Page 189 - Standard Handbook Petroleum Natural Gas Engineering VOLUME2
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158    Reservoir Engineering












                                        6000








                                        6100


                    Figure 5.88.  Example of  a natural gamma spectroscopy log presentation.




                  uranium and thorium. Thus, shales typically have high radioactivity. Sandstones
                  (quartzose), carbonates and evaporites have  strong bonds and generally do not
                  allow impurities. Limestones undergo  rearrangement of  crystal structure  and
                  addition of  magnesium to become dolomites. Impurities like uranium (which is
                  very  soluble) may  enter the  crystal lattice during recrystallization. Feldspathic
                  sandstones contain an abundance of  potassium40  and  therefore  show  higher
                  radioactivity than quartzose sandstone. Some evaporite minerals (such as KC1)
                  contain high amounts of potassium40 and may appear as shales on the log. Serra
                  et al.  [207]  provide an excellent discussion of  interpretation  of  the natural  or
                  spectral gamma-ray tool.

                  Sonic (Acoustic) Log. The sonic (acoustic or velocity) tool measures the time
                  it takes for a compressional wave to travel through one vertical foot of formation.
                  It can be used to determine porosity (if the lithology is known) and to determine
                  seismic velocities for geophysical surveys when combined with a density log. The
                  sonic log also has numerous cased hole applications.
                  Theow. A 20 khz sound wave  is produced by  the tool and travels through the
                  mud into the formation. The wave travels vertically through the formation. The
                  first arrival of  the compressional wave is picked up by  a receiver about one foot
                  away  from the  transmitter. The wave  continues through  the formation and is
                  picked up by  the far receiver (normally 2-ft below  the ne& receiver). The time
                  difference between the near  and far receivers is  used  to determine formation
                  travel time  (At). Fractures, vugs, unconsolidated formations, gas-cut mud, lost
                  circulation materials, and rough boreholes can cause sharp increases in At, called
                  cycle  skips.
                  Interpretation. Table 5-26 shows the velocity and travel time for several commonly
                  encountered oilfield materials. The  tm value in  the  fourth  column  is  at  0%
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