Stress and Strain — Core Principles
Core Principles
Stress and strain are fundamental concepts in understanding how solid materials respond to external forces. Stress () is defined as the internal restoring force developed per unit cross-sectional area of a body when it is deformed.
Its SI unit is Pascal ( or ). There are three main types: Normal stress (tensile or compressive, acting perpendicular to the surface), Tangential or Shear stress (acting parallel to the surface), and Volumetric or Hydraulic stress (uniform normal stress causing volume change).
Strain () is the dimensionless measure of deformation, defined as the ratio of the change in dimension to the original dimension. Corresponding to stress types, we have Longitudinal strain (), Shear strain ( or ), and Volumetric strain ().
Materials exhibit elasticity if they regain their original shape after force removal, up to an elastic limit. Beyond this limit, they show plasticity, undergoing permanent deformation. Within the elastic limit, stress is proportional to strain, a relationship known as Hooke's Law.
Important Differences
vs Pressure
| Aspect | This Topic | Pressure |
|---|---|---|
| Definition | Stress: Internal restoring force per unit area within a deformed solid. | Pressure: External normal force per unit area exerted by a fluid or gas. |
| Nature | Stress: Tensor quantity (can be normal or tangential). | Pressure: Scalar quantity (always acts perpendicularly inwards). |
| Origin | Stress: Arises from internal molecular forces resisting deformation. | Pressure: Arises from external forces, typically from fluid collisions with a surface. |
| Effect | Stress: Causes deformation (strain) in solids. | Pressure: Causes compression or expansion, primarily in fluids, but also volumetric changes in solids. |
| Types | Stress: Normal (tensile/compressive), Shear, Volumetric. | Pressure: Hydrostatic pressure, atmospheric pressure, gauge pressure, etc. |