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                 80    Mechanical Engineering Design
                  Figure 3–8                    y                                 y

                  (a) General three-dimensional       y
                  stress. (b) Plane stress with
                                                                                    y
                  “cross-shears” equal.                  yx                             xy
                                                            xy
                                                     yz                                   xy
                                                                  x
                                                                                                    x
                                                    zy                 x                      x
                                                                   x       xy

                                                     zx
                                                             xz                  xy    y

                                               z
                                          z
                                                      (a)                          (b)


                                          Note that double subscripts are necessary for the shear. The first subscript indicates
                                          the direction of the surface normal whereas the second subscript is the direction of
                                          the shear stress.
                                              The state of stress at a point described by three mutually perpendicular surfaces is
                                          shown in Fig. 3–8a. It can be shown through coordinate transformation that this is suf-
                                          ficient to determine the state of stress on  any surface intersecting the point. As the
                                          dimensions of the cube in Fig. 3–8a approach zero, the stresses on the hidden faces
                                          become equal and opposite to those on the opposing visible faces. Thus, in general, a
                                          complete state of stress is defined by nine stress components,  σ x ,σ y ,σ z ,τ xy ,
                                          τ xz ,τ yx ,τ yz ,τ zx , and τ zy .
                                              For equilibrium, in most cases, “cross-shears” are equal, hence
                                                                                                            (3–7)
                                                             τ yx = τ xy  τ zy = τ yz  τ xz = τ zx
                                          This reduces the number of stress components for most three-dimensional states of
                                          stress from nine to six quantities, σ x ,σ y ,σ z ,τ xy ,τ yz , and τ zx .
                                              A very common state of stress occurs when the stresses on one surface are zero.
                                          When this occurs the state of stress is called plane stress. Figure 3–8b shows a state of
                                          plane stress, arbitrarily assuming that the normal for the stress-free surface is the
                                          z direction such that σ z = τ zx = τ zy = 0. It is important to note that the element in
                                          Fig. 3–8b is still a three-dimensional cube. Also, here it is assumed that the cross-shears
                                          are equal such that τ yx = τ xy , and τ yz = τ zy = τ xz = τ zx = 0.


                                  3–6     Mohr’s Circle for Plane Stress

                                          Suppose the dx dy dz element of Fig. 3–8b is cut by an oblique plane with a normal n at
                                          an arbitrary angle φ counterclockwise from the x axis as shown in Fig. 3–9. Here, we are
                                          concerned with the stresses σ and τ that act upon this oblique plane. By summing the
                                          forces caused by all the stress components to zero, the stresses σ and τ are found to be

                                                               σ x + σ y  σ x − σ y
                                                           σ =        +        cos 2φ + τ xy sin 2φ         (3–8)
                                                                  2        2
                                                                 σ x − σ y
                                                           τ =−        sin 2φ + τ xy cos 2φ                 (3–9)
                                                                   2
                                          Equations (3–8) and (3–9) are called the plane-stress transformation equations.
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