III. Strain and Stress

1. III. Strain and Stress • Strain • Stress • Rheology Reading Suppe, Chapter 3 Twiss&Moores, chapter 15

4. Photomicrograph of ooid limestone.  Grainsare 0.5-1 mm in size.  Large grain in center shows well developed concentric calcite layers.

5. Thin section (transmitted light) of deformed oolitic limestone, Swiss Alps. The approximate principal extension (red) and principal shortening directions (yellow) are indicated. The ooids are not perfectly elliptical because the original ooids were not perfectly spherical and because compositional differences led to heterogeneous strain. The elongated ooids define a crude foliation subperpendicular to the principal shortening direction. Photo credit: John Ramsay. http://www.rci.rutgers.edu/~schlisch/structureslides/oolite.html

6. Deformed Ordovian trilobite. Deformed samples such as this provide valuable strain markers.Since we know the shape of an undeformed trilobite of this species, we can compare that to this deformed specimen and quantify the amount and style of strain in the rock.

8. Deformation of a deformable body can be discontinuous (localized on faults) or continuous. • Strain: change of size and shape of a body

9. III. Strain and Stress • Strain • Basics of Continuum Mechanics • Geological examples Additional References : Jean Salençon, Handbook of continuum mechanics: general concepts, thermoelasticity, Springer, 2001 Chandrasekharaiah D.S., Debnath L. (1994) Continuum Mechanics Publisher: Academic press, Inc.

10. Basics of continuum mechanics, Strain • A. Displacements, trajectories, streamlines, emission lines • 1- Lagrangianparametrisation • 2- Eulerianparametrisation • B Homogeneous and tangent Homogeneous transformation • 1- Definition of an homogeneous transformation • 2- Convective transport equation during homogeneous transformation • 3- Tangent homogeneous transformation • C Strain during homogeneous transformation • 1- The Green strain tensor and the Green deformation tensor • Infinitesimal vs finite deformation • 2- Polar factorisation • D Properties of homogeneous transformations • 1- Deformation of line • 2- Deformation of spheres • 3- The strain ellipse • 4- The Mohr circle • E Infinitesimal deformation • 1- Definition • 2- The infinitesimal strain tensor • 3- Polar factorisation • 4- The Mohr circle • F Progressive, finite, and infinitesimal deformation : • 1- Rotational/non rotational deformation • 2- Coaxial Deformation • G Case examples • 1- Uniaxial strain • 2- Pure shear, • 3- Simple shear • 4- Uniform dilatational strain

11. A. Describing the transformation of a body • Reference frame (coordinate system): R • Reference state (initial configuration): k0 • State of the medium at time t: kt • Position (at time t), particle path (=trajectory) • Displacement (from t0 to t), • Velocity (at time t) • Strain (changes in length, angle, volume)

12. A.1 Lagrangian parametrisation • Displacements • Trajectories • Velocites

13. A.1 Lagrangianparametrisation • Volume Change

14. A.2 Eulerian parametrisation • Trajectories: • Streamlines: (at time t)

15. A.3 Stationary Velocity Field • Velocity is independent of time NB: If the motion is stationary in the chosen reference frame then trajectories=streamlines

16. B. Homogeneous Tansformation • definition

17. Homogeneous Transformation • Convective transport of a vector Implication: Straight lines remain straight during deformation

18. Homogeneous transformation • Convective transport of a volume

19. Tangent Homogeneous Deformation • Any transformation can be approximated locally by its tangent homogeneous transformation

20. Tangent Homogeneous Deformation • Any transformation can be approximated locally by its tangent homogeneous transformation

21. Tangent Homogeneous Deformation • Displacement field

22. D. Strain during homogeneous Deformation • The Cauchy strain tensor (or expansion tensor)

23. Strain during homogeneous Deformation • Elongation (or stretch) in the direction of a vector V : • Extension (or extension ratio), relative length change in the direction of a vector V:

24. Strain during homogeneous Deformation • Shear characterizes the change of angle between 2 initially orthogonal vectors • Shear angle ψ : • Beware of confusing terminology: • Shear angle (angular shear strain): ψ • Engineering shear strain: γ=tan(ψ) • Tensor shear strain: tan(ψ)/2

25. Strain during homogeneous Deformation • Signification of the strain tensor components

26. Strain during homogeneous Deformation Cauchy strain tensor: Elongation along ei: Note that it is symmetrical Shear of (ei, ej) An orthometric reference frame can be found in which the strain tensor is diagonal. The SVD yields the 3 principal axes of the strain tensor. In which the Cauchy strain tensor simplifies to: Principal quadratic elongations (streches): λi2Principal elongations (stretch): λi Jacobian:

27. Strain during homogeneous Deformation • The Green-Lagrange strain tensor (strain tensor)

28. Strain during homogeneous Deformation • The Green-Lagrange strain tensor

29. Strain during homogeneous Deformation • Rigid Body Transformation

30. Strain during homogeneous Deformation • Rigid Body Transformation

31. Strain during homogeneous Deformation • Polar factorisation

32. Strain during homogeneous Deformation • Polar factorisation

33. Strain during homogeneous Deformation • Polar factorisation

34. Strain during homogeneous Deformation • Pure deformation: The principal strain axes remain parallel to themselves during deformation

35. D. Some properties of homogeneous Deformation

36. Some properties of homogeneous Deformation • The strain tensor is uniquely characterized by the strain ellipsoid (the deformed state of a sphere with unit radius in the initial configuration)

37. Some properties of homogeneous Deformation • The strain tensor associated to an homogeneous transformation does not define uniquely the transformation (the translation and the rotation terms remain undetermined)

38. Homogeneous Transformation x= R S X + c c x1=S X x2=R x1 x= x2+c

39. Classification of strain The Flinn diagram characterizes the ellipticity of strain (for constant volume deformation: with

40. E. Infinitesimal transformation

41. E. Infinitesimal transformation Infinitesimal strain tensor

42. Infinitesimal transformation

43. Relation between the infinitesimal strain tensor and displacement gradient

44. The strain ellipse NB: The representation of principal extensions on this diagram is correct only for infinitesimal strain only

45. Relation between the infinitesimal strain tensor and displacement gradient

46. F. Finite, infinitesimal and progressive deformation • Finite deformation is said to be non-rotational if the principle strain axis in the initial and final configurations are parallel. This characterizes only how the final state relates to the initial state • Finite deformation of a body is the result of a deformation path (progressive deformation). • There is an infinity of possible deformation paths to reach a particular finite strain. • Generally, infinitesimal strain (or equivalently the strain rate tensor) is used to describe incremental deformation of a body that has experienced some finite strain • A progressive deformation is said to be coaxial if the principal axis of the infinitesimal strain tensor remain parallel to the principal axis of the finite strain tensor. It characterizes the progressive deformation.

47. Rotational vs non-rotational deformation If A and B are parallel to a and b respectively the deformation is said to be non-rotational (This means R= 1)

48. Non-rotational transformation A a B b (a//A and b//B) x= S X + c

49. Non-rotational non-coaxial progressive transformation a Stage 1: b A Stage 2: B

50. Uniaxial strain NB: Uniaxial strain is a type a non-rotational deformation (pure strain)