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114   Applied Petroleum Geomechanics


          s 3 ¼ 50 MPa, and the hydrostatic pressure p n ¼ 31 MPa. Two scenarios on
          how pore pressure variations impact the minimum stress are examined here.
          If the total stresses (s 1 , s 2 , and s 3 ) keep unchanged with pore pressure
          variations, the increase in pore pressure (or overpressure) will reduce the
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          minimum and maximum effective stresses (s 1 , s 3 ). This will move the
          Mohr circle to the left side, making the Mohr circle touch or cross the shear
          failure envelope and causing shear failures (Fig. 3.22A). However, in most
          cases the increase of pore pressure may also cause the minimum horizontal
          stress s 3 to increase as field observed (e.g., Hillis, 2000; Engelder and
          Fischer, 1994). Therefore, the other scenario is that the increase in the
          minimum horizontal stress induced by the increase of pore pressure causes
          the Mohr circle size reduction (Fig. 3.22B) with assumption of no change in
          vertical stress s V . The rock in this case is much less likely to have shear
          failures than the one shown in Fig. 3.22A. By contrast, the decrease in pore
          pressure (e.g., the reservoir depletion) increases the Mohr circle size and
          moves the circle to the right side (Dohmen et al., 2013, 2017), and the
          increased Mohr circle sizes may, then, cross the shear failure envelope and
          cause shear failures (see Fig. 3.22B).

          3.4.2.2 Modified MohreCoulomb failure criterion
          Triaxial tests have found that the MohreCoulomb failure envelope has a
          nonlinear behavior (e.g., Fig. 3.23). It was recognized in 1970s that the
          shear strength envelopes for intact rocks, when tested over a wide range of
          confining stress, would have an obvious curvature, and eventually reach a
          horizontal stage with no further increase in strength (Barton, 2013). This
          was termed the “critical state,” and the simple relation s 1 ¼ 3s 3 suggested


















          Figure 3.23 Nonlinear failure envelope from triaxial compression tests for Daye
          marble. (Plotted from the data presented by Ouyang, Z., Elsworth, D., 1991.)
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