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                          3.2.1.2.1.4.2. Equation for calculation of wetted and effective surface areas
                                  For determination of the wetted surface area the following equation is
                          suggested [83, 84]:



                           i L       m
                           ^  = l-K Ie-                                                      (93)
                            a

                          where:


                           m = bRef                                                          (94)



                                  The experimental constants in this equation are as follows:
                                                        Lp L           Z       b         P
                          Rings 15-35 mm [85]           0.028-8.3      1.02    0.16      0.4
                           Rings 15 mm [86]             0.17-5.5       1.0     0,167     0.415
                           Saddles 15 mm [86]           0.17-5.5       1.0     0,089     0.7


                                  It is not correct from the similarity theory point of view to use
                           Re L instead of L, without changing the viscosity, for obtaining of these
                           experimental constants. The Buckingham theorem requires in this case 4
                           dimensionless values, but not only two.
                                  Hikita and Kataoka [69] based on their own experimental data obtained
                           with paper Raschig rings, using the colour method described in 2.1.2.5.1,
                           proposed the equation:



                                     ( f()                                                  (95)
                                     L
                            a


                           where m =        ^
                                  The mass liquid superficial velocity L.p L for obtaining of this equation
                                                         2  1
                           is changing from 0.14 to 5.6 kg m'  s .
                                  Using data from different investigators, Bolshakov and Grinevieh [98]
                           obtained the equation:
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