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METHODS OF STRESS ANALYSIS

                                        When the axes of the ellipse are oriented parallel to the field stress directions, equation
                                        6.22 reduces to
                                                           p              2        2
                                                        =    {(1 + K)[(1 + q ) + (1 − q ) cos 2  ]
                                                           2q
                                                                          2             2
                                                           − (1 − K)[(1 + q) cos 2  + (1 − q )]}      (6.23)
                                        In assessing the state of stress in the sidewall and crown of an elliptical excavation,
                                        i.e. for points A and B (  =  /2,   = 0) in Figure 6.4c, it is useful to introduce the
                                        effect of the local boundary curvature on boundary stress. For an ellipse of major and
                                        minor axes 2a and 2b, the radius of curvature at points A and B,   A and   B , is found
                                        from simple analytical geometry (Lamb, 1956) to be

                                                                      b 2       a 2
                                                                   A =  ,    B =
                                                                      a         b
                                        Since q = W/H = a/b, it follows that

                                                                  $            $
                                                                     W     1      H
                                                               q =      ,    =
                                                                    2  A   q     2  B
                                        Sidewall and crown stresses in the ellipse boundary, for the problem defined in Figure
                                        6.4c, may then be expressed as

                                                                                   $    !
                                                                                     2W
                                                       A = p(1 − K + 2q) = p 1 − K +
                                                                                        A
                                                                                                      (6.24)
                                                                                        $
                                                                                             !
                                                                     2K                   2H

                                                       B = p K − 1 +     = p K − 1 + K
                                                                     q                      B
                                          It will be shown later that the formulae for stress distribution about ideal excavation
                                        shapes, such as a circle and an ellipse, can be used to establish useful working ideas
                                        of the state of stress around regular excavation shapes.



                                        6.4  Computational methods of stress analysis

                                        The preceding discussion indicated that even for a simple two-dimensional excavation
                                        geometry, such as an elliptical opening, quite complicated expressions are obtained for
                                        the stress and displacement distributions. Many design problems in rock mechanics
                                        practice involve more complex geometry. Although insight into the stress distributions
                                        around complex excavation shapes may be obtained from the closed form solutions for
                                        approximating simple shapes, it is sometimes necessary to seek a detailed understand-
                                        ing of stress distribution for more complicated configurations. Other conditions which
                                        arise which may require more powerful analytical tools include non-homogeneity of
                                        the rock mass in the problem domain and non-linear constitutive behaviour of the
                                        medium. These conditions generally present difficulties which are not amenable to
                                        solution by conventional analysis.
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