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Lutzky Associates Development, LP - Geolechnical Investigation <br />MACTEC Project 4953-03-2631 <br />September 18. 2003 <br />6.6 TIME HISTORIES <br />Spectral Matching Procedure <br />The computer program RSPMATCH (Abrahamson, 1998) was used to perform time-domain <br />spectral matching of¥ seven orthogonal sets of horizontal time hi@ories. The spectral matching <br />procedure modifies the empirically recorded (initial) time histories usually by adding a tapered <br />cosine wave so that the response spectrum of the modified time history and the target spectrum <br />match. <br />For each period, the time of the maximum response is computed for the initial (unmodified) time <br />history. A tapered cosine wave is then added at that computed time to either increase or decrease <br />the spectral response and match the target spectrum for the specific period. The initial phasing of <br />the time history can be maintained because the modification for each period is applied at the time <br />of maximum spectral response rather than throughout the entire time history, as is done in <br />frequency-domain spectral matching. The spectral matching was performed for the DBE and the <br />UBE design response spectra with 5% damping. <br />Spectral Matching Procedure <br />We performed spectral matching for the DBE and UBE level earthquake in accordance with the <br />Appendix 16A of the California Building Code, 2001 edition. De-aggregation results for the PGA <br />(zero spectral period) indicate that seismic events from strike-slip and reverse-oblique faults with <br />magnitudes ranging from 5 to 7 at distances of about six kilometers or nearer are the predominant <br />contributors to the seismic shaking hazard of the project site. <br />The seven time histories selected for matching are presented in Table 6, Empirical Time Histories <br />Selected for Spectral Matching. <br />These records were selected based on the following factors: robust long-period content, inclusion <br />of strong directivity or near-source ground motions, and the results of de-aggregation of <br />probabilistic seismic hazard. <br />23