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108    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                    Equating Equations 3.10 and 3.1 1 and solving for k gives:



                                                                                 (3.12)



                    By definition, porosity is



                                                                                 (3.13)


                    Substituting 4 = nn?/@ from Equation 3.13 into Equation 3.12, one
                    obtains a simpler relationship between  permeability and porosity for
                    pores of the same size and radii equal to r:



                                                                                 (3.14)



                    where k is in cm2 (1  an2 = 1.013 x  lo8 darcys) or in pm2 (1 mD  =
                    9.871 x 10-4pm2) and 4) is a fraction.

                    Let svP be the internal surface area per unit of pore volume, where the
                    surface area As for n capillary tubes is n(2nrL) and the pore volume Vp is
                    n(nr;?L):


                                                                                 (3.15)



                    Let  svgr be the specific surface area of  a porous material or the total
                    area exposed within  the pore  space per unit  of  grain volume.  For a
                    bundle of capillary tubes, the total area exposed, At, is equivalent to the
                    internal surface area As; and the grain volume, Vg.  is equal to &L(l-9).
                    Thus



                                                                                 (3.16)


                    Combining Equations 3.15 and 3.16 gives:

                    SVg'  svp (")

                               1-4)                                              (3.17)
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