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224   •  Chapter 7    /    Dislocations and Strengthening Mechanisms

                                each relative to the stress axis (f and l angles) also differs. However, one slip system is
                                generally oriented most favorably—that is, has the largest resolved shear stress, t R (max):
                                                     t R (max) = s(cos f  cos l) max                (7.3)
                                In response to an applied tensile or compressive stress, slip in a single crystal commences on
                                the most favorably oriented slip system when the resolved shear stress reaches some critical
            critical resolved   value, termed the critical resolved shear stress t crss ; it represents the minimum shear stress
              shear stress      required to initiate slip and is a property of the material that determines when yielding
                                  occurs. The single crystal plastically deforms or yields when t R (max)   t crss , and the magni-
            Yield strength of   tude of the applied stress required to initiate yielding (i.e., the yield strength s y ) is
            a single crystal—
            dependence on the                                     t crss
            critical resolved                           s y =                                       (7.4)
            shear stress and the                             (cos f cos l) max
            orientation of the
            most favorably      The minimum stress necessary to introduce yielding occurs when a single crystal is ori-
            oriented slip system  ented such that f = l = 45 ; under these conditions,
                                                             s y = 2t crss                          (7.5)
                                   For a single-crystal specimen that is stressed in tension, deformation is as in
                                Figure 7.8, where slip occurs along a number of equivalent and most favorably oriented
                                planes and directions at various positions along the specimen length. This slip defor-
                                mation forms as small steps on the surface of the single crystal that are parallel to one
                                another and loop around the circumference of the specimen as indicated in Figure 7.8.
                                Each step results from the movement of a large number of dislocations along the same
                                slip plane. On the surface of a polished single-crystal specimen, these steps appear as
                                lines, which are called slip lines. A zinc single crystal that has been plastically deformed
                                to the degree that these slip markings are discernible is shown in Figure 7.9.














                                         Direction
                                          of force






                                                 Slip plane







                                                                    Figure 7.9  Slip in a zinc single crystal.
                                     Figure 7.8                     (From C. F. Elam, The Distortion of Metal
                                     Macroscopic slip in a          Crystals, Oxford University Press, London,
                                     single crystal.                1935.)
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