Page 287 - Petrophysics 2E
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260    PETROPHYSICS: RESERVOIR ROCK PROPERTIES


                    Combining Equations 4.122-4.126, one can obtain the Waxman-Smits
                    general equation for water-saturated shaly (clayey) sands:


                                                                                (4.127)

                    with  C,,,   the  equivalent  conductance  of  clay  exchange  cations,
                    expressed in mho/cm2/meq-'  and given by:

                    c,,  = 10-~h~,                                              (4.128)

                    Equation 4.127 can be written as follows:


                                                                                (4.129)

                     or:


                                                                                (4.130)


                    where FR is the Archie formation resistivity factor for clean sand, Cw/Co.
                     Hoyer and Spann used Equation 4.129 to quantify the effects of shaliness
                     on electric log response [29]. They showed that ifCeqQ,/Cw  < 0.10, the
                     shaliness effect is negligible, and conventional clean sand relationships
                     can be used to interpret well logs. Shaliness effect is significant when
                     Ceq&/C,  > 0.10, and shaly sand relationships must be used to interpret
                     logs. Several methods are available for measuring the cation exchange
                     capacity of  a rock,  Qv. Mortland  and Mellow described a procedure
                     for measuring CEC  that  gives  results with  an  accuracy equivalent to
                     that using the ammonium acetate method [30]. This procedure requires
                     repeated  equilibration of the crushed rock sample with concentrated
                     barium chloride (BaC12) solution and washing to remove excess barium
                     ions,  followed by  conductometric titration with  standard magnesium
                     sulfide (MgSO4)  solution. Table 4.8 gives porosity, @;  permeability, k;
                     formation resistivity factor,  F* ; cation exchange capacity,  Qv; water
                     conductivity, Cw; and rock conductivity at 100% water saturation, Co,
                     of some of representative sandstone samples.
                       Waxman  and  Smits  presented  a  lengthy  but  rigorous  procedure
                     to  determine  CEC  [28]. Because  the  method  used  was  destructive,
                     conductivity measurements  were made on rock samples adjacent to the
                     locations where the cores originated. The rock samples were equilibrated
                     by repeated flushing and storing  in a desiccator filled with the appropriate
                     salt solution. The CEC and conductivity measurements were  made at
                     25OC on the shaly sands equilibrated with NaCl solutions at 10 different
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