Page 84 - Fundamentals of Reservoir Engineering
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SOME BASIC CONCEPTS IN RESERVOIR ENGINEERING                          23

                     the derivative of which, with respect to pressure, is

                           ∂ V  =−  ZnRT      1  −  1 ∂ Z

                           ∂ p         p      p    Z ∂  p


                     and substituting these two expressions in the isothermal compressibility definition,
                     equ. (1.11), gives

                                    1 ∂ V     1     1 ∂ Z
                           c =−            =     −                                                  (1.31)
                            g
                                    V  ∂ p    p     Z ∂ p
                     In fig. 1.9, a plot of the gas compressibility defined by equ. (1.31) is compared to the
                     approximate expression.

                                 1
                           c =                                                                      (1.32)
                            g
                                 p
                     for the 0.85 gravity gas whose isothermal Z−factor is plotted in fig. 1.8 at 200°F. As can
                     be seen, the approximation, equ. (1.32), is valid in the intermediate pressure range
                     between 2000−2750 psia where ∂Z/∂p is small but is less acceptable at very high or
                     low pressures.


                     EXERCISE 1.1 GAS PRESSURE GRADIENT IN THE RESERVOIR

                     1)   Calculate the density of the gas, at standard conditions, whose composition is
                          listed in table 1.1.
                     2)   what is the gas pressure gradient in the reservoir at 2000 psia and 180° F
                          (Z = 0.865).


                     EXERCISE 1.1 SOLUTION

                     1)   The molecular weight of the gas can be calculated as


                                M =     nM =   19.91
                                         i
                                           i
                                       i
                          and therefore, using equ. (1.28) the gravity is
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