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50                                            Part I Liquid Drilling Systems


           Calculating surge and swab pressures can be a complex undertaking,
        depending on the pipe configuration and the hole geometry. Burkhardt
        (1961) developed a relationship between well geometry and the effect of
        the fluid being dragged by the pipe. Based on Burkhardt’swork,the
        effective annular velocity is equal to
                                                                    (2.80)
                                   v e = v m − κv p
        where

           v e = effective annular velocity, ft/s or m/s
           v m = mud velocity, ft/s or m/s
           v p = pipe velocity, ft/s or m/s

        and κ is referred to as the clinging constant, which is a function of
        annular geometry. Burkhardt presented a chart for determining the value
        of κ in both laminar flow and turbulent flow. We found that the chart
        can be replaced by the following correlations with minimal error. For
        laminar flow, the correlation is

                                         d p
                               κ = 0:275    + 0:25                  (2.81)
                                         d h
        where

           d p = outer diameter of pipe, in or mm
           d h = hole diameter, in or mm
        For turbulent flow, the correlation is


                                        d p
                                κ = 0:1    + 0:41                   (2.82)
                                        d h
        For closed-end pipes, such as a casing string with a float shoe, the mud
        velocity can be calculated by
                                             2  !
                                            d
                                             p
                               v m = − v p  2  2                    (2.83)
                                          d − d
                                           h   p
        For open-end pipes, the mud velocity can be calculated by

                                       2       2    4   !
                                     4d ðd h − d p Þ − 3d
                                       p            p
                       v m = − v p         2  2                     (2.84)
                                                  2
                                   2
                                 4d ðd h − d p Þ ðd − d Þ + 6d 4
                                   p          h   p     p
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