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CMG Research: Mathematical Modeling of the Dynamics of Multi-scale Phenomena During Folding and Fracturing of Sedimentary Rocks Ronaldo I. Borja, Craig.

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Presentation on theme: "CMG Research: Mathematical Modeling of the Dynamics of Multi-scale Phenomena During Folding and Fracturing of Sedimentary Rocks Ronaldo I. Borja, Craig."— Presentation transcript:

1 CMG Research: Mathematical Modeling of the Dynamics of Multi-scale Phenomena During Folding and Fracturing of Sedimentary Rocks Ronaldo I. Borja, Craig D. Foster, and Pablo F. Sanz Department of Civil and Environmental Engineering Stanford University

2 Outline of Presentation
Ronnie’s Presentation (40 minutes): General kinematics of deformation Constitutive model - plasticity and damage models Finite element model Boundary conditions, interface elements Pablo’s Presentation (10 minutes): Three-invariant plasticity models Craig’s Presentation (10 minutes): Element enhancements for strain localization analysis

3 Kinematics of Deformation
Features that must be captured: Folding - change in geometry Fracturing - large strain at crack tip Finite rotation of fracture zone Finite deformation formulations: Lagrangian formulation - appropriate for solids Eulerian formulation - appropriate for fluids Both formulations can handle geometric nonlinearity, large strain, finite rotation, and frame-invariant constitutive models.

4 Lagrangian versus Eulerian Formulations
We follow the motion of a material point Constitutive model applies to a material point Finite element mesh could be severely distorted Re-meshing possible for severely distorted meshes Eulerian: We describe the motion of a fixed point in space Point in space occupied by different material points Finite element mesh will not be distorted ALE (Arbitrary Lagrangian-Eulerian)

5 Lagrangian Formulation
Why this formulation is OK for the CMG project: Constitutive response applies to a material point Accommodates coupled plasticity-damage models We do not expect the mesh to be severely distorted Captures rotation of fracture as rock folds Facilitates specification of boundary conditions Finite element implementation is well developed Finite element implementation: Integration performed over the undeformed mesh Constitutive model uses Kirchhoff or Cauchy stress

6 Illustration of Lagrangian Formulation
Graphics 1

7 Illustration of Lagrangian Formulation

8 Constitutive Model Features to capture: Brittle response
Quasi-brittle response Ductile response Plasticity Damage Localized deformation Framework for continuum model: Coupled elastoplastic-damage formulation One unifying model that captures all required features Framework for post-localized model: Finite element with embedded strong discontinuity


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