Laserfiche WebLink
V <br /> Geotechnical Engineering Report 3 January 7,2020 <br /> QFC 852 Fuel Station,Everett, Washington RGI Project No.2019-258A <br /> variations in the amount of rainfall, runoff, and other factors not evident at the time the <br /> explorations were performed. In addition, perched water can develop within seams and <br /> layers contained in fill soils or higher permeability soils overlying less permeable soils <br /> following periods of heavy or prolonged precipitation. <br /> 4.5 SEISMIC CONSIDERATIONS <br /> Based on the 2015 International Building Code (IBC), RGI recommends the follow seismic <br /> parameters in Table 1 be used for design. <br /> Table 1 IBC Seismic Parameters <br /> 2015 IBC Parameter Value <br /> Site Soil Class' DZ <br /> Site Latitude 47.952457° N <br /> Site Longitude 122.21214°W <br /> Maximum considered earthquake spectral response <br /> acceleration parameters (g) Ss=1.371, S1 =0.521 <br /> Spectral response acceleration parameters adjusted for site <br /> Sms =1.371, Smt =0.781 <br /> class (g) <br /> Design spectral response acceleration parameters (g) Sds =0.914, Sd1 =0.521 <br /> 1 Note: In general accordance with the USGS 2015 International Building Code. IBC Site Class is based on the average characteristics <br /> of the upper 100 feet of the subsurface profile. <br /> 2 Note:The 2015 International Building Code requires a site soil profile determination extending to a depth of 100 feet for seismic <br /> site classification. The current scope of our services does not include the required 100 foot soil profile determination. Borings <br /> extended to a maximum depth of 31.5 feet, and this seismic site class definition considers that similar soil continues below the <br /> maximum depth of the subsurface exploration. <br /> Liquefaction is a phenomenon where there is a reduction or complete loss of soil strength <br /> due to an increase in water pressure induced by vibrations from a seismic event. <br /> Liquefaction mainly affects geologically recent deposits of fine-grained sands that are <br /> below the groundwater table. Soils of this nature derive their strength from intergranular <br /> friction. The generated water pressure or pore pressure essentially separates the soil <br /> rains and eliminates this inter ranular friction thus reducin or eliminatin the soil s <br /> g g g g <br /> strength. <br /> RGI reviewed the soil conditions encountered during field exploration and assessed the <br /> potential for liquefaction of the site's soil during an earthquake. Due to the dense nature <br /> of the deposits and depth of ground water level, RGI considers the potential for <br /> liquefaction of the site soils to be minimal. <br /> i- <br /> RILEYGROUP <br />