Page 190 - Open-Hole Log Analysis and Formation Evaluation
P. 190

~
                                     NaCl    grains/gal  at  75°F—>                     eos   oor   oor  4   003-4   ogi
                                           |    ppm——                                               O99   002   20,,   4,   “oe,   00,   04   205
                                  CONCENTRATION
                                 domo
                                    dog
                                        DN
                                          BE
                                           2
                                             £
                                      x
                                         n
                                       wy
                                        FOR  Nacl   ~
                                       SOLUTIONS
      176



                                e
                                 °
                               AYNLVESdW3L











                                                           RESISTIVITY  OF  SOLUTION  (OHM-METERS)             ~_  wdd   +>   doGL   05 /ujosB
                                9.
                                   w+—do
                              FIG         .     sgt
                                §  ~~
                                URE  9.11  Solution  Resistivity  vs.  Temperature  and  Concentration.  Courtesy  Schlumberger  Well
                              Services.
                                                                      o  \  i>















                                                                                                    more
           ratio
                                                                             to
                          SP
                                                                                          x  =
                          is
                                                                       ionic
           found
                                                                                                             0.08
                        or
                                                            #9.4
                            #9.5
                                                                                                             X
                                                                                                                 Ryps75
           from
                        figure
                                                                             Note
           the

                                                                                                             82/187
                                                                                                     more
            SP.
                                                                                          (0.6414
                                                                       the
                Rie
                                                                                    Of Ryz
                                                                   R,,, than
                                                                                                                 7/180
                                               Ratio  from
                                                          is
            mo   R,.  is   found  by   dividing  the   known  value  of   Step  5:   Computing           calculator  9.13  to  find  value  of   Rmjo/ Rwe   The   -100  mV  and   temperature  is   QUESTION           nn   where  K  =  =  (T°F  +   505)/8.   Alternatively,   Ruel Rwe  =   1O-sP/K,   ratio,   provided  a   calculator   The  SP   equation  may  be:  used   direct ly  to   compute   Step  4:   Rmje/Rwe  SP       Raye:   Ry  at   formation   temper ature  0.036
                                                                                                                 +
                          formation
                                                                       is
                                                                                    Ringe
                        the
                                                                              9.12
                                           is available:

                                                                       it
                                                           Om.

                                                                         filtrates
                                                                                           R,).
                                                                                                   Hilchie
                                   figure
                                                                                                     approximation

                                                                                to
              Ry,
                                                                                                     to
                                                                              constructed
                                                                          not
                                                                        normal
                                   9.13
                                                           figure
                                                                                be
              by
                           180°F.
                                                                        to
                                                                      =
                                                                                                     the
                                                                              for
                                                                                                   equation
                                              the
                                                                            and  calcium
                                                           9.12
              the
                           Use
                                                                                  Of  RingtO
                                                                      9:89.
                                   may  be
                                                           to
                                                                        treat
                                                                                                      data
                                                                          contain
                                                                                                   states

                                                                                                      of
                                                                                  Ryze:
                                                                                converted
                                                                              average
                                                                          the
                                                                            cations
                                                                      Rmy
                                                           find
                                                                                                      |
                                              Rmpe/ Rue
                                  oy
                           either a
                                   used.
                                                           .
                                                                        the.
                                                                      :
              Ry, sol Rive
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