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Project No. D-3885-06 <br />Christ Our Savior Catholic Parish <br />We have used this method and the results of the liquefaction study including depth vs. <br />factor of safety, soil behavior type, and cyclic stress ratio, based on the site profile are <br />presented in Appendix E. <br />In accordance with the latest USGS Design Maps in the 2010 ASCE-7 Standard for Risk <br />Category I/llllII, adjusted for other site class D,5% Damped Design Spectral <br />Acceleration at short period, Sp5 is l.02lg and Sp1 for long period is 0.5689. Liquefaction <br />is generally analyzed for Sp5/2.5 = 0.41g or 0.586 g from Figure 22-7 (USGS, Design <br />Maps) or 2% probability of exceedance in 50 years is 0.78529 in accordance with <br />U.S.G.S. National Seismic Hazard Mapping Project PSH Deaggregation Interactive <br />program, and 213 rd of 0.78529 = 0.5239. Thus, as per USGS Design Maps, Figrre 22-7 <br />of 0.5869 is more conservative and has been used in liquefaction analysis. <br />Liquefaction analyses have been performed for earthquake magnitude of M6.6 and <br />ground acceleration of 0.59g. Historical high groundwater depth was considered as 5 feet <br />below the existing ground surface. Results of the liquefaction study including depth vs. <br />factor of safety and estimated settlements for liquefiable layers based on generalized soil <br />profile for CPT's and borings are all presented in Appendix E. <br />Liq uefaction-Ind uced Settlement of Saturated Soils <br />t7 <br />l <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />t <br />I <br />I <br />T <br />I <br />I <br />I <br />u <br />As a result of liquefaction, the proposed structure may be subject to several hazards <br />including liquefaction-induced settlement. In order to estimate the amount of post- <br />earthquake settlement, the method proposed by Tokimatsu and Seed (1987) was used in <br />which the seismically induced cyclic stress ratios and corrected N-values are related to the <br />volumetric strain of the soil. The amount of soil settlement during a strong seismic event <br />depends on the thickness of the liquefiable layers, the density and/or consistency of the <br />soils and groundwater level. Computer analysis of estimated settlement, based on data <br />from SPT and Cone Penetration tests are presented in Appendix E. <br />E <br />r