Page 33 - A Practical Companion to Reservoir Stimulation
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PRACTICAL COMPANION TO RESERVOIR STIMULATION




            EXAMPLE B-3                                          EXAMPLE B-4

            Calculation of Horizontal Stresses                   Critical Depth for Horizontal
                                                                 vs. Vertical Hydraulic Fractures
            Calculate the minimum horizontal stress at  10,000 ft depth
            for a formation with  the properties used  in  Example B-2.   Assuming  that  the  Poisson’s  relationship  is  in  effect  and
            Assume that  the  Poisson’s ratio  is  0.25. Will  the  absolute   assuming that the horizontal stresses are ‘‘locked’’  in place,
            minimum stress increase or decrease during reservoir deple-   what  would  be  the  critical  depth  above  which  horizontal
            tion?                                                fractures would be generated if 2000 ft of overburden were
                                                                 removed by  some geologic means? Use the formation vari-
            Solution (Ref. Section 2-4.1)                        ables given in Example B-2.
            Equation 2-41 a provides the absolute minimum  horizontal
            stress as a function of the vertical stress. The vertical stress is   Solution (Ref. Section 2-4.1)
            equal to the weight of the overburden. Furthermore, the pore   The  solution  to  this  problem  is  outlined  in  the  graphical
            pressure was assumed to be the hydrostatic value. Thus, at   construction shown in Fig. 2-20. Eq. 2-4 1 a can be rewritten
            10,000 ft,                                           as a function of depth, and with substitution of the calculated
                                                                 variables in Example B-2, it becomes
                          0.25
                    -           [I 1,483 - (0.72) (3507)l
              OH, miri  -                                                                                   (B-17)
                       (I  - 0.25)
                                                                   Figure B-2 is a graph of the vertical and minimum hori-
                       + (0.72) (3507)  =  55 1 1 psi.   (B- 13)   zontal stresses. The “original” vertical  stress is shown as a
            The effective minimum stress is then                 dashed line, whereas the current vertical stress, relieved by
                                                                 2000 ft of  overburden, is shown as a solid line, starting at
              (5~,.,jr,  =  551 1  - (0.72) (3507)  =  2986 psi.   (B-14)   H  = -2000  ft.  The  slope  of  this  curve  is  also  165/144 =
                                                                 1.146, as for the “original” vertical stress.
            During  depletion  a  rearrangement  of  Eq.  2-41a  can  be   The intercept happens at 3847 ft from the original ground
            instructive:                                         surface or at  1847 ft from the current ground surface. Thus,
                                                                 depths shallower than this will likely develop a horizontal
                                                                 hydraulic fracture, and depths below this level will develop a
                                                                 vertical hydraulic fracture.
              As the pore pressure decreases, the C  J  decreases. For a  ~  ~  ~  ~  ~
                                                  ~
                                                     ~
                                                         ~
            1 000-psi depletion in  the reservoir pressure, the  minimum
            horizontal stress for this formation will decrease by
             A~~~,,,jJl (0.72) (1000) [ 111:;5] =  480psi.  (B-16)
                    =
                                   ~


























            B-4
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