12.07.2015 Views

Report - PEER - University of California, Berkeley

Report - PEER - University of California, Berkeley

Report - PEER - University of California, Berkeley

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Table 1. — ContinuedM12M13M14M15M3 equipped with viscoelastic seismic isolation bearings;isolated period is 3.5 seconds; approximately 10% <strong>of</strong> criticaldamping in the first mode.M3 equipped with viscoelastic seismic isolation bearings;isolated period is 3.5 seconds; approximately 20% <strong>of</strong> criticaldamping in the first mode.M3 equipped with coupled bilinear seismic isolation bearings:Qd= 0.06W; second-slope isolation period is 2.5 seconds;isolator yield displacement is 25 mm.M3 equipped with coupled bilinear seismic isolation bearings:Qd= 0.06W; second-slope isolation period is 3.5 seconds;isolator yield displacement is 25 mm.1. First mode period in transverse (short) direction.2. Period calculation based on second slope (post-yield) isolator stiffness.3.573.572.60 13.57 1Preliminary results are presented in this paper for 11 <strong>of</strong> the 15 models: M3, M6,M7, M8, M9, M10, M11, M12, M13, M14 and M15. Seismic demands on NCCs inthe 11 buildings was assessed by nonlinear response-history analysis in the transverse(north-south) direction only. The earthquake histories used for the response-historyanalysis were those generated for a NEHRP Soil Type S D (firm soil) site in LosAngeles as part <strong>of</strong> the SAC Steel Project (Sommerville et al. 1997). Three bins <strong>of</strong> 20histories were developed, each representing a different probability <strong>of</strong> exceedance (2%in 50 years, 10% in 50 years and 50% in 50 years). The response spectrum for eachhistory in the 10% in 50 year (hereafter denoted 10/50) bin is shown in Figure 4a. Themedian, 16th and 84th percentile spectra are shown in Figure 4b together with thetarget spectral ordinates (shown circled) at periods <strong>of</strong> 0.3, 1, 2 and 4 seconds, toprovide the reader with information on the variability in the earthquake histories usedin the response-history analysis.Spectral acceleration (g)432100 1 2 3 4Spectral acceleration (g)432100 1 2 3 4a. response spectra b. 10/50 spectral dataFigure 4. Binned 10/50 ground motion data for response-history analysis.118

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!