test versus initial porosity n0 
Normalized triaxial modulus versus initial porosity n0 
   
ref 
E50 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Stiffness Modulus 
Summary of data for sand: Vermeer & Schanz (1997) 
Comparison of normalized stiffness moduli from oedometer and 
Triaxial test 
   
ref s y 
Eoed = Eoed 
' 
pref 
ref s x 
E50 = E50 
' 
pref 
Engineering practice: mostly data on Eoed 
Test data: 
   
ref »E50 
Eoed 
ref 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Triaxial Data on gp » 2e1 
p 
Equi-g lines (Tatsuoka, 1972) for dense Toyoura Sand 
Yield and failure surfaces for the Hardening Soil model 
   
= qa 
E50 
2e1 
q 
qa-q 
   
æ  
è  
ref s3 
E50=E50 
m 
' sinj+ccosj 
pref sinj+ccosj 
ç  
ö  
÷  
ø  
   
qf 
qa= 
Rf 
-1 
=M(p+ccotj)Rf 
   
M= 6sinj 
3-sinj 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Plasticity 
Yield and hardening functions 
   
gp =e1 
p-e2 
p-e3 
p »2e1 
p =2e1 
e = qa 
-2e1 
E50 
q 
qa-q 
-2q 
Eur 
f = qa 
E50 
q 
qa-q 
-2q 
Eur 
-gp =0 
3D extension 
In order to extent the model to general 3D states in terms of stress, we use 
a modified expression for in terms of and the mobilized angle of 
internal friction 
    
q 
    
q˜ 
   
jm 
˜ q =s1'+(a-1)s2 
3 
'-a' 
sa=3+sinjm 
3-sinjm 
˜ = 6sinjm 
f=q˜ -M˜ (p+ccotj) 
M3-sinjm 
where 
Compvutiadtioenaol Gseo.teechdnichs ole.com Non-Linear Hyperbolic Model & Parameter Selection
Plasticity 
   
q* 
=s1 
'+(b-1)s2 
3 
'-b' 
s   
b=3+sinym 
3-sinym 
   
g=-m 
y(p+ccot) 
* M* 
q   
M*= 6sinym 
3-sinym 
Plastic potential and flow rule 
with 
   
ê  
ê  
ê  
ê  
ê  
· 
= 
ep 
· 
e1 
p 
· 
ú  
ú  
ú  
ú  
ú  
e2 
p 
· 
e3 
p 
é  
ë  
ù  
=L · 
û  
¶g 
¶s12 
12 
+L · 
¶g 
¶s13 
13 
=L · 
ê  
ê  
ê  
12 
1 
2-1 
2siny 
-1 
ú  
ú  
ú  
+L · 
2-1 
2siny 
0 
é  
ë  
ù  
û  
ê  
ê  
ê  
13 
1 
2-1 
2siny 
0 
-1 
ú  
ú  
ú  
2-1 
2siny 
é  
ë  
ù  
û  
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Plasticity 
Flow rule 
with 
· 
· =sinym 
· 
=sinygp 
=sinjm 
C [kPa] j’ [o] y [o] E50 [Mpa] 
0 30-40 0-10 40 
Eur = 3 E50 Vur = 0.2 Rf = 0.9 m = 0.5 Pref = 100 kPa 
   
ev 
p 
gp 
Þp 
v 
e· 
   
sinym 
-sinjcv 
1-sinjm 
sinjcv 
   
jcv=jp 
-yp 
Primary soil parameters and standard PLAXIS settings 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Plasticity 
Hardening soil response in drained triaxial experiments 
Results of drained loading: 
stress-strain relation (s3 = 100 kPa) 
Results of drained loading: 
axial-volumetric strain relation (s3 = 100 kPa) 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Plasticity 
   
Undrained hardening soil analysis 
Method A: switch to drained 
Input: 
c';j';y' 
Eref 
50 
ì  
í  
ï  
ï  
î  
nur=0.2;Eur=3E50;m=0.5;pref =100kPa 
   
