Page 321 - Petrophysics 2E
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292    PETROPHYSICS: RESERVOIR ROCK PROPERTIES



                   The bulk density, Pb in g/cm3, is read from the density log. The density
                   of fluid in pores, generally mud filtrate, is 1 .O when fresh muds are used
                   and 1.1 for salty drilling muds. If the formation is saturated with gas in the
                   vicinity of the borehole, Le., little or no mud invasion,   = 0.7 g/cm3
                    [25]. In shaly (clayey) formations Equation 4.157 becomes [43]
                                                                              :

                                                                               (4.158)


                    Determining porosity, especially in carbonate rocks, is one of  the most
                    important applications of  neutron logs. These rocks generally contain
                    smaller amounts of clay minerals than the sandstones. Neutron logs also
                    can be used to define bed boundaries and, when used in conjunction
                    with other logs, as an indicator of lithology of gas-bearing zones. Modern
                    neutron log data is recorded directly in apparent porosity units with only
                    a minor correction, required to account for salinity, temperature, and
                    tool positioning. Porosity can be determined from the combination of
                    neutron and density logs using Equation 4.96. The presence of shale (clay)
                    in reservoir rocks (sandstone, limestone, or dolomite) will influence to
                    some degree the measured response of all three porosity logs.
                      As previously stated, the standard practice at present for estimating
                    the reservoir permeability distribution is to combine permeability values
                    obtained from laboratory measurements  on cores with logderived param-
                    eters, such as porosity and water saturation. The following summary of
                    a field case is a typical example of such practice [50].

                    EXAMPLE


                    The Howard-Glasscock  field is located south of  Big Spring, Texas, and
                    has produced oil from the lower Grayburg and San Andres carbonate
                    formations since 1929. The 80-well field was unitized in 1972 and, during
                    1973,40 additional wells were drilled to expand the ongoing waterflood,
                    which was initiated in 1964. Ten wells were cored and 38 wells were
                    logged. The objective is essentially to [50]:

                    (a)  calculate  average  values  of  permeability,  porosity  and  water
                       saturation,
                    (b)  prepare contour maps of porosity and water saturations, and
                    (c)  estimate oil reserves.


                      Core Interpretation of Data
                      The  core recovery  efficiency was  98.2% or  an  average  of  404.5ft
                    of  core  recovered per 411.8ft attempted per well.  This  recovery is
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