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Published byKathlyn Johns Modified over 6 years ago
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Fracture of Solids Theoretical tensile strength of a solid U(r) a r
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Fracture of Solids Work of fracture F(r) a 2g r
Work of fracture for a defect-free solid
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Stress Concentrations
Airy stress function a
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Stress Concentrations
Elliptical flaw 2a 2b The radius of curvature at a is, so for Def: Stress Concentration factor, Kt For the circular flaw
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Stress field of an Elliptical flaw
y ao bo x ao is the ellipse defined by the flaw. 2a The Cartesian coordinates, x, y are connected to the elliptical coordinates a, b by a b
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Stress field of an Elliptical flaw
r is the distance along y = 0. The relative values of r/a and b/a compared to 1 determine the behavior of and define regions of interest. In the region r/a < 1 the leading term (dominant) including the bluntness contribution of b/a is, r < a As b/a 0 (a sharp “crack”) the stress field decays as (a/r)1/2. In the region, r/a >1 and the stress field scales as (a/r)2
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Sharp Cracks 2a Central crack of length 2a in an infinite plate under uniform tension. The leading terms for r <<a, Def: Stress Intensity Factor, K
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Sharp Cracks The stress intensity factor defines the strength of the crack in much the same way as the Burgers vector defines the strength of a dislocation.
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Crack Loading Modes Mode III: Out-of plane or longitudinal shear
Opening Mode II: In-plane shear
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Units of K Y = numerical factor depending on geometry and loading MPa
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Sharp Cracks Mode I stress field Cartesian coordinates
Cylindrical polar coordinates
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Sharp Cracks Mode II stress field Cartesian coordinates
Mode III stress field Cartesian coordinates
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Griffith theory of fracture
Consider a crack of length 2a in a 2D plate of infinite extent under external boundary tractions. 2a da 2(a+da) The total energy, UT of the system is composed of 3 terms. Here U load is the work done by the applied loads Ti on the system. We will subsequently show that
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Griffith theory of fracture
For a thin plate under load the excess elastic energy in the system owing to the presence of the crack is, The surface energy of the crack system is The total energy may now be written as U a a*
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Griffith theory of fracture
We can find the position of the energy for fracture, corresponding to the maximum in UT, For the case of plain strain
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Griffith theory of fracture
Def: Crack extension force G is the (negative) change of potential energy per unit crack extension per unit width. Energy/area = Force/length
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Griffith theory of fracture
Mechanical work during crack extension 2a da 2(a+da) Apply tractions loading the crack system During crack extension the work done is
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Griffith theory of fracture
Mechanical work during crack extension The elastic energy at location 3 is just The change in elastic energy is just Then
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Griffith theory of fracture
Plane Strain We can rearrange this to read What is a “typical value” of K at which fracture of a brittle solid is predicted E ~ 1011 Pa, g ~ 1Jm-2 Many materials exhibit critical K values times larger then this. Why?
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Crack extension force a+da a P D Def: Crack extension force mg
Crack growth under fixed load
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Crack extension force a+da a P D Def: Crack extension force
Crack growth under fixed displacement
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Crack extension force Crack growth under fixed load
Crack growth under fixed displacement
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1st estimate of the plastic zone radius
At edge of plastic zone
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Reminder: Mode I Stress Intensity Factor
y (x2) r q x (x1) z (x3)
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Von Mises criterion (It helps to obtain principal stresses, first)
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Identify elastic-plastic boundary, r(q)
Principal stresses Identify elastic-plastic boundary, r(q) Substitute these stresses into Von Mises criterion & solve for r as function of q where
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SIZE & SHAPE OF THE PLASTIC ZONE
1.0 x y SIZE & SHAPE OF THE PLASTIC ZONE PLANE STRESS r(q)/ry PLANE STRAIN r(q)/ry
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