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Brittleness

physical science Maturity 11-13 Next article →

Brittleness describes how certain materials respond to stress. A material is considered brittle if it fractures with very little elastic deformation. This means it does not stretch or bend significantly before it breaks. There is also very little plastic deformation, which is a permanent change in shape. Because they do not deform much, brittle materials absorb relatively little energy before they fail. When they do break, the event is often accompanied by a sharp snapping sound.

Glass fracture
Glass fracture

One way to identify a brittle fracture is by looking at the broken pieces. In a truly brittle failure, the two broken halves should fit together exactly. This occurs because no plastic deformation happened to change the shape of the edges. This is a key concept in materials science. Scientists use this to understand how materials fail under pressure.

Cast iron tensile test
Cast iron tensile test

Different types of materials show different levels of brittleness. Polymers, which are common plastics, are very sensitive to temperature changes. For example, poly(methyl methacrylate) is extremely brittle at 4°C. As the temperature increases, it experiences increased ductility, meaning it becomes more flexible. Amorphous polymers can even change their entire state of matter. They may act like glass in a glassy region at low temperatures. At intermediate temperatures, they enter a leathery or glass transition region. At high temperatures, they enter a viscous flow region where they act like liquids. This changing behavior is known as viscoelastic behavior.

Metals and ceramics also behave in unique ways due to their internal structures. In metals, brittleness is often linked to slip systems. A slip system is a path that allows parts of the metal to move. Metals with many slip systems can undergo plastic deformation easily. Conversely, metals with fewer slip systems are more brittle. Hexagonal close packed (HCP) metals are a good example of this. Because they have few active slip systems, they are typically brittle.

Stress strain comparison brittle ductile
Stress strain comparison brittle ductile

Ceramics are generally brittle because it is difficult for dislocation motion to occur. Dislocation motion, or slip, is the movement of atoms within the crystal. In crystalline ceramics, there are very few slip systems available for this movement. Furthermore, most ceramics exhibit ionic bonding. The electric charges of the ions cause them to repel like-charged ions. This repulsion further restricts the ability of the material to slip or deform.

Engineers can perform a balancing act to change how brittle a material is. A naturally malleable metal can be made stronger by impeding plastic deformation. This can be done through work hardening or reducing grain size. However, if this is taken to an extreme, the material may become brittle. To improve toughness, scientists use different techniques. For laminated glass, two sheets are separated by an interlayer of polyvinyl butyral. This viscoelastic polymer absorbs the energy of a growing crack.

Brittleness diagrams
Brittleness diagrams

Another method involves creating composite materials to increase strength. In these materials, brittle glass fibers are embedded in a ductile matrix, such as polyester resin. When the material is strained, many cracks form at the glass-matrix interface. These many tiny cracks absorb a great deal of energy, which toughens the material. This same principle is used to create metal matrix composites. Some ceramics are also naturally less brittle. Silicon carbide is very strong, and transformation-toughened zirconia is another example of a less brittle structural ceramic.

There are even extreme examples of how cracks move through materials. Some cracks can undergo supersonic fracture. This means the crack moves faster than the speed of sound in that material. This phenomenon was discovered by scientists from the Max Planck Institute for Metals Research and the IBM Almaden Research Center. They included researchers Markus J. Buehler, Huajian Gao, and Farid F. Abraham. Finally, pressure can change brittleness in nature. Deep in the Earth's crust, high pressure can increase brittle strength. This creates a transition zone where rocks are less likely to fracture and more likely to deform ductilely.

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🖼️ Images & Media (4)
File:Glass fracture.jpg
Glass fracture.jpg
File:Cast iron tensile test.JPG
Cast iron tensile test.JPG
File:Stress strain comparison brittle ductile.svg
Stress strain comparison brittle ductile.svg
File:Brittleness diagrams.jpg
Brittleness diagrams.jpg
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