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i <br /> I Subsurface£xplora[ion, Geologic Hazard, and <br /> Sno-lsle Ski(Is Center Addition Preliminary Geotechnica!Engineering Repon <br /> Everett, Washington Geologic Hazards and Mitigmions <br /> Iturbidiry reading is 25 NTU or lower. If the monitored turbidity exceeds 250 NTU, the resulu <br /> must be reported to Ecology within 24 hours and corrective action taken. Daily turbidity <br /> Imonitoring is continued undl the corrective action lowers the turbidiry to below 25 NTU. <br /> I In order to meet U►e current Ecology requiremenu, a properly developed, constructed, and <br /> maintained erosion control plan consistent with the City of Everett standazds and best <br /> management erosion conuol practices will be required for this project. AESI is available to <br /> I assist the project civil engineer in developing site-specific erosion conVol plans. Based on past <br /> experience, it will be necessary to make adjustments and provide additional measures to the <br /> TESC plan in order to optimize its effectiveness. Ultimately> the success of the TESC plan <br /> � depends on a proactive approach to project planning and contractor implementation and <br /> maintenance. <br /> I The erosion hazard of the site soils is low. The most effective erosion conuol measure is the <br /> maintenance of adequate ground cover. Maintaining cover measures atop disturbed ground <br /> provides the greatest reduction to the potential generation of turbid runoff and sediment <br /> I transport. During the local wet season (October 1° tluough Mazch 31°), exposed soil should <br /> not remain uncovered for more than 2 days unless it is actively being worked. Ground-cover <br /> I measures can include erosion control matting, plastic sheeting> straw mulch, crushed rock or <br /> recycled concrete, or mature hydroseed. <br /> � Flow-convol measures aze also essential for collecting and controlling the site runoff. Flow <br /> paths across slopes shouid be kept to less than 50 feet in order to reduce the erosion and <br /> sediment vansport potential of concentrated flow. Ditclilswale spacing will need to be <br /> I shortened with increasing slope gradient. Ditches and swales that exceed a gradient of about <br /> 7 to 10 percent, depending on theit flow length, should have properly constructed check dams <br /> installed to reduce the flow velociry of the runoff and reduce the erosion potential within the <br /> � ditch. Flow paths that aze required to be constructed on gradients between 10 to 15 percent <br /> should be placed in a riprap-lined swale with the riprap properly sized for the flow conditions. <br /> Flow paths constructed on slope gradients steeper than 15 percent should be placed in a pipe <br /> � slope drain. AESI is available to assist the project civil engineer in developing a suitable <br /> erosion conttol plan with proper flow control. <br /> � Some fine-graioed surface soils aze the result of natural weathering processes that have broken <br /> down pazent materials into their mineral componenu. These mineral components can have an <br /> inherent electrical chazge. Electrically chazged mineral fines will attract oppositely chazged <br /> particles and can combine (flocculate) co form lazger particles that will settle out of suspension. <br /> The sediments produced during the recent glaciation of Puget Sound aze, however, most <br /> commonly the suspended ��sls that are carried by site storm water. The fine-grained fraction <br /> of the glacially derived soil is referred to as "rock flour," which is primarily a silt-sized <br /> particle with no electrical chazge. These particles, once suspended in water, may have settiing <br /> i <br /> times in periods of months, not hours. <br /> �une�1 z008 ASSOCIATED EARTN SCIENCES,INC. � <br /> ( EGad-F�'OB0113A5-Prolen11I0W02731FPIWP Page 7 <br /> I <br />