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1,2 GROIINDWATERCONDITIONS <br />Fluctuations of the groundwater level, localized zones of perched water, and soil moisture <br />content should be anticipated during and tbllowing the rainy season. Irrigation of landscaped <br />areas on or adjacent to the site can also cause a fluctuation of soil moisture content and local <br />groundwater levels. <br />4.3 SOIL EN(;INEERINC PROPERTIES <br />Physical tests were performed on the relatively undisturbed samples to characterize the <br />engineering properties ofthe native soils. Moisture content and dry unit weight determinations <br />were performed on the samples to evaluate the in-situ unit weights of the different materials. <br />Moisture content and dry unit weight results are shown on the boring logs in Appendix A. <br />5.0 STRONG GROUND MOTION POTENTIAL <br />The project site is located in a seismically active area typical of Southem California and likely <br />to be subjected to a strong ground shaking due to earthquakes on nearby faults. <br />5,I CBC DESIGN PARAMETERS <br />The project site is located in a seismically active area typical of Southem Califomia and likely <br />to be subjected to a strong ground shaking due to earthquakes on nearby faults. <br />To accommodate effects of ground shaking produced by regional seismic events, seismic <br />design can, at the discretion of the designing Structural Engineer. be performed in accordance <br />with the 2019 edition of the California Building Code (CBC). Table below, 2019 CBC Seismic <br />Parameters, lists (next) seismic design parameters based on the 201 9 CBC methodology, which <br />is based on ASCE/SEI 7- I 6: <br />Dennis- l -0'l <br />Groundwater was encountered within our exploratory boring B-l at an approximate depth of l0 <br />feet bgs. Based on information from the Califomia Geological Survey (Califomia Division of <br />Mines and Geology, 1997). the historic high ground water level in the site vicinity is at a depth <br />of approximately 5 feet beneath the existing ground surface. <br />3