Page 539 - Petrophysics
        P. 539
     506    PETROPHYSICS: RESERVOIR ROCK PROPERTIES
                    SOLUTION
                      Using Equation 4.5 the formation resistivity factor is:
                        Ro     1.77
                    F=-=--          - 50.57
                        Rw    0.035
                    The tortuosity is calculated from Eq. 8.8b:
                    z = F ((1 - @?>$:"'  + @?)
                     = (50.57) ((1 - 0.0371.5)(0.152) + 0.0371.5) = 1.5
             POROSITY PARTITIONING COEFFICIENT
                      Reservoirs with a fracture-matrix porosity system-such  as found in
                    many carbonate rocks due to the existence of vugs, fractures, fissures,
                    and joints-differ  considerably from reservoirs having only one porosity
                    type. The secondary porosity strongly influences the movement of fluids,
                    whereas the primary pores of  the matrix, where most of  the reservoir
                    fluid is commonly stored (more than 96% in Type-3 naturally fractured
                    reservoirs), are poorly interconnected. The Spraberry field of West Texas
                    is  an  example of  a naturally fractured sandstone oil reservoir, which
                    is composed of  alternate layers of  sands, shales, and limestones. The
                    Altamont trend oilfield  in Utah is another naturally fractured sandstone
                    reservoir with a porosity of 3% to 7% and an average matrix permeability
                    less than 0.01 mD [13].
                      Laboratory-measured values  of  permeability for  naturally fractured
                    cores can be  significantly different from the in-situ values determined
                    by well pressure analysis. The difference is attributed to the presence of
                    fractures, fissures, joints and vugs, which are not adequately sampled in
                    the core analysis. One of the earliest methods used to analyze full-sized
                    naturally fractured cores was developed by Locke and Bliss  [30]. The
                    method consists of  injecting water into a core sample and measuring
                    the pressure values as a function of the cumulative injected volume of
                    water (Figure 8.11). The secondary pore space, Vf, because of  its high
                    permeability, will be the first to fill up with water. A sharp increase in
                    pressure is recorded later, indicating that the matrix porous space, V,,
                    has to fill up. The total pore volume, Vt  = Vf + @fVm, is considered to
                    be fdled up when a pressure of  1,000 psi is reached in the test. If  the
                    fraction of total pore volume in the secondary porosity is v, then:
                                  vc
     	
