Page 62 - Standard Handbook Petroleum Natural Gas Engineering VOLUME2
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50    Reservoir Engineering


                    where cf is the formation (rock) compressibility with common units of  psi-', V
                    is pore volume, p is pressure in psi, and the subscript T denotes that the partial
                    derivative is taken at constant temperature. The effective rock compressibility
                    is  considered a  positive quantity  that  is  additive  to  fluid  compressibility;
                    therefore,  pore  volume decreases as fluid  pressure  decreases [26,66]. Since
                    overburden pressure of a reservoir is essentially constant, the differential pressure
                    between  the  overburden pressure and the  pore  pressure will  increase as  the
                    reservoir is depleted. Thus, porosity will decrease slightly, on the order of  only
                    one-half percent  for  a  1,000 psi  change in  internal  fluid  pressure [17].  For
                    different  reservoirs,  porosities  tend  to  decrease as  overburden pressure  (or
                    depth) increases. Therefore, porosity under reservoir conditions may differ from
                    values  determined  in  the  laboratory  [67]. For  sandstones with  15%  to  30%
                    porosity, reservoir porosity was  found  to be  about  1% lower under  reservoir
                    conditions; for low  porosity limestones, the difference was  about 10% [68J.
                      One  of  the  commonly cited correlations between  rock  compressibility and
                    porosity was  developed by  Hall  [69] (Figure 5-34} for  several sandstone and
                    limestone reservoirs. All measurements were conducted with an external pressure
                    of  3,000 psi  and  internal pressures  from  0  to  1,500 psi.  Fatt  [67] found no
                    correlation between compressibility and porosity, although the porosity range
                    studied (10% to 15%) was very narrow. Van  der Knapp [68], citing his measure-
                    ments and those of  Carpenter and Spencer [70], observed a general trend  of
                    increasing pore volume compressibility with decreasing porosity. For a particular
                    limestone reservoir, Van der. Knapp  [68] found  that  pore  compressibility and





                                                              0 LIMESTONE           -
                                                              e SANDSTONE           -
                                                                                    -
                                                                                    -

                                                                              22






                           -

                           -
                         3-
                           -
                         2-                      -a  w-                             "
                                                   3d
                          I-                                                        -
                           -                     I  1  '  '  '  '  '  '  '  1  '  '  I  1  ' '
                         0   '  '  1   1-1   I  '  I  1  __
                                            ~
                          0    2   4    6    8   IO   12   14   16   18   20  22  24  26
                                                  POROSITY , O/o
                            Figure 5-34. Effective rock compressibility vs.  porosity 1691.
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