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Chapter 3 Loah and Dynamic Response for offshore Structures           49




























                             Figure 3.6   A FPSO System and Coordinates for Wave Directionality
                                         and Wave Spreading

                  3.4.2   Response Amplitnde Operator (RAO)
                  A wave scatter diagram provides a  long-term wave  description for only one specific site.
                  Determining the stress Frequency Response Function (FRF) or Response Amplitude Operator
                  (RAO), H  (0; an,&) is one of the major efforts in the strength assessment, because it allows
                  the  transfer of  the  exciting waves  into the  response of  structures. This concept  of  linear
                  dynamic theory is applicable to any type of oscillatory "load" (wave, wind-gust, mechanical
                  excitation, etc.) and any type of "response" (motion, tension, bending moment, stress, strain
                  etc.).
                  For a linear system the response function at a wave frequency can be written as
                        Response(t) = RAO.q(t)

                  where V(t) denotes the wave profile as a function of time t. The RAO could be determined
                  using theoretical computation or experimental measurement (Bhattacharyya, 1978). Almost all
                  of the theoretical computation has neglected viscosity and used potential flow.
                  The structure may be envisaged in a general terms as a ''black box",  see Figure 3.7. The input
                  to the box is time-history of loads and the output from a structural analysis is time-history of
                  the  response.  The  basic  assumption  behind  the  RAO  concept  is  linearity,  that  allows
                  superimpose the output based on superimpose of the input. In these situations, the response to
                  regular oscillatory loading of any waveform  can be  obtained by expressing the  load  as a
                  Fourier series, and then estimate the corresponding Fourier series of the response for each
                  component. A typical RAO is shown in Figure 3.8, that is a roll RAO of a barge in beam seas.
                  The RAO is given in degrees (or meters/A)  of motion amplitude, per meter (or A)  of wave
                  amplitude and expressed as a function of wave period (second). The RAO may be calculated
                  using the first order wave theory as wave fkequency response.
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