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Chapter 2.  Fundamentals of  mechanics of solids   33

            located  inside the body and that point B coincides with the origin 0 of Cartesian
            coordinates x. y, z in  Fig. 2.1. Then, the oblique plane  of the tetrahedron can be
            treated  as a coordinate plane z‘ = 0 of  a new coordinate frame x’, y’, 1 shown in
            Fig. 2.4 and such that  the normal element to the oblique plane coincides with the
            z’-axis, while axes x’  and y’  are located in this plane. Component P,~of the surface
            traction in Eqs. (2.2) can be treated now as the projection  on the x-axis of stress (T
            acting on plane z’ = 0. Then, Eqs. (2.2) can be presented  in the following explicit
            form specifying projections  of stress (T







            Here, I  are directional cosines of axis z’ with respect to axes x, y, and z (see Fig. 2.4
            in which the corresponding cosines of axes x’  and y’ are also presented).  Normal
            stress o=,can be found now as








            The final result was obtained with the aid of Eqs. (2.6)and (2.7). Changing x’for y’,
            y‘  for 2. and z’ for x’, Le., performing permutation  in Eq. (2.8) we can write similar
            expressions for a.,~and cy!.



























                                 Fig. 2.4.  Rotation of the coordinate frame.
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