Brittle fracture is a sudden and catastrophic mode of failure in materials that occurs without significant plastic deformation. It typically propagates rapidly once initiated, often along specific crystallographic planes, and is considered dangerous in structural applications because it offers no visible warning before failure.
Very little or no plastic deformation before fracture.
Sudden failure—material breaks almost instantaneously once the crack propagates.
Fracture surface is flat, shiny, and granular, often showing cleavage facets.
Crack often propagates perpendicularly to the applied tensile stress.
Fracture occurs along crystallographic planes in a transgranular or intergranular manner.
Brittle fracture generally occurs through one of the following pathways:
1. Crack Initiation
Begins at a stress concentration site such as:
Surface scratches
Notches
Inclusions
Grain boundaries
These flaws intensify local stress, leading to crack nucleation.
2. Crack Propagation
Once a crack is initiated, it propagates very rapidly with minimal energy absorption.
Propagation is typically unstable and follows a cleavage plane—a crystallographic plane of low atomic density.
Atomic bonds break along this plane without significant dislocation movement or plastic flow.
Brittle fracture can occur in two main forms:
a. Transgranular Fracture (Cleavage)
The crack passes through the grains of the material.
Fracture surfaces appear faceted due to separation along specific crystal planes.
Common in BCC and HCP metals, ceramics, and glasses.
b. Intergranular Fracture
The crack propagates along grain boundaries.
Indicates grain boundary weakening due to:
Impurities or segregation
Environmental effects (e.g., corrosion)
Improper heat treatment
Often seen in metals with embrittlement or heat-affected zones in welds.
In a stress-strain curve, brittle fracture is indicated by:
A short elastic region and no noticeable plastic region.
The material fractures at or near the ultimate tensile strength (UTS).
Sharp, vertical drop at fracture point.
Ceramics and glasses (very brittle by nature)
High-strength steels, especially at low temperatures
Cast iron
Hardened metals (e.g., quenched and tempered steels)
Polymers at low temperatures
Low Temperature: Reduces atomic vibration, inhibiting dislocation motion.
High Strain Rates: Rapid loading limits the time for plastic deformation.
Triaxial Stress State: Increases internal stress, especially in thick materials.
Material Condition:
High hardness
Large grain size
Impurities or segregated phases
Notches and Flaws: Act as crack initiation points by concentrating stress.