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152   Applied Petroleum Geomechanics












                         Figure 4.10 Model of a penny-shaped fracture.


          (p 0 ) acting over the whole circular area, Sneddon (1946) derived the
          following equation to calculate the fracture width:

                                            2
                                     8ð1   n Þ  p ffiffiffiffiffiffiffiffiffiffiffiffiffiffi
                                                  2
                              wðrÞ¼          p o L   r 2              (4.47)
                                        pE
             If the applied pressure p(r) is constant over a circular area of radius a   L
          (i.e., the internal pressure only acts on a certain area of 0 < r < a), then it
          has:

                                 pðrÞ¼ p 0 ;  0 < r < a
                                 pðrÞ ¼ 0;  a < r < L

             The fracture width can be obtained in the following form (Sneddon,
          1946):

                                   2  p
                            8ð1   n Þ   ffiffiffiffiffiffiffiffiffiffiffiffiffiffi    p ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
                                                          2
                                         2
                     wðrÞ¼          p o L   r 2  1    1   a =L 2      (4.48)
                               pE
             The maximum fracture width appears at the center of the circular
          fracture (when r ¼ 0):
                               8ð1   n Þp o L     p ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
                                      2
                                                       2
                         w max ¼            1     1   a =L 2          (4.49)
                                    pE
             Sneddon’s solution has been applied into oil and gas industry for
          hydraulic fracturing modeling and wellbore strengthening design (e.g.,
          Perkins and Kern, 1961; Khristianovic and Zheltov, 1955; Geertsma and de
          Klerk, 1969; Alberty and McLean, 2004; Zhang et al., 2016).


          4.4 Natural fractures and mechanical behaviors
               of discontinuities
          4.4.1 Discontinuities and discrete fracture network
          One of the most prominent features of the earth’s upper crust is the
          presence of joints and fractures (discontinuities) at all scales. A rock mass
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