What Is Strain? Deformation & Hooke's Law
Strain turns deformation into a material property — independent of how long or thick the specimen is.
Stretch a rubber band and it gets longer. Stretch a steel rod by the same force and the change is almost too small to see. But if you measure the *fractional* change in length — the elongation divided by the original length — you get a number that describes the material itself, not the size of the bar. That fractional change is strain, and it is the bridge between stress and deformation.
Normal strain: the fractional change in length
When you pull on a bar, it lengthens. The absolute elongation ΔL depends on the original length — a 2 m bar stretches twice as much as a 1 m bar under the same strain. To remove that size dependence, engineers use normal strain:
Shear strain: the change in angle
Shear stress does not change the length of a material element; it distorts its shape. Imagine a square element becoming a rhombus: the angle between two originally perpendicular edges changes by a small amount γ. That angle change, in radians, is the shear strain.
Hooke's law does not say 'the bar stretches by 2 mm.' It says 'at every point in the bar, the stress is 200 times the strain.' That local relationship is what makes it powerful: you can integrate it over a complex shape, apply it to a tiny finite element, or use it in a simple hand calculation. But it is only valid in the elastic range — once the material yields or cracks, the linear relationship breaks down.
- Normal stress: σ = P/A = 50 000 N / 250 mm² = 200 MPa.
- Elastic strain: ε = σ/E = 200 MPa / 200 000 MPa = 0.001 = 1000 × 10⁻⁶.
- Elongation: ΔL = ε × L = 0.001 × 2000 mm = 2.0 mm.
- Shear modulus: G = E / [2(1+ν)] = 200 000 / [2(1.3)] = 200 000 / 2.6 = 76 923 MPa ≈ 76.9 GPa.
- Sanity check: the elongation is small (0.1% of the length), consistent with elastic deformation of steel.
- ε = ΔL / L = 0.75 mm / 1500 mm = 0.0005 = 500 × 10⁻⁶.
- ε = σ / E = 120 / 200 000 = 0.0006 = 600 × 10⁻⁶.
Check your understanding
- Normal strain ε = ΔL/L is a dimensionless measure of elongation.
- Shear strain γ is the angle change (radians) caused by shear stress.
- Hooke's law: σ = Eε and τ = Gγ, valid only in the elastic range.
- For isotropic materials, G = E / [2(1+ν)].
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