Method B: switch to undrained 
Input: 
cu;ju 
;y 
ref 
E50 
ì  
í  
ï  
îï   
nur=0.2;Eur=3E50;m=0.5;pref =100kPa 
Compvutiadtioenaol Gseo.teechdnichs ole.com Non-Linear Hyperbolic Model & Parameter Selection
Plasticity 
Interesting in case you have data on Cu and not no C’ and f’ 
2cu 
m 
=E50 
m 
=Eur 
Eu » 1.4 E50 
50 =E50 
Eref s3 
' sinju 
+Cucosju 
pref sinju 
+Cucosju 
æ  
ç  
è  
ö  
÷  
ø  
ref =const. 
+Cucosju æ  
è  
ref s3 
Eur =Eur 
' sinju 
+Cucosju 
ç  
pref sinju 
ö  
÷  
ø  
ref =const. 
Assume E50 = 0.7 Eu and use graph by Duncan & Buchignani (1976) to estimate Eu 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Plasticity 
Hardening soil response in undrained triaxial tests 
Results of undrained triaxial loading: 
stress-strain relations (s3 = 100 kPa) 
Results of undrained triaxial loading: p-q 
diagram (s3 = 100 kPa) 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
HS-Cap-Model 
   
fc=q˜ 2 
M2+p2-pc 
2 
gc=fc 
· 
= p · 
ep 
v 
Kc 
- p · 
Ks 
(Associated flow) 
=1 
H 
p · 
   
H= Kc 
Ks-Kc 
Ks 
Cap yield surface 
Flow rule 
Hardening law 
For isotropic compression we assume 
with 
Compvutiadtioenaol Gseo.teechdnichs ole.com Non-Linear Hyperbolic Model & Parameter Selection
HS-Cap-Model 
For isotropic compression we have q = 0 and it follows from 
   
p · 
=p · 
¶g 
¶pc 
· 
=HL · 
For the determination of, we have another consistency condition: 
c 
   
p · 
v 
=Hep 
cc 
=2HL · 
cp 
   
T 
· 
c=¶fc 
f 
¶s 
+¶fc 
¶pc 
s · 
p · 
c=0 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
HS-Cap-Model 
Additional parameters 
The extra input parameters are K0 (=1-sinf) and Eoed/E50 (=1.0) 
The two auxiliary material parameter M and Kc/Ks are determined 
iteratively from the simulation of an oedometer test. There are no direct 
input parameters. The user should not be too concerned about these 
parameters. 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
HS-Cap-Model 
1 
Graphical presentation of HS-Cap-Model 
I: Purely elastic response 
II: Purely frictional hardening with f 
III: Material failure according to Mohr-Coulomb 
IV: Mohr-Coulomb and cap fc 
V: Combined frictional hardening f and cap fc 
VI: Purely cap hardening with fc 
VII: Isotropic compression 
2 3 
Yield surfaces of the extended HS model in p-q space (left) and in the deviatoric plane (right) 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
HS-Cap-Model 
s1 = s2 = s3 
Yield surfaces of the extended HS model in principal stress space 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Simulation of Oedometer and Triaxial 
Tests on Loose and Dense Sands 
Comparison of calculated () and measured triaxial tests on loose Hostun Sand 
Comparison of calculated () and measured oedometer tests on loose Hostun Sand 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Simulation of Oedometer and Triaxial 
Tests on Loose and Dense Sands 
Comparison of calculated () and measured triaxial tests on dense Hostun Sand 
Comparison of calculated () and measured oedometer tests on dense Hostun Sand 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
Summary 
Main characteristics 
•Pressure dependent stiffness 
•Isotropic shear hardening 
•Ultimate Mohr-Coulomb failure condition 
•Non-associated plastic flow 
•Additional cap hardening 
HS-model versus MC-model 
As in Mohr-Coulomb model 
Normalized primary loading stiffness 
Unloading / reloading Poisson’s ratio 
Normalized unloading / reloading stiffness 
Power in stiffness laws 
Failure ratio 
   
c,j,y 
   
ref 
E50 
   
nur 
   
ref 
Eur 
   
m 
Rf 
Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection

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Video lecture for mca ! Edhole

