One amplitude sets the stress near the tip
Put the origin at the tip of a crack that is opened by tension across its faces. At a small distance from the tip, the stress components all have the same form: an amplitude, divided by the square root of the distance, times a fixed function of the angle. The angular functions are universal. The geometry and the loads enter only through the amplitude.
That amplitude is the stress intensity factor. It has units of stress times the square root of length, so it must contain a length from the specimen, usually the crack length. For a centre crack in a large plate it is the remote stress times the square root of pi times the half-length. In a plate of finite width, a correction factor depending on the ratio of half-length to half-width multiplies it.
Stress intensity and energy release rate are one criterion
The near-tip field carries the energy that reaches the tip, so the energy release rate can be computed from the amplitude alone. The result is the square of the stress intensity factor divided by an effective modulus. In plane stress, for thin sheets, that modulus is Young’s modulus. In plane strain, for thick bodies, it is larger by one over one minus Poisson’s ratio squared.
For the centre crack this reproduces chapter one: the square of the stress times pi times the half-length, over the modulus. A critical stress intensity factor and a fracture energy are two ways of stating the same material property, for a crack that grows straight ahead under opening.
Worked example
Read the stress intensity factor from photoelastic fringes
A photoelastic sheet between crossed circular polarizers shows dark fringes where the principal stress difference is a whole multiple of a material fringe value divided by the thickness. For the near-tip field, the principal stress difference equals the stress intensity factor times the sine of the angle, over the square root of two pi times the distance. Each fringe is therefore a closed loop whose radius is largest straight above the tip.
Measure the largest radius of a loop of known order and solve for the stress intensity factor. The loop radius grows as the square of the stress intensity factor, so doubling the load makes each fringe loop four times larger. In practice a uniform stress parallel to the crack, absent from this one-term field, tilts and stretches the loops; careful measurements fit additional terms. The one-term reading is a first estimate.
How small the broken region has to be
The square-root field cannot hold all the way to the tip. In a metal the material yields where the field exceeds its yield stress. A first estimate of the size of that region sets the opening stress ahead of the tip, from the first formula of this chapter, equal to the yield stress and solves for the distance. It ignores the load that the yielded material passes on to its surroundings, so it only gives the order of magnitude. Bouchbinder, Fineberg and Marder list two requirements: linear elasticity must hold away from the tip, and all nonlinear processes must stay in a region that is small compared with the crack and the specimen.
If the region is not small, the energy release rate still exists as an energy flow, but a single critical value no longer predicts failure. That situation returns in chapter six, where a strength length comparable to the notch spreads the onset of cracking over an interval of grip openings.