Stress intensity factor

Stress intensity factors for various modes

In 1957, G. Irwin found that the stresses around a crack could be expressed in terms of a scaling factor called the stress intensity factor. He found that a crack subjected to any arbitrary loading could be resolved into three types of linearly independent cracking modes. These load types are categorized as Mode I, II, or III as shown in the figure. Mode I is an opening (tensile) mode where the crack surfaces move directly apart. Mode II is a sliding (in-plane shear) mode where the crack surfaces slide over one another in a direction perpendicular to the leading edge of the crack. Mode III is a tearing (antiplane shear) mode where the crack surfaces move relative to one another and parallel to the leading edge of the crack. Mode I is the most common load type encountered in engineering design.

Different subscripts are used to designate the stress intensity factor for the three different modes. The stress intensity factor for mode I is designated K_{\rm I} and applied to the crack opening mode. The mode II stress intensity factor, K_{\rm II}, applies to the crack sliding mode and the mode III stress intensity factor, K_{\rm III}, applies to the tearing mode. These factors are formally defined as:

: \begin{align} K_{\rm I} & = \lim_{r\rightarrow 0} \sqrt{2\pi r},\sigma_{yy}(r,0) \ K_{\rm II} & = \lim_{r\rightarrow 0} \sqrt{2\pi r},\sigma_{yx}(r,0) \ K_{\rm III} & = \lim_{r\rightarrow 0} \sqrt{2\pi r},\sigma_{yz}(r,0) ,. \end{align}

Relationship to energy release rate and J-integral

In plane stress conditions, the strain energy release rate (G) for a crack under pure mode I, or pure mode II loading is related to the stress intensity factor by: : G_{\rm I} = K_{\rm I}^2\left(\frac{1}{E}\right) : G_{\rm II} = K_{\rm II}^2\left(\frac{1}{E}\right) where E is the Young's modulus and \nu is the Poisson's ratio of the material. The material is assumed to be an isotropic, homogeneous, and linear elastic. The crack has been assumed to extend along the direction of the initial crack

For plane strain conditions, the equivalent relation is a little more complicated: : G_{\rm I} = K_{\rm I}^2\left(\frac{1-\nu^2}{E}\right), : G_{\rm II} = K_{\rm II}^2\left(\frac{1-\nu^2}{E}\right),.

For pure mode III loading, : G_{\rm III} = K_{\rm III}^2\left(\frac{1}{2\mu}\right) = K_{\rm III}^2\left(\frac{1+\nu}{E}\right) where \mu is the shear modulus. For general loading in plane strain, the linear combination holds: : G = G_{\rm I} + G_{\rm II} + G_{\rm III},. A similar relation is obtained for plane stress by adding the contributions for the three modes.

The above relations can also be used to connect the J-integral to the stress intensity factor because : G = J = \int_\Gamma \left(W~dx_2 - \mathbf{t}\cdot\cfrac{\partial\mathbf{u}}{\partial x_1}~ds\right) ,.

Critical stress intensity factor

Main article: Fracture toughness

The stress intensity factor, K, is a parameter that amplifies the magnitude of the applied stress that includes the geometrical parameter Y (load type). Stress intensity in any mode situation is directly proportional to the applied load on the material. If a very sharp crack, or a V-notch can be made in a material, the minimum value of K_\mathrm{I} can be empirically determined, which is the critical value of stress intensity required to propagate the crack. This critical value determined for mode I loading in plane strain is referred to as the critical fracture toughness (K_\mathrm{Ic}) of the material. K_\mathrm{Ic} has units of stress times the root of a distance (e.g. MN/m3/2). The units of K_\mathrm{Ic} imply that the fracture stress of the material must be reached over some critical distance in order for K_\mathrm{Ic} to be reached and crack propagation to occur. The Mode I critical stress intensity factor, K_\mathrm{Ic}, is the most often used engineering design parameter in fracture mechanics and hence must be understood if we are to design fracture tolerant materials used in bridges, buildings, aircraft, or even bells.

Polishing cannot detect a crack. Typically, if a crack can be seen it is very close to the critical stress state predicted by the stress intensity factor.

G–criterion

The G-criterion is a fracture criterion that relates the critical stress intensity factor (or fracture toughness) to the stress intensity factors for the three modes. This failure criterion is written as : K_{\rm c}^2 = K_{\rm I}^2 + K_{\rm II}^2 + \frac{E'}{2\mu},K_{\rm III}^2 where K_{\rm c} is the fracture toughness, E' = E/(1-\nu^2) for plane strain and E' = E for plane stress. The critical stress intensity factor for plane stress is often written as K_{\rm c}.

Examples

Infinite plate: Uniform uniaxial stress

Penny-shaped crack in an infinite domain

Finite plate: Uniform uniaxial stress

Edge crack in a plate under uniaxial stress

Infinite plate: Slanted crack in a biaxial stress field

Crack in a plate under point in-plane force

Loaded crack in a plate

Stack of Parallel Cracks in an Infinite Plate

Source:

If the crack spacing is much greater than the crack length (h a), the interaction effect between neighboring cracks can be ignored, and the stress intensity factor is equal to that of a single crack of length 2a.

Then the stress intensity factor at crack tip is

\begin{align} K_{\rm I} & = \sigma\sqrt{\pi a} \end{align}

If the crack length is much greater than the spacing (a h ), the cracks can be considered as a stack of semi-infinite cracks.

Then the stress intensity factor at crack tip is

\begin{align} K_{\rm I} & = \sigma\sqrt{h} \end{align}

Compact tension specimen

Single-edge notch-bending specimen

References

References

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