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GEOTECHNICAL ENGINEERING STUDY <br />Inform, Inc <br />May 9, 2002 <br />E-8493-5 <br />Page 3 <br />The underlying native soil consists of silty sand (SM) with localized interbeds of poorly <br />graded sand with silt and gravel (SP-SM), and sandy silt (ML) to the maximum exploration <br />depth of twenty one and one half (21.5). At the boring location B-201 located in the <br />eastern portion of the planned development area, the native soil was medium dense to <br />approximately seven and one half feet below grade. The soil became dense from <br />approximately seven and one half (7.5) to fifteen and one half (15.5) feet, grading to very <br />dense to the maximum exploration depth. in Boring B-202. the native soil was genarally <br />dense to very dense from two (2) to twenty one and one. half 121.5) feet below yrade. <br />However, from eight and one half (8.5) to sixteen (16) feet below grade we encountered <br />medium dense to dense silty sand with a much lower silt c,ontent. <br />Groundwater <br />At the time of our subsurface exploration IApril 2002i, moderate to heavy groundwater <br />seepage was encountered at around five feet below grade to the maximum r:xploration <br />depth at both of our boring locations. The observed seepage appears to bn occurring <br />within interbeds of relatively permeable poorly graded sand within the surrounding lower <br />permeability silty sand. The observed seepage is likely indicative of a seasonal high, <br />perched groundwater condition with groundwater collecting along dense to very dense, <br />low permeability glacial till. Based on our review of the previous boring logs for the <br />existing Safeway Store, the groundwater seepage conditions at the proposed fueling <br />station site appear to be heavier and more extensive. The heavier groundwater seepage <br />conditions are likely due to the presence of the permeable sand interbeds which were not <br />as extensive at the previous boring locations. <br />The contractor should be made aware of the potential for seepage, and understand that <br />groundwater levels are not static. There will Iikeiy be fluctuations in the seepage and <br />groundwater table Ievel depending on the season, amount of rainfall, surface water <br />runoff, and other factors. Generally, the water level is higher and seepage rate is greater <br />in the wetter winter months Itypically Gctober through May1. The presence of <br />groundwater seepage should be expected in the proposed excavation for the underground <br />storage tanks, especially if the excavation is conducted during the wet season. <br />Ennh Cnn�uhnnl�,lnc. <br />