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i <br /> PROBLEM ASSESSMENT REPORT <br /> 1 605 South EI Dor.do Street Stockton California <br /> Based on water levels observed during drilling, perforated casing was set from 40 to <br /> 60 feet bs in wells MW-4, MW-5 and MW-7, and from 35 to 55 feet bs in well MW-6 <br /> Each of the wells was capped with a locking wellhead cap and secured by a water- <br /> tight, traffic-rated wellhead vault The top-of-casing elevation, above mean sea level, <br /> of each well was surveyed based on a City of Stockton benchmark <br /> In the vapor extraction wells, perforated casing was set from 5 to 15 feet bs in <br /> VEW-1 , within the former UST backfill, and 15 to 35 feet bs in VEW-2 Each of the <br /> wells was capped with a locking wellhead cap and secured by a water-tight, traffic- <br /> rated wellhead vault <br /> The groundwater monitoring wells were surged and developed with a 10-foot-long <br /> baler on the drilling rig prior to placing the bentonite seal The wells were developed <br /> by purging each of approximately 55 gallons, until the water ran relatively clear Well <br /> development water was stored temporarily on site in DOT-approved, 55-gallon drums, <br /> pending laboratory analysis of the groundwater samples <br /> 3 4 Groundwater Levels <br /> On June 21 , 1993, Aegis personnel collected depth-to-groundwater measurements <br /> from all wells associated with the site Based on data from the previously-existing <br /> wells (MW-1 through MW-3), water levels have risen approximately 1 4 feet since <br /> March 25, 1993 (Figure 6) The June 1993 measurements indicated depth-to- <br /> groundwater ranged from 42 15 to 44 76 feet bs, corresponding to groundwater <br /> Ielevations ranging from 31 27 to 31 43 feet below mean sea level <br /> Figure 7 is a potentiometric surface map of the shallow water-bearing zone on <br />' June 21 , 1993 Based on this map, groundwater is estimated to flow to the east- <br /> northeast at an average gradient of approximately 0 001 ft/ft The March 1993 <br /> measurements indicated an average groundwater gradient of 0 001 ft/ft to the east <br /> Previous groundwater levels are summarized in Table 5 All groundwater elevation <br /> measurements were made from the referenced wellhead elevations, measured to the <br /> nearest 0 01 foot, and conducted according to the Aegis SOP included as Appendix A <br /> 3 5 Groundwater Sampling and Analysis <br /> On June 21 1993 Aegis personnel collected groundwater samples from all wells <br /> (MW-1 through MW-7) associated with the site The samples were delivered under <br /> chain-of-custody to PACE The samples were analyzed for concentrations of <br /> • TPH, as gasoline by EPA Method 8015 <br /> • BTEX by EPA Method 8020 <br /> 91 044A PAR 7 <br /> i <br />