Materials can be changed to become more brittle or less brittle.
Toughening s for brittle and ductile materials When a material has reached the limit of its strength, it usually has the option of either deformation or fracture. A naturally
malleable metal can be made stronger by impeding the mechanisms of plastic deformation (reducing
grain size,
precipitation hardening,
work hardening, etc.), but if this is taken to an extreme, fracture becomes the more likely outcome, and the material can become brittle. Improving material
toughness is, therefore, a balancing act. Naturally brittle materials, such as
glass, are not difficult to toughen effectively. Most such techniques involve one of two
mechanisms: to deflect or absorb the tip of a propagating crack or to create carefully controlled
residual stresses so that cracks from certain predictable sources will be forced closed. The first principle is used in
laminated glass where two sheets of glass are separated by an interlayer of
polyvinyl butyral. The polyvinyl butyral, as a
viscoelastic polymer, absorbs the growing crack. The second method is used in
toughened glass and
pre-stressed concrete. A demonstration of glass toughening is provided by
Prince Rupert's Drop. Brittle
polymers can be toughened by using metal particles to initiate crazes when a sample is stressed, a good example being
high-impact polystyrene or HIPS. The least brittle structural ceramics are
silicon carbide (mainly by virtue of its high strength) and transformation-toughened
zirconia. A different philosophy is used in
composite materials, where brittle
glass fibers, for example, are embedded in a ductile matrix such as
polyester resin. When strained, cracks are formed at the glass–matrix interface, but so many are formed that much energy is absorbed and the material is thereby toughened. The same principle is used in creating
metal matrix composites.
Effect of pressure Generally, the
brittle strength of a material can be increased by
pressure. This happens as an example in the
brittle–ductile transition zone at an approximate depth of in the
Earth's crust, at which rock becomes less likely to fracture, and more likely to deform
ductilely (see
rheid). ==Crack growth==