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                  200,
                N









          (153.73 cm/se?j  I
                 -200   I                          Time in seconds -
                     0              5             10            15             20            25

                      Peak ground acceleration = 0.15 g   'This  can be determined by drawing a Fourier spectrum, which
                      Predominant frequency*  = 2 Hz   would identify the fundamental frequencies that build up the
                                                       multi-frequency spectrum.
                                                     (a) Acceleration












                                                   Time in seconds -
                  -8"   I
                     0              5             10             15            20             25
                                                      (b) Velocity
                   lo 1










                                                   Time in seconds -
                  -10  I
                     0              5             10             15            20             25

                                                    (c) Displacement
                     Figure 14.12(b)  Time history of  earthquake at Charnoli, India, which occurred in March 1999


         3  Ground acceleration  response  spectrum in  terms  of   the basis of  equipment design and their seismic testing
           spectral acceleration, g, versus natural period of oscilla-   and are provided by the user to the equipment manufac-
           tions (Figure 14.16).                       turer.
                                                         In the above instance, the response spectra shown in
         These spectra represent the nature of peak displacement/   Figures  14.14-14.16  are for 5% damping. The damping
         velocity/forces  and their magnitudes that may generate   levels described here are generally in the range  1-10%
         in  a  vibrating  system of  different  damping  levels  and   and frequency in the range  of  1-33  Hz for systems at
         periods on the occurrence of  an earthquake. They form   ground level and 0.5-10  Hz for floors above the ground
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