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1 - <br /> • Hydrological Unit 2(HU2)extends from 45 to approximately 75 feet bsg,11U2 is composed <br /> • of sand, with minor layers of silt and cemented sand The interval is characterized by low <br />' pore pressure <br /> • Hydrological Unit 3 (HU3) extends from 75 to 113 feet bsg, and is dominantly composed of <br />' silt, clay and stiff, fine-grained intervals Unit 3 is charactenzed by a fluctuating range of <br /> pore pressures, varying from low to medium low <br /> • Hydrological Unit 4 (HU4) extends from 113 feet bsg to 117 feet bsg, and is composed of <br />' sand The interval 2s characterized by low pore pressures <br /> • Hydrological Unit 5 (HU5)extends from 117 feet bsg to total depth, and is composed of silt <br />' The interval is characterized by increasing pore pressures, from medium low at <br /> approximately 117 feet bsg to high at total depth of 147 feet <br />' Cross sections A-A' and B-B' depicted general lithology beneath the site The hydrological units are <br /> depicted in cross sectional views A-A' and B-B' <br /> I <br /> HYDROCARBON IMPACTED SOIL AND CONTAMINANT MIGRATION <br />' The mayor source of soil contamination was the former gasoline UST located at the western edge of <br /> the main office building <br /> 1• A release of petroleum hydrocarbons occurred from the former gasoline UST Hydrocarbons <br /> were detected at concentrations as high as 5,800 mg/kg Available data is suggestive of <br />' discharge at the western edge former gasoline UST area <br /> • Once released to the subsurface, the contaminants migrated to a vertical depth of <br /> approximately 40 feet bsg(MW-6),at which point the contaminants migrating locally down <br /> to a depth of 85 feet bsg(CPT1-85) The contaminants migrated east and northeast from the <br /> former UST area, under the building at the site, to a then vertical depth of approximately <br /> I 40 feet bsg,where the variation concentration in soil samples suggest a smear zone between <br /> 35 feet and 40 feet bsg Low concentrations of impacted soil was only detected at greater <br /> than 30 feet bsg in downgradient monitoring well pilot boring samples <br /> • The highest impact to soil in the upper vadose zone is present at boring MW-6 The highest <br /> impact to soil near the water table and below the water table to a depth of 85 feet bsg occurs <br /> inthe area of bonng MW-6 and CPT1 Soil samples collected from the a depth of 30 feet bsg <br /> had concentrations of TPH-g (4,100 mg/kg), benzene (17 mg/kg) and EDB/1,2-DCA <br /> (460 mg/kg/410 mg/kg), which represents the core of the impacted soil <br /> • TPH-g were detected in ground water samples collected from wells on the site, at <br /> concentrations as high as 150,000 µg/1 from the ground water extraction well in the former <br /> UST excavation TPH-g-impacted shallow ground water has been defined,with only minor <br /> concentration detected in well MW-3, north of the former UST <br /> IAdvanced GeoEnnronmental,Inc <br />