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Example 2
                     Natural gas, saturated with water vapor at conditions of

                     1000 psia and 90 F is exposed to cooling in a flow line due to
                     heat losses, where the temperature reaches 35 F and the pressure

                     remains the same.
                     (a)  Calculate how much liquid water will drop out of the gas.
                     (b)  Assuming that the gas flowing through the pipeline is to
                          reach a delivery point at 300 psia pressure, find the corre-
                          sponding dew point of the gas.

                     Solution

                     (a)  From Figure 2, we obtain the following:
                         Water content of the gas stream at the initial conditions

                           (1000 psia and 90 F) is 46 lb/MMCF (MMCF: 10 6 cubic
                           feet).
                         Water content of the gas stream at conditions of 1000 psia

                           and 35 F is 7.6 lb/MMCF.
                         Water   to  be  separated  is  46   7.6 ¼ 38.4 lb/MMCF
                           (MMCF: 10 6 cubic feet).
                     (b)  The natural gas, once it reaches the delivery point at 300 psia,
                          carries with it a water content of 7.6 lb/MMCF. Applying
                          these two parameters to Figure 2, one can read the dew point
                          temperature of 12 F.


            12.2.2  Analytical Methods

            The calculations presented in this section are concerned with finding
            the hydrate formation temperature T at a given pressure P, or the pressure P
            at which hydrate formation takes place for a given operating temperature
            T. A knowledge of the temperature and pressure of a gas stream at the
            wellhead is important for determining whether hydrate formation can be
            expected when the gas is expanded into the flow lines. In general, the
            temperature at the wellhead can change as the reservoir conditions or
            production rate change over the production life of the well. Wells,
            therefore, that initially flowed at conditions where no hydrate formation
            occurred in downstream equipment may require hydrate inhibition, or vice
            versa. The computational approach is analogous to the one used in the






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