Page 103 - The Geological Interpretation of Well Logs
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-  SONIC  OR  ACOUSTIC  LOGS  -


         K—          SEQUENCE  FOR  SINGLE  LOG  VALUE  ————_-   consisting  of  a  transmitter  coupled  with  a  near  receiver
                                                           and  a  far  receiver  (Figure  8.4a).  Because  the  sonic  is
                     INTERVAL  BETWEEN
                         PULSES                            generally  run  hole-centred,  any  pulse  transmitted  by  the
                     50ms  (60  x  1079  5)
                                                           tool,  passes  first  into  the  mud,  it  is  then  refracted  at  the
                     jo.  20  times/second

                                                           borehole  wall,  travels  through  the  formation  close  to
                                                           the  borehole  wall  and,  at  a  critical  (slower)  velocity  is
          o
                                                           refracted  back  into  the  mud,  so  to  reach  the  tool  again
          é

         aly  ha,     Nace       Y  Nae    V   vr   _      where  it  is  detected.  A  significant  part  of  the  trajectory
                      V

         ,                                                 is  in  the  borehole  mud  (Figure  8.42).  However,  if  this
             200 ns                                        travel  path  is  considered  when  one  transmitter  is  used
          (200  2  1075  s)
                                                           with  two  receivers  (a  near  and  a  far),  the  mud  effects  can
           SONIC  PULSE
                                                           be  eliminated.  This  is  simply  achieved  by  measuring  the
         Figure  8.3  Sonic  tool  emitter  patterns  (schematic).  Typically
                                                           time  it  takes  for  the  signal  to  reach  the  far  receiver  and
         a  pulse  lasting  200  microseconds  is  emitted  every  50
                                                           from  this  subtracting  the  time  it  takes  to  reach  the  near
         milliseconds,  i.e.  20  times  a  second.  Four  pulses  are  needed
         for  a  complete  (BHC)  log  measurement.  (Re-drawn  from   receiver.  The  path  from  tool  to  borehole  wall  and  back,  in
         Serra,  1979).                                    the  mud,  is  effectively  common  to  both  trajectories,  as  is
                                                           the  section  of  the  path  between  the  transmitter  and  near
          The  borehole-compensated  sonic  tool  has  two  trans-   receiver:  al]  are  eliminated  on  subtraction.  What  is  not
         Mitter-receiver  groups  (one  inverted),  each  group   common  to  the  two  trajectories  is  the  time  taken  between
                                       a)  BOREHOLE            b)  LONG  SPACING
                                        COMPENSATED                 SONIC
                                           SONIC












                                                                              long





                                                                                measure



                                              Ty             [Ul   short







                                                                      T=transmitter
                                                                     L=lower  U=upper
                                                                       R=  receiver



         Figure  8.4  Sonic  tools.  Representations  of  (a)  a  borehole-compensated  sonic  tool  which  gives  instantaneous  readings  with  an
         inverted  receiver  transmitter  array  and  (4)  the  Long  Spacing  Sonic  Tool  (Schlumberger)  which  gives  long  and  short-spaced
         readings  using  2  time  (i.e.  position}  delay  system:  positions  (1)  and  (2)  are  both  relative  to  the  same  measure  point.  (Modified
         from  Thomas,  1977  and  Purdy,  1982).

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