Page 162 - Basic Well Log Analysis for Geologist
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LOG  INTERPRETATION  CASE  STUDIES




        Case  Study  1  Answer
           A  careful  examination  of  the  logs  recorded  through  the   moveable  oil  saturation  (MOS)  values  are  also  low.  Again,
         Atoka  Sandstone  provides  the  following  information.  On   this  is  initially  puzzling  because,  in  a  good  reservoir  with
         the  caliper  log  (Fig.  55),  mudeake  development  is  shown  by   high  porosity  and  permeability,  these  values  should  be  high.
         the  decreasing  hole  size.  This  mudcake  development  is   Additional  anomalous  information  comes  from  the
         important  because  it  indicates  a  permeable  zone.  Mudcake   calculation  of  the  moveable  hydrocarbon  index.  The  values
         forms  by  the  accumulation  of  solid  particles  from  drilling   are  greater  than  0.7,  but  (usually)  favorable  moveability
         muds  on  the  borehole  walls  when  a  porous  and  permeable   values  are  less  than  0.7.  Analyses  of  ROS,  MOS,  and  the
        zone  1s  invaded  with  drilling  fluids.  The  SP  log  (Fig.  54)   moveable  hydrocarbon  index  provide  negative  evidence  that
         shows  hydrocarbon  suppression  because  the  SP  reading  is   hydrocarbons  will  move.  Indeed,  all  of  these  factors  suggest
         less  than  SSP  Such  suppression  suggests  the  presence  of   that  most  of  the  hydrocarbons  will  remain  in  place  in  the
         hydrocarbons;  sample  shows  and  the  neutron-density  log   reservoir.
        response  (Fig.  55)  through  the  Atoka  tell  you  that  in  this   While  information  relating  to  inadequate  hydrocarbon
        case  the  hydrocarbons  will  probably  be  gas.  The  density  log   moveability  should  not  be  ignored  in  initial  log  evaluation,
        (Fig.  55)  reads  a  much  higher  porosity  than  the  neutron  log.   itcan  sometimes  be  explained  in  the  following  way.  In  this
         When  this  occurs,  it  is  because  of  gas  effect.   case,  what  is  stgnificant  is  the  high  residual  gas  saturation  in
           If  water  saturation  Archie  (S,,,)  and  porosity  (@)  values   the  flushed  zone  (1.0  —  S,,  =  residual  hydrocarbon
         are  crossplotted  (Fig.  57),  a  grain  size  variation  of   saturation).  This  high  residual  gas  saturation  is  the  result  of
         medium-grained  to  coarse-grained  is  shown  on  the  plot.   the  bypassing of gas  by  drilling  fluids  invading  a  reservoir.
        This  supports  sample  cutting  examination  which  indicates  a   The  high  residual  gas  saturation  left  behind  after  invasion
         medium-grained  to  coarse-grained  sandstone.           can  be  erroneously  read  by  the  logs  as  unmoved
          Crossplotting  irreducible  water  saturation  versus  porosity   hydrovarbons  (S,,,  <  S,"/5:  Chapter  V1).
         (see  Fig.  58)  reveals  that  the  Atoka  zone  has  good   Even  though  you  are  concerned  about  negative
        permeability  with  values  ranging  from  10  to  over  100   information  from  the  drill  penetration  rate  through  the
         millidarcies  (md).  Another  crossplot  in  Figure  59,   Atoka  Sandstone,  and  about  the  pessimistic  moveability
        comparing  a  calculated  irreducible  water  saturation  (Sj,  =   data,  vou  decide  that  the  other  evidence  from  sainple

         \F2000)  with  water  saturation  Archie.  shows  a  high   examination.  gas  shows,  and  log  interpretation  supports  a
        relative  permeability  to  gas  (K,,).  The  high  relative   decision  to  set  pipe.  Log  interpretation  information
        permeability  to  gas  (K,,)  means  there  is  a  correspondingly   especially  significant  to  your  decision  is:  high  porosities  on
         low  permeability  to  water  (K,,).  The  reservoir,  therefore,   the  neutron-density  logs,  strong  gas  effect  on  the
        should  not  produce  water.                              neutron-density  logs.  low  water  saturation  calculated  by  the
          The  values  derived  for  both  water  saturation  and  bulk   Archie  equation,  high  log-derived  permeabilities  from
         volume  witer  are  low.  These  low  values  also  indicate  that   various  permeability  crossplots,  and  the  low  bulk  volume
        the  Atoka  Sandstone  is  a  reservoir  with  a  high  gas  saturation   water  values.  While  you  believe  the  well  contains  a
        at  irreducible  water  saturation.  Because  water  saturation   gas-filled  Atoka  Sandstone  reservoir,  you  want  to  determine
         values  are  low,  it  follows  that  the  reservoir  must  have  high   whether  or  not  the  well  will  be  acommercial  success.  To  do
        gas  saturation  (remember:  |.0  —  S,  =  hydrocarbon   so.  you  calculate  volumetric  gas  reserves  before  making
        saturation).                                              your  final  pipe  setting  decision.
          Other  evidence  that  the  reservoir  is  at  irreducible  water   Anestimation  of  Atoka  Sandstone  gas  recovery  of  11.0
        saturation  und  has  high  gas  saturations  can  be  interpreted   BCF  is  calculated  by  using  the  following  paraineters:
         from  a  crossplot  (Fig.  60)  of  bulk  volume  water.  This   geothermal  gradient  =  0.014  <  formation  depth:  pressure
        expected  that  hydrocarbons  would  be  moved  out  instead  of     factor  =  0.85;  formation  temperature  =  205°F;  initial
                                                                  gradient  =  0.35  X  formation  depth;  drainage  area  =  560
        crossplot  is  created  by  plotting  water  saturation  Archie
        versus  porosity  (cb).  The  data  points  cluster  along  a
                                                                  acres;  reservoir  thickness  =  [5  ft:  effective  porosity  =
        hyperbolic  line  and  have,  then,  approximately  equal  values
                                                                  15%,  water  saturation  =  13%;  gas  gravity  =  0.65;  recovery
         for  bulk  volume  water  (BVW).  Bulk  volume  water  values
                                                                  bottom  hole  pressure  =  5,117  PSI;  Z  factor  =
                                                                                                        0.988.
        plotted  along  the  hyperbolic  line  range  from  0.015  to  0.027.
                                                                    The  Atoka  Sandstone  was  perforated  from  14,610  to
        Their  clustering  also  supports  the  conclusion  that  the
                                                                  14,615  ft.  The  calculated  absolute  open  flow  (CAOF)  was
        reservoir  has  high  gas  saturation  at  irreducible  water
                                                                  21,900,000  cu  ft  of  gas  per  day  (21,900  mcfgpd)  with  a
        saturation.
                                                                  high  shut-in  tubing  pressure  (SITP)  of  3,758  pounds  per
           Values  calculated  for  residual]  oil  saturation  (ROS)  are
                                                                  square  inch  (PSI)  and  a  high  initial  bottom  hole  pressure
        high.  This  ts  anomalous  because  other  evidence  supports
        the  conclusion  that  the  reservoir  has  high  porosity  and
                                                                  (IBHP)  of  5.556  PSL.  The  gas  gravity  was  0.599  at  a  bottom
        permeability.  Under  these  conditions,  it  could  ordinarily  be
                                                                  hole  temperature  of  219°F  The  well’s  first  year  cumulative
                                                                  production  was  3,268,129  mcf  plus  95,175  barrels  of
         left  behind  in  the  rock.  Furthermore,  calculations  of   condensate.
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