  • 1. Video Lecture for MCA By: video.edhole.com
  • 2. Non-Linear Hyperbolic Model & Parameter Selection Short Course on Computational Geotechnics + Dynamics Boulder, Colorado January 5-8, 2004 Stein Sture Professor of Civil Engineering University of Colorado at Boulder video.edhole.com
  • 3. Contents Introduction Stiffness Modulus Triaxial Data Plasticity HS-Cap-Model Simulation of Oedometer and Triaxial Tests on Loose and Dense Sands Summary Computational Geotechnics Non-Linear Hyperbolic Model video.edhole.com & Parameter Selection
  • 4. Introduction Hardening Soils Most soils behave in a nonlinear behavior soon after application of shear stress. Elastic-plastic hardening is a common technique, also used in PLAXIS. Usage of the Soft Soil model with creep Creep is usually of greater significance in soft soils.   Rf = qf qa   Eur=3E50 Hyperbolic stress strain response curve of Hardening Soil model Computational Geotechnics Non-Linear Hyperbolic Model video.edhole.com & Parameter Selection
  • 5. Stiffness Modulus Elastic unloading and reloading (Ohde, 1939) We use the two elastic parameters nur and Eur Definition of E50 in a standard drained triaxial experiment   æ è ref ccotj -s3 æ è ref s3 ç E50 =E50 m ' +ccotj pref +ccotj ç m ö ÷ ø æ è ref s3 =E50 ' sinj +ccosj pref sinj +ccosj ç ö ø m ÷   Eur ' ccotj + pref ö ÷ ø Gur = 1 2(1+n) Eur   pref=100kPa Initial (primary) loading Computational Geotechnics Non-Linear Hyperbolic Model video.edhole.com & Parameter Selection
  • 6. Stiffness Modulus Definition of the normalized oedometric stiffness Values for m from oedometer test versus initial porosity n0 Normalized oedometer modulus versus initial porosity n0 Oedometer tests   ref Eoed Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 7. Stiffness Modulus Normalized oedometric stiffness for various soil classed (von Soos, 1991) Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 8. Stiffness Modulus Values for m obtained from triaxial test versus initial porosity n0 Normalized triaxial modulus versus initial porosity n0   ref E50 Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 9. Stiffness Modulus Summary of data for sand: Vermeer & Schanz (1997) Comparison of normalized stiffness moduli from oedometer and Triaxial test   ref s y Eoed = Eoed ' pref ref s x E50 = E50 ' pref Engineering practice: mostly data on Eoed Test data:   ref »E50 Eoed ref Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 10. Triaxial Data on gp » 2e1 p Equi-g lines (Tatsuoka, 1972) for dense Toyoura Sand Yield and failure surfaces for the Hardening Soil model   = qa E50 2e1 q qa-q   æ è ref s3 E50=E50 m ' sinj+ccosj pref sinj+ccosj ç ö ÷ ø   qf qa= Rf -1 =M(p+ccotj)Rf   M= 6sinj 3-sinj Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 11. Plasticity Yield and hardening functions   gp =e1 p-e2 p-e3 p »2e1 p =2e1 e = qa -2e1 E50 q qa-q -2q Eur f = qa E50 q qa-q -2q Eur -gp =0 3D extension In order to extent the model to general 3D states in terms of stress, we use a modified expression for in terms of and the mobilized angle of internal friction   q   q˜   jm ˜ q =s1'+(a-1)s2 3 '-a' sa=3+sinjm 3-sinjm ˜ = 6sinjm f=q˜ -M˜ (p+ccotj) M3-sinjm where Compvutiadtioenaol Gseo.teechdnichs ole.com Non-Linear Hyperbolic Model & Parameter Selection
  • 12. Plasticity   q* =s1 '+(b-1)s2 3 '-b' s  b=3+sinym 3-sinym   g=-m y(p+ccot) * M* q  M*= 6sinym 3-sinym Plastic potential and flow rule with   ê ê ê ê ê · = ep · e1 p · ú ú ú ú ú e2 p · e3 p é ë ù =L · û ¶g ¶s12 12 +L · ¶g ¶s13 13 =L · ê ê ê 12 1 2-1 2siny -1 ú ú ú +L · 2-1 2siny 0 é ë ù û ê ê ê 13 1 2-1 2siny 0 -1 ú ú ú 2-1 2siny é ë ù û Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 13. Plasticity Flow rule with · · =sinym · =sinygp =sinjm C [kPa] j’ [o] y [o] E50 [Mpa] 0 30-40 0-10 40 Eur = 3 E50 Vur = 0.2 Rf = 0.9 m = 0.5 Pref = 100 kPa   ev p gp Þp v e·   sinym -sinjcv 1-sinjm sinjcv   jcv=jp -yp Primary soil parameters and standard PLAXIS