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1656_C02.fm  Page 45  Thursday, April 14, 2005  6:28 PM





                       Linear Elastic Fracture Mechanics                                            45



                                    TABLE 2.3
                                    Nonzero Stress and Displacement Components in Mode III
                                    (Linear Elastic, Isotropic Material)

                                          K       θ 
                                    τ xz  =−  III  sin
                                                 2
                                           2 πr   
                                         K      θ 
                                    τ yz  =  III  cos
                                                2
                                          2 πr   
                                                  θ
                                     u =  2 K µ  III  2π  r  sin  
                                      z
                                                  
                                                  2

                          Consider the Mode I singular field on the crack plane, where θ = 0. According to Table 2.1,
                       the stresses in the x and y direction are equal:
                                                                  K
                                                       σ    σ =  =  I                            (2.39)
                                                         xx
                                                             yy
                                                                  2 πr
                       When θ = 0, the shear stress is zero, which means that the crack plane is a principal plane for pure
                       Mode I loading. Figure 2.15 is a schematic plot of σ , the stress normal to the crack plane vs. distance
                                                               yy
                       from the crack tip. Equation (2.39) is valid only near the crack tip, where the 1  r   singularity
                       dominates the stress field. Stresses far from the crack tip are governed by the remote boundary
                       conditions. For example, if the cracked structure is subjected to a uniform remote tensile stress, σ yy
                                               ∞
                       approaches a constant value σ . We can define a singularity-dominated zone as the region where the
                       equations in Table 2.1 to Table 2.3 describe the crack-tip fields.
                          The stress intensity factor defines the amplitude of the crack-tip singularity. That is, stresses
                       near the crack tip increase in proportion to  K. Moreover, the stress intensity factor completely
                       defines the crack tip conditions; if K is known, it is possible to solve for all components of stress,
                       strain, and displacement as a function of r and θ. This single-parameter description of crack tip
                       conditions turns out to be one of the most important concepts in fracture mechanics.


                       2.6.2 RELATIONSHIP BETWEEN K AND GLOBAL BEHAVIOR

                       In order for the stress intensity factor to be useful, one must be able to determine K from remote
                       loads and the geometry. Closed-form solutions for  K have been derived for a number of simple


















                                                               FIGURE 2.15 Stress normal to the crack plane in
                                                               Mode I.
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