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-  THE  GEOLOGICAL  INTERPRETATION  OF  WELL  LOGS  -


       Table  6.6  Resistivity  (conductivity)  measuring  tools  (see  also   these  tools  are  best  used  in  holes  drilled  with  conductive
       Figures,  6.14,  6.17  and  symbols  in  Table  6.4).   (salt)  muds,  (see  Section  6.6).  Of  the  very  shallow  ‘look-
                                                         ing’,  pad  mounted  devices,  the  Micro-spherically  focused
              Tool               Symbol     Resistivity
                                                         log  of  Schlumberger  (MSFL)  or  equivalent  from  other

                                                         companies,  is  the  one  most  frequently  used  for  a  good
       Pad
                                                         measurement  of  flushed  zone  resistivity,  R,,  (Table  6.6,
       tool    {Micro-log   normal   ML2”   Rt  Ry
                                                         Figure  6.18).  The  pad  devices  can  only  be  run  in  holes
                         inverse   MLI"  X  1”
                                                         with  conductive  muds.
              Micro-laterolog    MLL        RC  +R
              Proximity  log     PL         Rt,          Recent  developments
               *Micro-spherically                        There  has  been  very  little  change  in  the  basic,  standard
               focused  log      MSFL       R,            ‘hardware’  of  resistivity  logging  over  the  last  20  years,
                                                         such  as  the  laterologs  and  the  microlaterologs.  Perhaps

       Hole                                              the  only  new  departure  in  this  area  is  the  array  laterolog  of
                                                         BPB  which  gives  a  pad  micro-resistivity,  intermediate
       centred   *Spherically
                                                         resistivity  and  conventional  shallow  and  deep  resistivities.
               focused  log      SFL        R,
               Laterolog   shallow  —_ LLs   R,          With  four  measurements  an  invasion  profile  can  be  built
                                                         up.  There  has  however  been  change  in  the  way  that  the
                          deep   LLd        R
               Induction   medium   ILm     R,-R,        data  are  presented  so  that  presently  profile  colour  images,
                log       deep   ILd        R,            and  even  colour  images  of  simple  logs  are  available.
              Array     shallow             R,-R,           Considerable  new  development  is  occurring  in  the
                Induction   to  deep        (profile)     more  specialist  fields  and  the  present  effort  in  resistivity

                                                          logging  seems  to  be  centred  on  such  aspects  as  thin  bed
       tMinilog  —  Dresser
                                                         deep  resistivity  evaluation,  oriented  (directed)  resistivity
       *Schlumberger
                                                          measurements  for  horizontal  drilling  (ie.  the  Azimuthal
                                                          Resistivity  Imager,  ARI  of  Schlumberger,  see  Chapter
                                                          16)  and  improved  signal  processing  (cf.  Maute,  1992).
        A.  RESISTIVITY  PROFILE
                                       Rxo               These  efforts  are  directed  at  petrophysical  problems  and  a
                                                          geological  evaluation  of  the  new  tools  and  processing
                          Ri
                                                          techniques  is  continuing.
             Rt                                  g
                                                          6.5  Induction  tools
                      distance  (no  scale)              Standard  toots
                                                         The  induction  too]  was  introduced  to  the  industry  by

                    1              ,          >  g
         uninvaded  zone  '   invaded  zone   ,   flushed  zone  lz  3
                                                          Henn  Doll  of  Schlumberger  in  1949.  It  was  based  on  the
                                                          design  of  a  mine  detector.  A  basic  induction  tool  consists
                                             CML)         of  an  emitting  coil  and  a  receiving  coil  separated  along
                Lid    to}         |
                                                          the  length  of  the  tool  by  an  electrically  isolated  section
             ua}  typ         [sr]  |   aay               (mandrel).  A  constant  amplitude  sinusoidal  current  is
                                                          applied  to  the  transmitter  coi].  This  creates  a  magnetic
                   |
                                                          field  around  the  tool  which  in  turn  induces  eddy  currents

        “                distance
                                                          in  the  formation,  flowing  in  a  circular  path  around  the
       B.  PRINCIPAL  RESISTIVITY  INDICATED  (schamatic)
                                                          too]  (Figure  6.19).  The  eddy  currents  create  their  own
                    [vn   SPL                      g      magnetic  field  and  induce  an  alternating  current  in  the
               _.         °                        s      receiver  coi].  The  eddy  currents  are  90°  out  of  phase  with
        iad       _   ~~    s                      &
                                                          the  emitter  current  and  the  receiver  current  a  further  90°:
             Lan   ~      TO                       2
       “ee                      ~                  w
                                                          the  emitter  and  receiver  therefore,  show  a  180°  phase
         ig~  ~~   ~~   un        ~L               2      shift.  This  measured  current  is  the  so  called  R-signal.
                   |ao2S>-~=s                      9
                                                          There  is  also  a  much  stronger  current  caused  by  a  direct
                    |     SE
        <“                                         &      coupling  of  the  emitter  and  receiver  coils  which  is  90°  out

                         distance
                                                          of  phase  with  the  emitting  current:  this  is  the  X-signal.
       Cc.  GEOMETRIC  TOOL  RESPONSE  (schematic)          The  standard  modern  induction  tool,  such  as  the  Dual
                                                          Induction  of  Schlumberger,  was  introduced  in  1963,
       Figure  6.18  The  type  of  resistivity  measured  by  the  various
                                                          although  the  technology  had  already  existed  in  separate
       tools  (after  Schlumberger).  IL  =  induction  log,  deep-medium:
                                                          tools  for  some  time.  These  dual  induction  tools  consisted
       LL  =  laterologs,  deep-shallow;  SFL  =  spherically  focused  log;
       MSFL  =  micro-spherically  focused  log;  PL  =  proximity  log;   of  emitting  and  receiving  coils  along  with  a  series  of
       MLL  =  microlaterolog;  ML  =  microlog.          paired,  reverse  wound  coils,  precisely  placed  to  eliminate
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