Page 480 - Petrophysics
P. 480

448    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                    The steady- or pseudosteady-state solutions of  this diffusivity equation
                    can be obtained using essentially the same mathematical procedure as
                    that used to solve Equation 7.54 for the flow of  incompressible fluids.
                    Thus, Equation 7.77 is equivalent to:


                                  wm(p)  - m(pw)l
                    qsc =                                                        (7.93)
                          1,422T[ln (0.472re/rw) + 0.25f + s)]


                    where:  qsc = gas flow rate at T,,  = GOOF and psc = 14.7 psia, MSCF/D.
                              k  = permeability, mD.
                              h  = thickness of formation, ft.
                              T = absolute reservoir temperature, OR
                              re = drainage radius, ft.
                             r,   = wellbore radius, ft.
                               f  = drainage boundary index, dimensionless.
                               s  = total skin factor, dimensionless.
                    m(pw), m(p)  = real gas pseudo-pressure at the well pressure and the
                                   average reservoir pressure, respectively, psi2/cP.


                    The real gas pseudopressure terms at any pressure, m(p), can be obtained
                    from published  tables  or by  numerical integration  (trapezoidal rule)
                    [26, 281. p also can be converted to m(p) by plotting the group 2p/pgz
                    vs. p on a Cartesian graph. This group is calculated for several values of
                    p using experimental values of pg and z. The area under the curve from
                    any convenient reference pressure, generally zero, to p is the value of
                    m(p) corresponding to p.
                      The m(p)  approach is theoretically a  better  method  than  p  and p2
                    approaches because it is valid for all pressure ranges, especially during
                    the unsteady-state flow regime when pg and z  may vary considerably.
                    Inasmuch as only the radial flows of gas during the steady and pseudo-
                    steady states are considered, all the gas-flow equations in the remainder
                    of  this  chapter  will  be  expressed  in  terms  of  the  pressure-squared
                    approach, and ps and z will be assumed to remain constant at the average
                    reservoir pressure. Several approaches are available in the literature for
                    deriving radial gasflow equations during the  steady-state flow regime
                    [27-291. By treating natural gas as a highly compressible fluid, radial flow
                    equations may be developed by combining Darcy’s law (assuming laminar
                    flow):




                                                                                 (7.94)
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