Page 165 - Standard Handbook Petroleum Natural Gas Engineering VOLUME2
P. 165

134   Reservoir Engineering


                  (text  continued from page  130)
                  The tools work well in low-resistivity formations with thick beds and in slightly
                  conductive muds.

                  lnduction  Tools. Since a  slightly conductive mud  is  necessary for  the  normal
                  tools, they cannot be used in very fresh muds or in oil-base muds. The induction
                  tool overcomes these problems by  inducing a current into the formation instead
                  of passing it through the mud-filled borehole. Figure 5-7513 shows a simplified
                  two-coil induction tool [58]. High-frequency alternating current is sent into the
                  transmitter coil. The alternating magnetic field that is created induces secondary
                  currents in the formation. These currents flow through a conductive formation
                  in circular paths called ground loops. These currents in turn create a magnetic
                  field  which  induces currents  in  the  receiver  coil.  The  signal  received  is  pro-
                  portional  to  the  formation  conductivity. Conductivity readings  are  then  con-
                  verted to resistivity. Additional coils are used to focus the tool so  that conductive
                  beds as thin as four feet can be detected. Induction tools work well in oil-base,
                  foam, air, gas, and fresh mud. The induction tool is unreliable above 500 a-m
                  and  useless  above  1,000 am  or  in  salt  muds.  Readings  are  only  considered
                  reasonable below  100 a-m and are accurate between 1 and 20 am when mud
                  is very fresh.
                  Phasor  lnduction  TOOIS. Since  the  early  1960’s, induction  logging tools  have
                  become  the  principal  logging  device for  fresh,  slightly conductive  to  non-
                  conductive (oil-base) muds. However, these devices are significantly affected by
                  environmental  (bore-hole size  and  mud  composition)  and  geological  (bed
                  thickness and invasion) conditions. Also, high formation resistivities (> 50 to
                  100 a-m) dramatically increase the difference between apparent Rt and true Rt
                  [58A, 1991. In 1986, Schlumberger introduced a new induction log to offset these
                  problems [58A]. This device is known by  the trade name Phasor Induction SFL
                  and  uses  a  standard  dual  induction  tool  array. The  difference  between  the
                  conventional  and  phasor  devices is  in  signal  processing  made  possible  by
                  miniaturization  of  computer  components.  Induction  tools  all  produce  two
                  signals: the  inphase (R-signal) induction measurement and the  quadrature  (X-
                  signal) induction  signal.  The  R-signal is what  is  presented on standard  dual
                  inductionSFL log presentations. The R-signal and X-signal measurements are
                  combined during advanced processing in  the logging tool  itself  to  produce a
                  log with  real  time  corrections  for  environmental and  geological conditions.
                  Apparent Rt is nearly equal to true Rt in most situations. Vertical resolution of
                  this device is about the same as conventional induction tools (about 6 feet), but
                  enhanced and  very  enhanced resolution phasor  tools  are  available that  have
                  vertical resolutions down to 2  feet [58A]. The primary advantages of  this tool
                  include much better  Rt  readings in high resistivity formations (i.e. > 100 a-m)
                  and more accurate readings in salty muds than previously possible.

                  Focused Resistivity Tools (Laferologs). The Laterologs are the primary salt-mud
                  resistivity tools. Salt mud presents a problem in that the path of least resistance
                  is within the borehole. Therefore the current must be forced into the formation
                  which  has higher resistance. To  do this, secondary electrodes (A,, and 4) are
                  placed  above and below  the  measuring current-emitting electrode (AJ.  These
                  secondary electrodes emit “focusing” or “guard” currents with the same polarity
                  as  the  measuring currents.  Small monitoring electrodes (MI, M,,  M,’ and  Me?
                  adjust the focusing currents so  that they are at the same potential as A, and 4.
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