Page 134 - Handbook Of Multiphase Flow Assurance
P. 134

130                        5.  Flow restrictions and blockages in operations

                            1000











                             100

                           Pressure (bar)  4








                             10











                              1
                               –10    –5      0      5     10     15     20     25     30
                                                      Temperature (°C)
                 FIG. 5.23  Hydrate stability conditions. Redrawn from Makogon Y.F., Sarkisyants G.A., 1966. Prevention of Hydrate
                 Formation in Production and Transport of Gas. Nedra Publisher, Moscow, 188 pp.


                   We reproduce the Katz method in Fig. 5.23 below to facilitate a quick estimate of hydrate
                 stability from known gas gravity in absence of a computer software or a calculator. As a check
                 point, methane hydrate stability at 0 °C is 26 bar.
                   Makogon and Shalyaho (1972) and  Makogon (1974, 1981, 1997) provided a simple
                 equation  method  for  the  gas  specific  gravity  range  of  0.6–1  for  hydrocarbon  hydrates
                 from 0 to 25 °C:
                                                                  kT C]) )
                                                             ° [ (
                                           [
                                       logP bar] = β + 0 0497  TC]+ (  ° [  2
                                                      .
                   Graphs for the coefficients β and k were digitized and fitted by Elgibaly and Elkamel (1997)
                                                    −
                                                               .
                                                      .
                                                .
                                            β = 2 681 3 811SG +1 679SG 2
                                                     +
                                                                .
                                            k  =−0 006 0 011SG + 0 011SG 2
                                                 .
                                                       .
   129   130   131   132   133   134   135   136   137   138   139