Part 2 · Theory of deformation
2.1 Configurations and the deformation gradient
Source: Carboni’s notes for lesson 2, Teoria della deformazione 1, pp. 1–4
Objectives
- Vocabulary. Reference and current configuration, deformation, displacement, fibre.
- Theorem. Near a point, any deformation acts on fibres as a linear map: .
- Recipe. Compute from the deformation or the displacement , and check that the deformation is admissible.
- Picture. turns a small square into a parallelogram.
The oscillator had one number, , for its deformation. A body has a deformation at every one of its points, and in every direction through each point. This part builds the tools that measure it, without any reference to forces: pure geometry.
The continuum and its configurations
A continuum is a model of a physical body in which its molecular structure is ignored: the body fills a region of space without gaps, and quantities such as displacement, density or internal force are smooth fields defined at every point of that region.
Fix an origin and an orthonormal basis : three unit vectors, mutually perpendicular. (Carboni’s handwriting writes the basis letter like ; the typed sheets write .)
- The reference configuration is the region the body occupies at the start. A point has the position vector
- The current configuration is the region the body occupies at time . The same material point is now at , with the position vector .
A breve () marks everything in the current configuration: , , later , .
The map which sends each material point to where it is at time , is the deformation (or transformation). Followed in time it describes the motion of the body. The displacement is what is added to the starting position:
In components, with is a label: it says which material point we mean. and are vector-valued functions of that label and of time.
In Carboni’s notation the bold is the displacement here, and later (§2.4 Polar decomposition) the same letter is the right stretch tensor of the polar decomposition. The context always says which: the displacement is a vector field , the stretch tensor a symmetric matrix.
What a deformation must satisfy
Not every map describes a real body. The notes ask for three things.
A deformation is admissible if:
- Regularity. Each is continuous, and so are its derivatives for all .
- Bijectivity (impenetrability). At each , is one-to-one and onto: one material point, one position, and back. So the inverse map exists. Two pieces of matter never end up in the same place.
- Positive volume ratio. A small volume around goes to a volume around with
Why the volume ratio is this determinant is proved in §2.5 Change of volume and area. Once is defined below, condition 3 reads simply .
What the sign of means.
- : no neighbourhood is squashed to zero volume, and can be inverted near each point.
- : orientation is kept. A right-handed triad of fibres stays right-handed: a body cannot be turned inside out, which a mirror image would do ().
Try the presets “turned inside out” and “collapsed” in Figure 2.1.1.
The deformation gradient
How does the deformation act near a point? Take a second point close to , at .
The short segment from to a nearby point is a fibre: a small material line through . The deformation takes it to , the segment between the new positions and .
To first order in the length of the fibre,
Proof
- Subtract the images of the two ends:
- Taylor-expand the first term about :
- The terms cancel. The fibre is short, so drop the higher-order terms: .
Component by component, the same steps read that is, as a matrix product,
The matrix , with entries (row : which component of ; column : which coordinate it is differentiated by), is the deformation gradient. It maps each fibre at to its image: .
Near a point, any deformation acts on fibres as a linear map, and is that map. However curved the deformation is on the scale of the body, a small enough neighbourhood sees only : straight fibres stay straight, parallel fibres stay parallel, a small square becomes a parallelogram and a small circle an ellipse.
changes from point to point and in time: it is a tensor field . Studying it at one point is studying the deformation locally.
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That the columns of are the images of the basis vectors is the subject of Stretch vectors in the next section.
L2 p. 3 writes the second term of the difference as , without the ; it is .
The displacement gradient
Often the data is the displacement rather than . Since and (the identity matrix), is the displacement gradient. Lesson 4 introduces it (Definition 2.6.5); it is used here already because it is the quickest way to from a displacement.
- Write the components (or differentiate and add at the end).
- Differentiate: row of holds , , .
- Evaluate at the point.
- Admissible there? Compute and check it is positive.
, at .
- , , .
- Differentiate:
- At :
- : admissible at . The volume around grows 18 times.
Exercises
. Compute , then and at . Is the deformation admissible there? (Exercises for the first partial, bis, Problem 1.)
Solution
: admissible at .
For simple shear, with a number, find , and . What happens to a unit square on ?
Solution
- , , .
- stays put, goes to : the square becomes a parallelogram of the same base and height, so the same area. Layers parallel to slide over each other, like a pack of cards.
Is an admissible deformation? What does it do?
Solution
, : not admissible. It stretches along and reflects across the plane , turning the body inside out, which no real body can do.