Page 17 - Basic Well Log Analysis for Geologist
P. 17

BASIC  RELATIONSHIPS  OF  WELL  LOG  INTERPRETATION


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       formation  will  produce  increasing  amounts  of  water  relative   often  have  different  values.  Resistivity  is  measured  by
       to  hydrocarbons.                                        electric  logs.
         Water  saturation—is  the  percentage  of  pore  volume  in  a   Conrad  Schlumberger  in  1912  began  the  first  experiments
       rock  which  ts  occupied  by  formation  water.  Water  saturation   which  led,  eventually.  to  the  development  of  modern  day
       is  measured  in  percent  and  has  the  symbol  S,.    petrophysical  logs.  The  first  electric  log  was  run  September
                                                                5.  1927  by  H.  G.  Doll  in  Alsace-Lorraine,  France.  In  1941,
                            formation water occupying  pores
        water  saturation  (Sy)  =  =  —-——       :             G.  E.  Archie  with  Shell  Oil  Company  presented  a  paper  to
                       .      total  pore  space  in  the  rock
                                                                the  AIME  in  Dallas,  Texas,  which  set  forth  the  concepts
       Water  saturation  represents  an  important  log  interpretation   used  as  a  basis  for  modern  quantitative  log  interpretation
       concept  because  you  can  determine  the  hydrocarbon   (Archie,  1942).
       saturation  of  a  reservoir  by  subtracting  water  saturation   Archie's  experiments  showed  that  the  resistivity  of
                                                                                                          a
       from  the  value,  one  (where  |.0  =  100%  water  saturation).   water-filled  formation  (R,).  filled  with  water  having  a
         Irreducible  water  saturation  or  Sy  jp,  is  the  term  used  to   resistivity  of  R,  can  be  related  by  means  of a  formation
       describe  the  water  saturation  at  which  all  the  water  is   resistivity  factor  (F):
       adsorbed  on  the  grains  in  a  rock,  or  is  held  in  the  capillaries
                                                                                   R,  Ry
                                                                                     =
                                                                                       FX
       by  capillary  pressure.  At  irreducible  water  saturation,  water
       will  not  move,  and  the  relative  permeability  to  water  equals   where  the  formation  resistivity  factor  (F)  is  equal  to  the
       zero.                                                    resistivity  of  the  formation  100%  water  saturated  (R,)
                  —is
         Resistivity  the  rock  property  on  which  the  entire   divided  by  the  resistivity  of  the  formation  water  (R,,).
       science  of  logging  first  developed.  Resistance  is  the   Archie's  experiments  also  revealed  that  formation  factors
       inherent  property  of  all  materials,  regardless  of  their  shape   can  be  related  to  porosity  by  the  following  formula:
       and  size,  to  resist  the  flow  ofan  electric  current.  Different
       materials  have  different  abilities  to  resist  the  flow  of
       electricity.
         Resistivity  is  the  measurement  of  resistance;  the   where  m  is  a  cementation  exponent  whose  value  varies  with
       reciprocal  of  resistivity  is  conductivity.  In  log  interpretation.   grain  size,  grain  size  distribution,  and  the  complexity  of  the
       hydrocarbons,  the  rock,  and  freshwater  all  act  as  insulators   paths  between  pores  (tortuosity).  The  higher  the  value  for
       and-are,  therefore,  non-conductive  and  highly  resistive  to   tortuosity  the  higher  the  m  value.
       electric  flow.  Saltwater,  however,  is  aconductor  and  has  a   Water  saturation  (S,,)  is  determined  from  the  water  filled
       low  resistivity.  The  unit  of  measure  used  for  the  conductor   resistivity  (R,)  and  the  formation  resistivity  (R,)  by  the
       is  acube  of  the  formation  one  meter  on  each  edge.  The   following  relationship:
       measured  units  are  ohm-meter2/meter,  and  are  called
       ohm-meters.

                                                                where  n  is  the  saturation  exponent  whose  value  varies  from
                                                                1.8  to  2.5  but  is  most  commonly  2.
       Where:                                                     By  combining  the  formulas:  R,  =  F  x  Ry
         R  =  resistivity  (ohm-meters)                        and  S,,  =  (R,/R,)!/"  the  water  saturation  formula  can  be
          r  =  resistance  (ohms)                              rewritten  in  the  following  form:   Un
       measurements  recorded  at  different  depths  into  a  formation     This  is  the  formula  which  is  most  commonly  referred  to  as
         A  =  cross  sectional  area  of  substance  being  measured
                                                                                     FX  Ry
           (meters?)
                                                                                  Ww
                                                                                        R,
         L  =  length  of  substance  being  measured  (meters)
         Resistivity  is  a  basic  measurement of  a  reservoir’s  fluid
                                                                the  Archie  equation  for  water  saturation  (S,,).  And.  all
       saturation  and  is  a  function  of  porosity,  type  of  fluid  (i.e.
                                                                present  methods  of  interpretation  involving  resistivity
       hydrocarbons,  salt  or  fresh  water),  and  type  of  rock.
                                                                curves  are  derived  from  this  equation.
       Because  both  the  rock  and  hydrocarbons  act  as  insulators
                                                                  Now  that  the  reader  is  introduced  to  some  of  the  basic
       but  saltwater  is  conductive,  resistivity  measurements  made
                                                                concepts  of  well  log  interpretation,  our  discussion  can  be
       by  logging  tools  can  be  used  to  detect  hydrocarbons  and
                                                                continued  in  more  detail  about  the  factors  which  affect
       estimate  the  porosity  of a  reservoir.  Because  during  the
                                                                logging  measurements.
       drilling  of a  well  fluids  move  into  porous  and  permeable
       formations  surrounding  a  borehole,  resistivity
                                                                  Where  a  hole  is  drilled  into  a  formation,  the  rock  plus  the
                                                                Borehole  Environment
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