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625 Cypress Avenue <br />Geotechnical Investigation <br /> <br />Project No. W1895-88-01 - 11 - April 23, 2024 <br />the ground acceleration and duration of the earthquake must also be of a sufficient level to induce <br />liquefaction. <br />A review of the State of California Seismic Hazard Zone Map for the Tustin Quadrangle indicates that <br />the site is located within an area designated as having a potential for liquefaction. Groundwater was <br />encountered during our site exploration at a depth of 49½ feet below ground surface. The historic high <br />groundwater level in the area is reported to be between 30 and 40 feet beneath the existing ground <br />surface (CDMG 2001). <br />Liquefaction analysis of the soils underlying the site was performed using the 1996 NCEER method <br />of analysis with the updates by Youd et al. (2001). This semi-empirical method is based on a <br />correlation between values of Standard Penetration Test (SPT) resistance and field performance data. <br />To supplement the SPT blow count data, California Modified Sampler blow count data was converted <br />to equivalent SPT blow counts based on a correlation factor of 0.55 (Rogers, 2006). <br />Screening criteria developed by Bray and Sancio (2006) characterize fine-grained soils which are not <br />susceptible to liquefaction as soils with a plasticity index (PI) that is greater than 18 or with a saturated <br />moisture content that is less than 80 percent of the liquid limit. In order to apply the screening criteria, <br />laboratory testing was performed to evaluate the Atterberg Limits and saturated moisture content of <br />select soil samples. Laboratory test results used for the screening criteria are presented as Figure B16. <br />The liquefaction analysis was performed for a Design Earthquake level by using a historic high <br />groundwater table of 35 feet below the ground surface, a magnitude 6.47 earthquake, and a peak <br />horizontal acceleration of 0.434g (⅔PGAM). The enclosed liquefaction analysis, included herein for <br />boring B1, indicates that the alluvial soils below the historic high groundwater level could be susceptible <br />to approximately 0.3 inch of total settlement during Design Earthquake ground motion (see enclosed <br />calculation sheets, Figures 13 and 14). <br />It is our understanding that the intent of the Building Code is to maintain “Life Safety” during Maximum <br />Considered Earthquake level events. Therefore, additional analysis was performed to evaluate the <br />potential for liquefaction during a MCE event. The structural engineer should evaluate the proposed <br />structure for the anticipated MCE liquefaction induced settlements and verify that anticipated <br />deformations would not cause the foundation system to lose the ability to support the gravity loads <br />and/or cause collapse of the structure. <br />The liquefaction analysis was performed for the Maximum Considered Earthquake level by using a <br />historic high groundwater table of 35 feet below the ground surface, a magnitude 7.3 earthquake, and <br />a peak horizontal acceleration of 0.651g (PGAM). The enclosed liquefaction analysis, included herein for