Page 251 - Petrophysics 2E
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224    PETROPHYSICS: RESERVOIR ROCK PROPERTIES



                              1000


                            ape les
                            O
                             LI
                             %oo
                             b
                             a-
                             0
                             m
                             LL
                             -
                             C
                             0
                             U
                             m
                               10
                             0
                             U
                                             ctm Varier  From
                                1
                                0.001        0.01         0.1          1.0
                                           Poroslty ( q5 1,  Fraction
                 Figure 4.13. Effect  of  overburden pressure on formation factor  (courtesy of  Core
                 Laboratories).


                 increases from 1.99 at zero overburden pressure to 2.23 at an overburden
                 pressure of 5,000 psi. Nearly all of the values of m in widespread use today
                 were determined on unconfined core samples.  Of  course, resistivity
                 measurements determined under representative overburden pressures
                 are strongly recommended for improved well log interpretation.


          THEORETICAL FORMULA FOR FR


                   Many attempts have been made to derive a general formula relating
                 formation resistivity,  porosity,  and  cementation factor. If  an electric
                 current  is  passed  through  a  block  of  nonconducting  porous  rock
                 saturated with  a  conducting fluid,  only a portion  of  the  pore  space
                 participates in the flow of electric current. Therefore, the total porosity
                 @ can be divided into two parts such that [9]:


                 @  = @ch -k  @tr                                             (4.41)
                 where @ch and    are, respectively, the flowing porosity associated with
                 the channels and the porosity associated with the regions of  stagnation
                 (traps) in a porous rock. Apparently, @ch is equivalent to the “effective
                 porosity” used by Chilingarian and  @tr is equivalent to the irreducible fluid
                 saturation [ 101. Figures 4.14 and 4.15  show that the electrical current
                 can flow only through the channel indicated by C, whereas no current
                 can flow through the traps indicated by T. In Figure 4.14 the traps are of
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