Page 104 - Theory and Design of Air Cushion Craft
P. 104

Steady drag forces







                                                            channel width greater than
                                                             10/ c and infinite depth

























                                                                                 8 /B c
                                                                                   l c
              Fig.  3.3  Cushion wave-making  drag coefficient  for  a rectangular  air cushion  over  calm water against  L CIB C.



              predicting  the  other  components  of  drag  also  developed  by  the  same  authors,  e.g.
              when  one  uses the equation  (3.4) for estimating the wave-making drag,  it is better  to
              use this together with the other formulae offered  by ref.  19 for estimating the seal drag,
              sidewall water friction  and  the residual drag of  sidewalls, otherwise the user may find
              inconsistencies  in calculation  of  the total  resistance of  the ACV.
                Owing to  the easy application  and  accuracy  of  Newman's  method,  MARIC  often
              uses Newman  and  Poole's  data  for estimating  the wave-making resistance  of  craft.  It
              is evident from  this work that  the bow wave strongly interacts with the stern wave. The
              lower  the cushion  beam  ratio,  the  stronger  the disturbance  between  the  two  compo-
              nents. This causes a series of  peaks and  troughs  on the resistance  curve. With respect
              to  water with infinite  depth,  the  last peak  appears  at  Fr  —  I/A/TT = 0.56.
                The theory mentioned  above was validated by the experimental results carried  out
              by Everest  and  Hogben  [20]. The  theoretical  prediction  agreed  quite  well with  exper-
              imental  results except at low speed.  In  this latter  case,  only two pairs  of  troughs  and
              peaks  appeared  in the test results rather  than  that  in the calculation  results. This  can
              be interpreted  as  follows:
              •  Hogben  proposed  that  the  wave  steepness  (hiA)  at  lower  Fr  predicted  by  linear
                theoretical  calculation  exceeded  the  theoretical  limit  value  of  1/7  between  the
                troughs  and  peaks,  so that  the  surface  geometry  would  be  unstable,  similar  to  a
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