Fracture, and particularly brittle fracture, is a good example of an
instability. For a homogeneous solid, subjected to a uniform stress
field, a crack may appear anywhere in the structure once the threshold
stress is reached. However, once a crack has been nucleated in some
place, further damage in the solid will in most cases propagate from the
initial crack, and not somewhere else in the solid. In this sense
fracture is an unstable process. This property makes the process
extremely sensitive to any heterogeneity present in the medium, which
selects the location of the first crack nucleated. In particular,
fracture appears to be very sensitive to disorder, which can favor or
impede local cracks. Therefore, in most realistic cases, a good
description of fracture mechanics should include the effect of disorder.
Recently this need has motivated work in this direction starting from
the usual description of fracture mechanics. Parallel with this first
trend, statistical physics underwent a very important development in the
description of disordered systems. In particular, let us mention the
emergence of some "new" concepts (such as fractals, scaling laws, finite
size effects, and so on) in this field. However, many models considered
were rather simple and well adapted to theoretical or numerical
introduction into a complex body of problems. An example of this can be
found in percolation theory. This area is now rather well understood and
accurately described.