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8.3 Ductile Fracture  •  253

              Fracture


              8.2  FUNDAMENTALS OF FRACTURE
                                 Simple fracture is the separation of a body into two or more pieces in response to an im-
                                 posed stress that is static (i.e., constant or slowly changing with time) and at  temperatures
                                 that are low relative to the melting temperature of the material. Fracture can also occur
                                 from fatigue (when cyclic stresses are imposed) and creep (time-dependent deformation,
                                 normally at elevated temperatures); the topics of fatigue and creep are covered later
                                 in this chapter (Sections 8.7 through 8.15). Although applied stresses may be tensile,
                                 compressive, shear, or torsional (or combinations of these), the present  discussion will
                                 be confined to fractures that result from uniaxial tensile loads. For  metals, two fracture
              ductile fracture,   modes are possible: ductile and brittle. Classification is based on the  ability of a material
              brittle fracture   to experience plastic deformation. Ductile metals typically exhibit substantial plastic de-
                                 formation with high energy absorption before fracture. However, there is  normally little
                                 or no plastic deformation with low energy absorption accompanying a brittle fracture.
                                 The tensile stress–strain behaviors of both fracture types may be  reviewed in Figure 6.13.
                                    Ductile and brittle are relative terms; whether a particular fracture is one mode or the
                                 other depends on the situation. Ductility may be quantified in terms of percent elongation
                                 (Equation 6.11) and percent reduction in area (Equation 6.12). Furthermore, ductility is a
                                 function of temperature of the material, the strain rate, and the stress state. The disposi-
                                 tion of normally ductile materials to fail in a brittle manner is discussed in Section 8.6.
                                    Any fracture process involves two steps—crack formation and propagation—in
                                 response to an imposed stress. The mode of fracture is highly dependent on the
                                 mechanism of crack propagation. Ductile fracture is characterized by extensive plastic
                                 deformation in the vicinity of an advancing crack. Furthermore, the process proceeds
                                 relatively slowly as the crack length is extended. Such a crack is often said to be stable—
                                 that is, it resists any further extension unless there is an increase in the applied stress.
                                 In addition, there typically is evidence of appreciable gross deformation at the fracture
                                 surfaces (e.g., twisting and tearing). However, for brittle fracture, cracks may spread
                                 extremely rapidly, with very little accompanying plastic deformation. Such cracks may
                                 be said to be unstable,  and crack propagation, once started, continues spontaneously
                                 without an increase in magnitude of the applied stress.
                                    Ductile fracture is almost always preferred to brittle fracture for two reasons:
                                 First, brittle fracture occurs suddenly and catastrophically without any warning; this is
                                 a consequence of the spontaneous and rapid crack propagation. However, for ductile
                                 fracture, the presence of plastic deformation gives warning that failure is imminent,
                                 allowing preventive measures to be taken. Second, more strain energy is required to
                                 induce ductile fracture inasmuch as these materials are generally tougher. Under the
                                 action of an applied tensile stress, many metal alloys are ductile, whereas ceramics are
                                 typically brittle, and polymers may exhibit a range of behaviors.


              8.3  DUCTILE FRACTURE
                                 Ductile fracture surfaces have distinctive features on both macroscopic and microscopic
                                 levels. Figure 8.1 shows schematic representations for two characteristic macroscopic
                                 fracture profiles. The configuration shown in Figure 8.1a  is found for extremely soft
                                 metals, such as pure gold and lead at room temperature, and other metals, polymers,
                                 and inorganic glasses at elevated temperatures. These highly ductile materials neck
                                 down to a point fracture, showing virtually 100% reduction in area.
                                    The most common type of tensile fracture profile for ductile metals is that repre-
                                 sented in Figure 8.1b, where fracture is preceded by only a moderate amount of necking.
                                 The fracture process normally occurs in several stages (Figure 8.2). First, after necking
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