Page 46 - The Geological Interpretation of Well Logs
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-  THE  GEOLOGICAL  INTERPRETATION  OF  WELL  LOGS  -

        changes  in  potential:  it  gives  no  absolute  values.  The   directly  into  the  soil.  Offshore,  however,  no  such
        surface  electrode  of  the  SP  must  be  an  effective  earth   possibility  exists.  Without  an  effective  earth,  the  SP  will
        (Wallace,  1968).                                 not  be  recorded.  The  SP  from  many  offshore  wells,  espe-
                                                          cially  from  floating  rigs,  is  useless  and  mostly  ignored.
        Log  presentation:  units  and  scales
                                                          This  is  a  pity.  The  SP  is  a  cheap  and  useful  log.
        SP  currents  are  measured  in  millivolts  (1   10°  volts)  and
                                                            The  search  for  an  effective  earth  offshore  is  difficult.
        the  scale  is  in  +  or  —  millivolts,  negative  deflections  to  the
                                                          The  one  most  commonly  used  for  floating  rigs  is  the
        left,  positive  to  the  right  (Figure  5.5).  The  log  is  usually  run
                                                          riser,  but  this  is  usually  in  electrical  connection  to  the  rig
        in  track  |  with  a  gamma  ray  or  caliper  log  (Figure  5.5).
                                                          and  any  rig  is  electrically  noisy.  Using  the  rig  legs  is  not
        Unwanted  logging  effects                        helpful  either  since  these  are  given  a  potential  themselves  to
        As  indicated  above,  for  the  SP  tool  to  work  effectively,  it   stop  rusting  and  as  waves  pass,  this  potential  changes  and
        must  be  connected  to  a  surface  earth.  For  onland  wells   causes  a  wavy  SP  —  which  is  only  indicative  of sea  state  and
        this  causes  no  problem  and  an  iron  probe  can  be  pushed   not  formation  characteristics!  (Wallace,  1968)  (Figure  5.7).
                        SPONTANEOUS  POTENTIAL
                                  -   >
                                 millivolts

                         1900m

                             °         \
                                        q
                                                            Well  data
                                                            R   m   0.4424  40  5°C

                                                            R       0.682  25°C
                                                              mf
                                                            Rmc    2:18  2   25°C

                                                            Borehole  temp.  80°C

                                                            Ry  *  0.27  2   25°C
                                             oC
                         1950m          an


                                    rm                      Lithology
                                    a|    /|$        ‘|
                                    ”     &          ‘|  clean
                             xt     ”     .           sand

                                     \y   o
                                          c£
                                          wh
                                        ae   i

                                         L4           ‘en   Produced  hydrocarbons


                                         aS
                                                         silt   tt  GAS

                                       <
                                                                 OIL
                                                            @
                         2000m


                                                         vopermeable
                                                         shaly
                                                  thin  sand


                                      !
                                                        4
        Figure  5.8  Example  of  the  shale  baseline  and  the  SSP  defined  on  an  SP  tog.  The  shale  baseline  is  the  maximum  positive  deflection
        (in  this  example)  and  occurs  opposite  shales.  The  SSP  is  a  maximum  negative  deflection  and  occurs  opposite  clean,  porous  and
        permeable  water-bearing  sandstones.
                                                       36
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