Page 318 - Petrophysics 2E
P. 318

FORMATION EVALUATION             289


                             The Rwa  technique gives excellent results when drilling fluid (mud)
                           invasion  is  not  deep,  as  in  the  high-porosity formation,  or  when
                           low-water-loss mud  is  used.  This  technique,  however,  can  yield
                           pessimistic results when formation is shaly and FR is determined from
                           the density log,


                             Porosity
                             Three  logging  porosity  tools  have  been  developed  to  determine
                           porosity, namely, the sonic-acoustic log, the formation density log, and
                           the neutron porosity log. In addition to porosity, these logs are affected
                           by other parameters, such as lithology, nature of  the pore fluids, and
                           shaliness. Combinations of  these logs are used to determine lithology
                           and porosity as well as the fracture porosity.
                             The sonic log measures the interval transit time, At, i.e., the shortest
                           time required for a compressional sound wave to travel through one foot
                           of formation parallel to the wellbore. The speed of sound in the formation
                           depends on the nature of minerals making up the rock, porosity, pore
                           space fluids, temperature, pressure, and rock texture. Inasmuch as for
                           any given lithology the zone of investigation of the sonic tool is essentially
                           in the invaded zone containing mud filtrate, the speed of sound, i.e., the
                           interval transit time, is primarily a function of porosity.
                             The velocity of  sound in the formation depends on the density and
                           elastic properties of  the medium,  such as bulk  and  shear moduli of
                           elasticity. It is faster in a hard substance than in a liquid. Hence, if one
                           considers a rock composed of only solid and liquid, the following ratio
                           of the transit times can be used to obtain porosity 1491  :


                                                                                       (4.150)



                           where:  t  = total transit time, ps/ft.
                                  tma  = matrix travel time, p~/ft.
                                   tfl = fluid travel time, ps/ft.


                             Equation 4.150 is commonly used for determining the approximate
                           value  of  porosity of  clean consolidated sandstones as well  as  that  of
                           carbonate formations with intergranular porosity. The fluid travel time is
                           approximately  190 ps/ft, whereas the matrix travel time can be obtained
                           from the following equation:



                                                                                       (4.1 5 1)
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