Page 137 - Open-Hole Log Analysis and Formation Evaluation
P. 137

to
                                          Ry
                             the
        had
                       F,
                                    The
                                  took
                                                           high.
                                          =
                         series
             length
                                 a
        to
           system
                   link
                 manner.
               tortuous
                           saturated
                     formation
        be
                                          FR,
                   the
            of  the
                                                                  Ro
                             resistivity
                 (The
               paths
                           rock
                                 number
                                                                  as
                     factor.
                         of  straight
                             of
                       determined
          increases.
                                                           Conversely,
        related
              that
          It
                                    method  Archie
                             the
                       in
            tubular
                   electrical
                 simple
        by
                         lines
                           system,
                               with  a  variety  ofbrines.
                                 of  cores
          was
                                                           if Ais
                     Archie
                                      Electrical  Formation
                       this
                                   used
              pores
                           Rj.
                               He
            pore,
                             water,
                                                                  a  Function
                                   to
        some
          thus
                tubular
                                                           large,
                             &,,
          a
                         of  slope
                   formation
                           When
                                      Factor
            grows
              actually
                                   arrive
                       manner,
                             and
                     conducted

                                 of  different
                           the
        inverse
                                   at
                model
                       is
                         F  (see
          logical
                             the
                  factor
              take;
            larger
                                   this
                         fig.
                     many
                  to
            as
          step
                bears
                           results
              see
        power
          to
            the
                       referred
                               could  then  measure,
                                                             resistivity
              fig.
                         6.15).
                little
                           were
                                 porosity  and
                               at
                             resistivity
                      to
                                                             of
                  porosity
                                   conclusion
                      as
                  in
        function.
              6.16.)
                    experiments
          propose
                             of  the
                  a
            tortuosity
                                   was
                           plotted,
                    in
                                 saturated
              The
                                                             rock
          that
        Note
                    an
                           he
                relationship
            of  the

                to
                                 each
                                   simple.
       that
              factor
          F  and
                                                             system
                the
                    attempt
                             100%-water-
              Z,
                      the  electrical
            pore
                  predictable
                          founda
                                   He
                               each  brine  salinity,
       by
                                 one
                                                             is



                                      "
               Sp
                     Sw»
                                Ry
       Se
                                          F
           Ina
                                             HH  F   Fsuch  that   factor  by  some   formation   related  to  R,,  say  that  Ro  is  F  /¢?  or  II   ),  Ro  =   SRu   used   formation   to   ly  close   we  may  write   porosity  itself,  to  the  a  and   proportional   Where   Since  A  is  to  as  Ro.   water  is   referred   saturated  with   tock  100%   low.   The  resistivity  ofa   the   resistivity  is  apm   the  the   of  length  Zand   conductive  path   fo
                                    with
                                          =.
                                =
               =
                 a
                                                           FS
                       related
                     Was
                                                                            FIGURE

                                                                                                                THE
                          Archie’s
                                    the
           more
                       to
                   resistivity,
                                                                        definition
                                                                            6.16
                       its
                                                     1
                            Saturation
                                Ro/F
                   Ro,
                     equal
      Ry/R,.
                                                               .
               R)/R,.
                                =
                                                                       the
                                          0.81/¢?
                   to
                                                                                                                PHYSICS
                     to
                                                     and
                                            0.62/¢""°
                                                                   itself.
                               Ry
                                    definition
                                                       mare
                   the
                     the
                                                                                               .   OD   IO QOROQON   oXe       §  OF
                         experiments
                                                    mis
           generalized
                                                                            Schematic
                               X
                                                  factor
                       resistivity.
                                                  to

                       He
                                                                       formation
                                                                                                 ees.
                                                                      resistivity  ofa  rock  sample
          form,
                                    of  Fand
                     square
                               b"/a
                                          (Sands)
                                                    usually
                         showed
                   formation
                                                                                                                ROCK/ELUID
          this
                                                          |
                       found
                     root

                                                                       factor
                                                  porosity
                         that
                                   arrive
                                              (Carbonates)
                                                    close
                                                       experimentally
                                                                       is
                     of
                                      Ina  wet  formation  we  may  therefore
                                   at
                                                                   Eventually  Archie
                       that
                                                    to
                         the
                                                    2
                                                                       the
                    the
                                   the
                  resistivity
                       the
          €quation
                                                  relations
                                                                   found
                  R,,
                                            (Humble  formula-soft
                                                    (fig.
                                     combine
          can
                                                                            of  Tortuous  Pore  System.
                                                                       tatio
                    fatio
                if
                                                  are:
                                                                   that
                                                      determined
          be
                         Saturation
                                   equation
                                                    6.17).
                  that  is:
                    of  the
                        of  a
                                                       |
                                           formations)
          written
                    wet
                                                    Three
                                                      constants.
                        core
                                                                     100%  saturated  with  water  to  the
         as:
                                                                       Ro/R,—that
                                                      ais


                        could
                                                          |  |
                                                              i
                      fractional  water  saturation,
                    formation
                        be
                                     the  Fto@  relationship
                                                      usual-
                                                    commonly
                                           »
                                                                       the
                                                                   laboratory-measured
                                                                    resistivity

                                                                      -  is,  of              —~—-   OSGQO     a
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