Page 182 - Introduction to Petroleum Engineering
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POROSITY LOGS                                                   169
              An estimate of the speed of sound v in a formation is given by Wyllie’s equation.
            If we write the speed of sound in fluids occupying the pore volume of a rock as v  and
                                                                           f
            the speed of sound in the rock matrix as v , Wyllie’s equation is
                                             ma
                                                −
                                       1  =  φ ( 1 φ)                      (9.3)
                                             +
                                       ν  ν f  ν ma
            where ϕ is rock porosity. We can write the speed of sound in each medium as the
            distance traveled divided by the transit time. If we assume the distance traveled is the
            same in each medium, then Wyllie’s equation can be written as

                                     ∆t = φ ∆t +(1 −φ  ∆t )  ma            (9.4)
                                           f
            where Δt is transit time in the bulk volume, Δt  is transit time in the interstitial fluid,
                                                 f
            and Δt  is transit time in the rock matrix. Porosity in the bulk volume is obtained by
                 ma
            rearranging Equation 9.4:
                                           ∆t  − ∆t
                                        φ =      ma                        (9.5)
                                           ∆t f  − ∆t ma
              In addition to providing a measurement of porosity, acoustic logs can be used to
              calibrate seismic measurements. The comparison of acoustic and seismic transit time
            measurements in a formation can improve the accuracy of converting seismic transit
            times to depths.
              The depth of investigation for sonic logs is typically 1–4 ft.


              Example 9.3  Acoustic Log

                                                              −
              An acoustic log measured the transit time of 75µs =  7510 s in a formation.
                                                           ×
                                                              6
                                                           ×
              The formation matrix has a transit time of 50µs =  50 10 s, and the fluid
                                                              −
                                                               6
              transit time is 185µs = 185 10 s. Use Equation 9.5 to calculate porosity.
                                       −
                                    ×
                                        6
              answer
                     ∆t  − ∆t   75  − 50
              Use φ =      ma  =      = 0 185.   or 18.5%
                     ∆t  − ∆t  185  − 50
                       f   ma
            9.3.3  Neutron Logs
            The  neutron  log  provides  information  about  the  formation  by  emitting  neutrons
            from a radioactive source in the logging tool. The emitted neutrons lose energy as a
            result of collisions with atomic nuclei in the formation to become slower thermal
            neutrons. Slower neutrons can be captured by nuclei in the formation. Hydrogen
            nuclei are especially effective at capturing thermal neutrons. Reservoir fluids (oil,
            water, and hydrocarbon gas) contain hydrogen while formation rock usually does
            not. Consequently, the detection of captured neutrons by the neutron logging tool
            indicates porosity.
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