Page 114 - Reservoir Geomechanics
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98     Reservoir geomechanics



                a.
                  300
                         Mohr–Coulomb criterion
                  250    C 0  = 325 MPa
                         m i  = 0.4
                         Mean misfit = 9.5 MPa
                  200
                  (MPa)  150

                 t
                  100


                   50

                   0
                    0         100       200       300       400       500
                                            s  (MPa)


                b.
                     800
                     700

                     600                           s 3

                     500                       s 3
                     (MPa)                 s 3 s 3
                     400                  s 3
                    s                   s 3
                     300                  s 2
                                        s 1                    (MPa)
                                                             s 3
                                                                = 0
                                                              s 3
                     200                                        = 6
                                                              s 3
                                                                = 15
                                                              s 3
                                  Modified Lade criterion       = 24
                                                              s 3
                     100          C  = 325 MPa                  = 46
                                   0                          s 3
                                                                = 72
                                  m i                         s 3
                      0
                       0    100   200  300   400  500  600   700  800
                                               (MPa)
                                            s 2
               Figure 4.10. Best-fitting solution for the Solenhofen limestone using the triaxial test data;
               (a) Mohr–Coulomb criterion; (b) modified Lade criterion. After Colmenares and Zoback (2002).
               Reprinted with permission of Elsevier.
               m and s. After studying a wide range of experimental data, Hoek and Brown (1980)
               proposed that the maximum principal stress at failure is given by

                              σ 3
               σ 1 = σ 3 + C 0 m  + s                                             (4.9)
                              C 0
               where m and s are constants that depend on the properties of the rock and on the extent
               to which it had been broken before being tested. Note that this form of the failure law
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