FKM Kompass
L2

Mechanical deformation: elasticity and plasticity

A stressed material first deforms elastically, recovering its original shape completely once the stress is removed, but past a material-specific yield point it deforms plastically instead, undergoing a permanent shape change driven at the microscopic level by the irreversible motion of dislocations through the crystal lattice, and continued deformation eventually leads to fracture.

Practise this concept

When a material is subjected to mechanical stress, it deforms — changes shape — and how it responds falls into two qualitatively different regimes separated by a material-specific threshold called the yield point. Below the yield point, deformation is elastic: the material's atoms are displaced slightly from their equilibrium positions, storing energy in stretched or compressed interatomic bonds, and removing the stress lets those bonds pull the atoms back to their original positions, restoring the material's original shape completely. Elastic deformation is reversible and, for many materials over a useful range, approximately proportional to the applied stress (Hooke's law) — this is the regime that springs, structural beams under normal loads, and most everyday mechanical components are designed to operate within.

Beyond the yield point, deformation becomes plastic: some of the atomic displacement becomes permanent, and removing the stress no longer restores the original shape. In crystalline materials such as metals, plastic deformation occurs overwhelmingly through the motion of dislocations — line defects in the otherwise regular crystal lattice, where a plane of atoms is partially inserted or offset relative to its neighbours. A dislocation can move through the crystal by breaking and reforming just one row of atomic bonds at a time, letting one plane of atoms slip past an adjacent plane at a much lower stress than would be needed to break every bond across an entire plane simultaneously, which is why real crystals deform plastically far more easily than a perfect, defect-free crystal would. This dislocation-mediated mechanism also explains work hardening: as a metal is plastically deformed, dislocations multiply and increasingly obstruct each other's motion, making further plastic deformation progressively harder — exactly why repeatedly bending a metal wire makes it stiffer and eventually brittle at the bend.

Pushed further still, beyond the material's capacity for plastic deformation, the material fractures — bonds break irreversibly and the material separates into pieces. The yield point and the fracture point are therefore two distinct thresholds along the same loading process, not the same event: a ductile material such as most metals shows substantial plastic deformation between yielding and fracture, absorbing considerable energy and giving visible warning (necking, bending) before breaking, while a brittle material such as ceramic or glass fractures with little or no plastic deformation once its (typically lower) fracture stress is reached, offering little warning before failure.

Key ideas

Requires: Structure and properties

Common misconceptions

  • A material that has been stretched always returns exactly to its original shape once the stress is removed.
  • Plastic deformation in a crystalline solid occurs by every atom in the crystal moving simultaneously past its neighbours.
  • The yield point and the fracture point of a material are the same thing.

Resources

Part of these UT courses

This concept is mapped as covering part of the following course(s) in the University of Tartu curriculum.