Part 3 · Kinematics
3.6 Strain measures
Source: Favata’s notes, Kinematics §1.6, p. 12–13 (spectral form of C, right stretch tensor); the polar decomposition and the Green–Lagrange strain are beyond the notes so far
Objectives
- Find the three fibres through a point that are stretched the most and the least, and stay orthogonal.
- Split any deformation gradient into a pure stretch followed by a rotation.
- Recipe: , , .
- Pictures: the principal directions and their images; played as stretch, then turn.
- Theorem: the polar decomposition.
- Vocabulary: principal stretch, principal direction, right stretch tensor, polar decomposition, Green–Lagrange strain.
Principal directions
is symmetric and positive definite (Theorem 3.3.3). The spectral theorem and Theorem 2.7.9 give with an orthonormal basis of eigenvectors of .
Here the are the eigenvalues of , not stretches. The stretches are their square roots.
The fibre along has stretch : the principal stretch. is the principal direction.
- : through every point there are three orthogonal fibres that are still orthogonal after the deformation. They are the axes of the ellipsoid that a small sphere becomes.
- For any fibre , , a weighted average of the . The largest and smallest stretches at a point are along principal directions.
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The right stretch tensor
is the square root of : symmetric, positive definite, and the only such tensor whose square is (Gurtin). The notes call its properties obvious; they are proved in Positive definite tensors and square roots.
- stretches each principal direction by and does not turn it: three extensions along three orthogonal directions, nothing rigid.
- It changes lengths exactly as does: .
- So and can differ only by something that keeps lengths: a rotation.
Examples: for a stretch along the axes, ; for a rigid deformation, .
The notes break off here; what follows is the standard continuation (Gurtin), in the notes’ notation.
Polar decomposition
Every with is uniquely
Proofbeyond the notes
- is orthogonal: , using .
- It is a rotation: .
- Unique: if with orthogonal and symmetric positive definite, then , so by uniqueness of the square root, and then .
Locally, every deformation is a pure stretch along the principal directions (), followed by a rotation (). The rigid information that discards is exactly .
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The same split in the other order: , with the left stretch tensor and the left Cauchy–Green tensor : turn first, then stretch along the turned directions . and are tensors on the current configuration.
Green–Lagrange strain
- The second form: .
- exactly for rigid deformations (Key observation 3.5.7): what a strain measure should do.
- Length change: .
- For small , dropping leaves , the infinitesimal strain (Definition 2.3.1); its skew partner is the infinitesimal rotation.
The notes print “strain gradient” on p. 12; they mean the deformation gradient.
Exercises
For the stretch along the axes of Exercise 3.5.3, find the principal stretches and directions, and .
Solution
is already in spectral form: , principal stretches . , so : no rotation.
For the plane simple shear with , , find the principal stretches.
Solution
, , . gives and . Principal stretches and : their product is , as it must be for an isochoric deformation. The direction of stretch solves : , so .
Show that and have the same determinant, and that has the same eigenvalues as .
Solution
. ; by Exercise 2.7.3 it has the eigenvalues of , with eigenvectors .