settings Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 14. Plasticity Hardening soil response in drained triaxial experiments Results of drained loading: stress-strain relation (s3 = 100 kPa) Results of drained loading: axial-volumetric strain relation (s3 = 100 kPa) Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 15. Plasticity   Undrained hardening soil analysis Method A: switch to drained Input: c';j';y' Eref 50 ì í ï ï î nur=0.2;Eur=3E50;m=0.5;pref =100kPa   Method B: switch to undrained Input: cu;ju ;y ref E50 ì í ï îï nur=0.2;Eur=3E50;m=0.5;pref =100kPa Compvutiadtioenaol Gseo.teechdnichs ole.com Non-Linear Hyperbolic Model & Parameter Selection
  • 16. Plasticity Interesting in case you have data on Cu and not no C’ and f’ 2cu m =E50 m =Eur Eu » 1.4 E50 50 =E50 Eref s3 ' sinju +Cucosju pref sinju +Cucosju æ ç è ö ÷ ø ref =const. +Cucosju æ è ref s3 Eur =Eur ' sinju +Cucosju ç pref sinju ö ÷ ø ref =const. Assume E50 = 0.7 Eu and use graph by Duncan & Buchignani (1976) to estimate Eu Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 17. Plasticity Hardening soil response in undrained triaxial tests Results of undrained triaxial loading: stress-strain relations (s3 = 100 kPa) Results of undrained triaxial loading: p-q diagram (s3 = 100 kPa) Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 18. HS-Cap-Model   fc=q˜ 2 M2+p2-pc 2 gc=fc · = p · ep v Kc - p · Ks (Associated flow) =1 H p ·   H= Kc Ks-Kc Ks Cap yield surface Flow rule Hardening law For isotropic compression we assume with Compvutiadtioenaol Gseo.teechdnichs ole.com Non-Linear Hyperbolic Model & Parameter Selection
  • 19. HS-Cap-Model For isotropic compression we have q = 0 and it follows from   p · =p · ¶g ¶pc · =HL · For the determination of, we have another consistency condition: c   p · v =Hep cc =2HL · cp   T · c=¶fc f ¶s +¶fc ¶pc s · p · c=0 Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 20. HS-Cap-Model Additional parameters The extra input parameters are K0 (=1-sinf) and Eoed/E50 (=1.0) The two auxiliary material parameter M and Kc/Ks are determined iteratively from the simulation of an oedometer test. There are no direct input parameters. The user should not be too concerned about these parameters. Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 21. HS-Cap-Model 1 Graphical presentation of HS-Cap-Model I: Purely elastic response II: Purely frictional hardening with f III: Material failure according to Mohr-Coulomb IV: Mohr-Coulomb and cap fc V: Combined frictional hardening f and cap fc VI: Purely cap hardening with fc VII: Isotropic compression 2 3 Yield surfaces of the extended HS model in p-q space (left) and in the deviatoric plane (right) Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 22. HS-Cap-Model s1 = s2 = s3 Yield surfaces of the extended HS model in principal stress space Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 23. Simulation of Oedometer and Triaxial Tests on Loose and Dense Sands Comparison of calculated () and measured triaxial tests on loose Hostun Sand Comparison of calculated () and measured oedometer tests on loose Hostun Sand Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 24. Simulation of Oedometer and Triaxial Tests on Loose and Dense Sands Comparison of calculated () and measured triaxial tests on dense Hostun Sand Comparison of calculated () and measured oedometer tests on dense Hostun Sand Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection
  • 25. Summary Main characteristics •Pressure dependent stiffness •Isotropic shear hardening •Ultimate Mohr-Coulomb failure condition •Non-associated plastic flow •Additional cap hardening HS-model versus MC-model As in Mohr-Coulomb model Normalized primary loading stiffness Unloading / reloading Poisson’s ratio Normalized unloading / reloading stiffness Power in stiffness laws Failure ratio   c,j,y   ref E50   nur   ref Eur   m Rf Computational Geotechnics Non-Linear Hyperbolic Model videos.edhole.com & Parameter Selection