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SHANNON 6WILSON,INC. <br /> historical earthquakes to create a relationship between soil density and liquefaction potential. <br /> The ability of a soil to resist liquefaction is expressed as a cyclic resistance ratio (CRR). The <br /> demand placed on the soil deposit by seismic loading is expressed as the cyclic stress ratio <br /> (CSR). The FS against liquefaction is the ratio of the CRR to the CSR. The results of the <br /> liquefaction analysis are present in Appendix C for the IBC ground motion and the 200-year <br /> design ground motion. <br /> We estimated the FS against liquefaction of each soil SPT sample between the <br /> groundwater table (estimated at+11 feet) and elevation -12 feet (a total of 21 samples from all of <br /> the borings performed for this project) for a variety of earthquake ground motion levels using the <br /> empirical methods discussed above. A summary of our analyses is shown in the following table: <br /> Surface <br /> Earthquake Return Peak Ground Moment Percent of Samples <br /> Period(years) Acceleration (g) Magnitude that Liquefy <br /> 100 0.18 6.4 10 <br /> 200 0.25 6.5 20 <br /> 224 0.26 6.5 30 <br /> 475 0.33 6.5 50 <br /> 975 0.39 6.5 60 <br /> 2475 0.48 6.5 70 <br /> Based on the above analyses, a 200-year return period ground motion selected by the Port <br /> for this project would represent a condition where about 20 percent of the samples within the fill <br /> and alluvium would liquefy. The results of the liquefaction analyses for the 200-year design <br /> ground motion are included in Appendix C. Based on these results, localized zones within the <br /> upper fill and alluvium deposits may liquefy during the 200-year design ground motion. <br /> Potential liquefaction in borings B-2, B-3C, and B-4 (Segments A. B. and C) is limited to one <br /> sample per boring for the 200-year design ground motion. Based on these results, the <br /> liquefaction would be localized and minimal and,therefore, can be neglected in our analyses, in <br /> our opinion. <br /> The relative density of the fill and alluvium soil sampled at boring B-1 B (Segment D) is <br /> less than that observed in Segments A, B, and C. Our analyses indicate that more liquefaction <br /> would occur in this area than along segments A, B and C. If bulkhead design for Segment D is <br /> pursued in the future, we recommend performing additional explorations along the Segment D <br /> alignment to confirm the relative density of the soils and evaluate the potential for liquefaction <br /> 21-i-?nv 1-ou 3-R i 1A10C./"J)rC q, 21-1-21761-003 <br /> 9 <br />