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FORMATION RESISTIVITY FACTOR            205
















                                                    rt-------rl

                                         Figure 4.1. Resistivity measurement of salty water (11.
                                              ,        ”  +;r-                 ,

                                                               E











                                                    +L----C(
                                     Figure 4.2. Resistivi@ measurement of aporous rock sample [l].


                             Dividing Equation 4.3 by Equation 4.2 and canceling similar terms gives






                             Archie defined this ratio as the “formation resistivity factor FR” or [2]:

                                   Ro
                             FR   -                                                        (4.5)
                                  RW
                             For a given value of E, Iw will be greater than Io. Hence & will be greater
                             than Rw  and FR will always be greater than unity. Figure 4.3 shows the
                             qualitative effect of  brine  resistivity (assuming  all other factors,  such
                             as porosity, cementation, and amount of  shale remain constant) on FR
                             for limestone and clean sand, and shaly (“dirty”) sand. The formation
                             factor is essentially constant for clean sand and limestone. For dirty or
                             shaly sand, FR decreases as brine resistivity, Rw , increases; and although
                             & increases, it does not increase proportionately because the clay in
                             the water acts as a conductor. This effect is dependent upon the type,
                             amount, and manner of distribution of the clay in the rock. Equation 4.5
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