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Continuum damage mechanics of geomaterials at finite strain A. Karrech, Research Scientist, CSIRO K. Regenauer-Lieb, T. Poulet, P. Schaubs, Y, Zhang 29.

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Presentation on theme: "Continuum damage mechanics of geomaterials at finite strain A. Karrech, Research Scientist, CSIRO K. Regenauer-Lieb, T. Poulet, P. Schaubs, Y, Zhang 29."— Presentation transcript:

1 Continuum damage mechanics of geomaterials at finite strain A. Karrech, Research Scientist, CSIRO K. Regenauer-Lieb, T. Poulet, P. Schaubs, Y, Zhang 29 September 2010 MDU

2 Outline 1 Background Motivation Current approach 2 Elasto-visco-plasticity at finite strain Multiplicative decomposition Constitutive relations 3 Damage mechanism Void growth under several control mechanisms The limit theory approximation 4 Validation / Application Validation of the large transformations model Damage of a notched plate and effects of pressure Chemo-thermo-hydro-mechanics (See Thomas Poulet) Damage down under (See Peter Schaubs) 5 Summary

3 Damage at Finite Strain Instabilities Large transformations to describe earth systems instabilities

4 Damage at Finite Strain Material Softening The predicted forces for splitting continents apart are much higher then available from plate tectonics. Time and length scales can’t be achieved in the laboratory. Regenauer-Lieb et al 06, Nature

5 Outline 1 Background Motivation Current approach 2 Elasto-visco-plasticity at finite strain Multiplicative decomposition Constitutive relations 3 Damage mechanism Void growth under several control mechanisms The limit theory approximation 4 Validation / Application Validation of the large transformations model Damage of a notched plate and effects of pressure Chemo-thermo-hydro-mechanics (See Thomas Poulet) Damage down under (See Peter Schaubs) 5 Summary

6 Finite strain -- Review Additive strain rate decomposition (similar to small deformations): Green Naghdi(65), Mandel (72), Nemat-Nasser (81)... Multiplicative gradient decomposition: Lee and Liu(67), Lee (69) Numerical integration: Simo et al. (80s-94), Argyris and Doltsinis(80s), Miehe(90s) Several inconsistencies (aberrant oscillations observed by Dienes (79) Simo and Pister (82), K. Regenauer-Lieb and H. Mulhaus (06)…) Logarithmic corotational rates: Xiao, Buhrns Meyers (98-06) Metallic materials: Lin, Brocks, Betten (02,04,06) Formulation + numerical integration for geomaterials: current work

7 Finite strain – Basic concept Small perturbations: (+) Well understood + Easy integration (-) Limitations in predicting instabilities Large transformations:

8 Finite strain – Oscillations Source of the figure: www.wikepidia.com How to formulate thermo- mechanical coupled models for frictional materials in finite strain How to overcome these spurious oscillations?

9 Decomposition The deformation gradient is: Hence, the multiplicative decomposition: We consider the measure of athermal strain:

10 Objective rates

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12 Dissipation inequality

13 Helmholtz F. E. and dissipation

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15 Principle of maximum dissipation

16 Outline 1 Background Motivation Current approach 2 Elasto-visco-plasticity at finite strain Multiplicative decomposition Constitutive relations 3 Damage mechanism Void growth under several control mechanisms The limit theory approximation 4 Validation / Application Validation of the large transformations model Damage of a notched plate and effects of pressure Chemo-thermo-hydro-mechanics (See Thomas Poulet) Damage down under (See Peter Schaubs) 5 Summary

17 Micro-scale model A. C. F. Cocks and M. F. Ashby, progress in materials science, 1982, Vol. 27, pp. 189 to 244

18 Comparison with other damage models For small f, Cocks and Ashby models coincide with the descriptions of Kachanov (58) and Lemaitre and chaboche (80s) The comparison highlights what we believe to be certain fundamental weaknesses of the continuum equations: first, the prediction that the damage-rate is finite even when there is no damage; second, the prediction that the damage-rate always accelerates with damage;

19 Current approach Assumptions: Vacancies within a given RVE are assumed to be within a spacing of min(2d, 2L), (d and L are distances in the longitudinal and radial directions) Voids are assumed to be of small size as compared to the Voids are self-similar in terms of shape during the deformation process. Upper limit (MARTIN, JMPS, 62)

20 Current approach After Integration (Karrech el al., ICAMEM Conference 2010) Similarly to Dahar et al (1996), we add a nucleation effect (no justification yet) Integration with respect to the thermodynamic force of damage:

21 Outline 1 Background Motivation Current approach 2 Elasto-visco-plasticity at finite strain Multiplicative decomposition Constitutive relations 3 Damage mechanism Void growth under several control mechanisms The limit theory approximation 4 Validation / Application Validation of the large transformations model Damage of a notched plate and effects of pressure Chemo-thermo-hydro-mechanics (See Thomas Poulet) Damage down under (See Peter Schaubs) 5 Summary

22 Axially loaded sample

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24 Simple Shear

25 Simple Shear in hyer-elasto-plasticity

26 Necking problem Good agreement between the experimental and numerical results

27 Triaxial test

28 Damage of a notched plate (Olivine)

29 Effect of pressure dependency

30 Courtesy of Arcady Dyskin, UWA

31 Outline 1 Background Motivation Current approach 2 Elasto-visco-plasticity at finite strain Multiplicative decomposition Constitutive relations 3 Damage mechanism Void growth under several control mechanisms The limit theory approximation 4 Validation / Application Validation of the large transformations model Damage of a notched plate and effects of pressure Chemo-thermo-hydro-mechanics (See Thomas Poulet) Damage down under (See Peter Schaubs) 5 Summary

32 Chemo-thermo-hydro-mechanics

33 Permeability evolution with damage

34 Chemo-thermo-hydro-mechanics Fluid flow through damaged zones Preliminary chemistry

35 Invitation I invite you to talk to Thomas Poulet for more details about multi- physics Problems

36 Outline 1 Background Motivation Current approach 2 Elasto-visco-plasticity at finite strain Multiplicative decomposition Constitutive relations 3 Damage mechanism Void growth under several control mechanisms The limit theory approximation 4 Validation / Application Validation of the large transformations model Damage of a notched plate and effects of pressure Chemo-thermo-hydro-mechanics (See Thomas Poulet) Damage down under (See Peter Schaubs) 5 Summary

37 Damage & thermo-coupling The Late Archaean Yilgarn Craton of Western Australia hosting orogenic gold deposits Different loading scenarios

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40 Invitation I invite you to talk to Peter Schaubs for more details about the field application

41 Outline 1 Background Motivation Current approach 2 Elasto-visco-plasticity at finite strain Multiplicative decomposition Constitutive relations 3 Damage mechanism Void growth under several control mechanisms The limit theory approximation 4 Validation / Application Validation of the large transformations model Damage of a notched plate and effects of pressure Chemo-thermo-hydro-mechanics (See Thomas Poulet) Damage down under (See Peter Schaubs) 5 Conclusions

42 Outline Finite strain for geo-materials based on logarithmic strain measures and corotational rates. Solution for the spurious oscillations Continuum damage mechanics following based on approximate potential Instabilities and localizations are accelerated in such circumstances Multi-physics problems in the context of mining

43 Thank you Computational Geoscience Group Dr Ali Karrech Research Scientist @ CSIRO Adjunct Associate Professor @ UWA Phone: +61 8 64 36 86 96 Email: ali.karrech@csiro.au Web: www.csiro.au


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