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Proposal for Geotechnical Engineering Services <br />Proposed Bank: 1515 132nd Street Southeast, Everett, Washington <br />March 15, 2019 <br />4.0 INFILTRATION CONSIDERATIONS <br />The native soils underlying the site consist of Vashon till, a dense to very dense deposit <br />comprised of clay, silt, sand, and gravel. Till is generally not a suitable receptor soil for <br />infiltration due to the high fines content and density. Where loosened by weathering <br />infiltration rates of about 'h inch per hour may be obtained. Where unweathered, <br />infiltration rates are typically less than '/ inch per hour. Perched groundwater, which can <br />limit infiltration, also develops in till soils during wet season at the transition from <br />weathered to unweathered soils. In summary, it is our opinion that non -infiltration <br />alternatives should be considered to manage the surface runoff at the site. <br />5.0 GEOTECHNICAL RECOMMENDATIONS <br />5.1 SEISMIC DESIGN PARAMETERS <br />The 2015 International Building Code (IBC) seismic design section provides a basis for <br />seismic design of structures. Table 1 below provides seismic design parameters for the site <br />that are in conformance with the 2015 IBC, which specifies a design earthquake having a <br />2% probability of occurrence in 50 years (return interval of 2,475 years), and the 2008 <br />USGS seismic hazard maps. <br />Table 1 — Seismic Design Parameters <br />Spectral <br />Spectral <br />Site <br />Design Spectral <br />Control Periods <br />Site <br />Class <br />Acceleration <br />at 0.2 sec. [g] <br />Acceleration <br />at 1.0 sec. [g] <br />Coefficients <br />Response <br />Parameters <br />[sec.] <br />F,, <br />F,, <br />Sos <br />Soi <br />To <br />Ts <br />Ss <br />S1 <br />C <br />1.404 <br />0.545 <br />1.000 <br />1.300 <br />0.936 <br />0.472 <br />0.101 <br />0.504 <br />The spectral response accelerations were obtained from the USGS Earthquake Hazards <br />Program Interpolated Probabilistic Ground Motion website (2008 data) for the project <br />latitude and longitude. <br />Liquefaction Potential. Liquefaction is a process that can occur when soils lose shear <br />strength for short periods of time during a seismic event. Ground shaking of sufficient <br />strength and duration results in the loss of grain -to -grain contact and an increase in pore <br />19-049 1515 132nd St SE Page 5 PanGEO, Inc. <br />