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118   Applied Petroleum Geomechanics


          friction in the plane of weakness, respectively; m w ¼ tan4 w ; and 4 w is the
          angle of internal friction in the plane of weakness.
             In terms of effective stresses, Eq. (3.49) can be expressed in the
          following form:


                                          2 c w þ m s 0
                              0   0              w 3
                             s   s ¼                                  (3.50)
                              1   3
                                      ð1   m cot bÞsin 2 b
                                            w
             The value of s 1 required to cause failure, as given by Eqs. (3.49) and
          (3.50), trends to infinity as b /90 or b / 4 w (i.e., failure in the rock). In


          other words, when 0 < b < 4 w and b ¼ 90 , the planes of weakness have
          no impact on the rock strength. If 4 w < b < 90 , shear failure will occur in

          the weak planes at a finite value of s 1 that varies with b, as shown in
          Fig. 3.26B. The minimum strength occurs in the following condition (refer
          to Fig. 3.26B):

                                  b min  ¼ 45 þ 4 =2                  (3.51)
                                                w
             Compared to the experimental results in the outcrop of the Mancos
          shale, the model of the planes of weakness Eq. (3.49) gives a good
          prediction (Fig. 3.27). For multiple sets of parallel planes of weakness, su-
          perposition principle can be used in Eq. (3.50) to solve the complex
          problem.

























          Figure 3.27 Measured uniaxial compressive strengths versus b and the strength
          predicted by the planes of weakness model in the Mancos shale (Eq. 3.49). (After Fjær,
          E., Nes, O.M., 2013. with permission of ARMA).
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