Griffith Rift

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The Griffith crack is a straight internal crack that is located in an infinitely extended disc . The Griffith crack represents the basic crack model in fracture mechanics and was named after Alan Arnold Griffith . Using this crack model, Griffith carried out fundamental theoretical analyzes of the crack and crack propagation. The Griffith crack is mainly used in theoretical considerations in linear-elastic fracture mechanics .

Load cases

Disc under tensile load

Griffith crack under tensile stress.

For a crack of length 2a in a disk under tensile stress (stress perpendicular to the crack plane) Griffith determined the rate of energy release

With

Where:

  • the modulus of elasticity
  • the Poisson's ratio
  • the specific surface energy

The stress intensity factor for crack opening mode I is calculated as follows

.

Washer under shear stress

Griffith crack under shear stress.

The stress intensity factor for crack opening mode II under shear stress is calculated as follows

.

meaning

Comparing the above K-factors for modes I and II with the general equation for the stress intensity factor for cracks in components

,

this shows that the geometry factors for the Griffith crack are and . Thus, the stress intensity factors and for cracks in any components can be normalized to the stress intensity factors of the Griffith crack.

See also

literature

  • TL Anderson: Fracture Mechanics; Fundamentals and Applications . CRC Press, Boca Raton 2004, ISBN 978-0849316562 .
  • D. Gross, Th. Seelig: fracture mechanics with an introduction to micromechanics . 5th edition, Springer, Berlin 2011, ISBN 978-3-642-10196-0 .
  • Kuna, M .: Numerical stress analysis of cracks - finite elements in fracture mechanics . 2nd edition, Vieweg + Teubner 2010, ISBN 978-3-8348-1006-9 .

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