Last reviewed 16 Sept 2026 · 6 min read
The four elastic constants
For a homogeneous, isotropic material loaded within the elastic range, four constants describe how it deforms:
| Constant | Definition | Symbol |
|---|---|---|
| Young's modulus | normal stress ÷ linear strain | |
| Modulus of rigidity (shear modulus) | shear stress ÷ shear strain | or or |
| Bulk modulus | direct stress (equal in all directions) ÷ volumetric strain | |
| Poisson's ratio | lateral strain ÷ linear strain (magnitude) | or |
Only two of them are independent for an isotropic material. Knowing any two, the other two follow from the relations derived below.
- Isotropic material: 2
- Orthotropic material (e.g. timber, laminated composites): 9
- General anisotropic material: 21
Poisson's ratio
When a bar is stretched it becomes longer and thinner. The ratio of the lateral contraction strain to the axial extension strain is constant within the elastic range:
| Material | Typical Poisson's ratio |
|---|---|
| Steel | 0.25 – 0.30 (0.3 commonly used) |
| Aluminium | about 0.33 |
| Cast iron | 0.21 – 0.26 |
| Concrete | 0.15 – 0.20 (IS 456 uses 0.2 for elastic analysis) |
| Rubber | nearly 0.5 |
| Cork | nearly 0 |
| Perfectly plastic material (volume constant) | 0.5 |
Cork has : pushing it into the neck does not make it bulge sideways, so it goes in and stays sealed. Rubber, with , bulges and grips.
Limits of Poisson's ratio
From , since and are positive, → . From , . So theoretically
For ordinary engineering materials . At the material is incompressible (, no volume change).
Strains in three dimensions (generalised Hooke's law)
When normal stresses , , act together (tension positive), each produces its own strain along its direction and lateral contraction in the other two:
Volumetric strain
Volumetric strain is the sum of the three linear strains (for small strains):
- Bar under axial stress :
- Rectangular block:
- Cylindrical rod:
- Sphere:
- Equal stress in all three directions:
Relation between E, K and μ
Apply equal tensile stress on all faces of a cube. Each linear strain is
so . By definition , therefore