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r <br /> (MW-1, MW-2, MW-3 and MW-4 respectively) installed on site The elevation of groundwater <br /> rin MW-1, MW-2, MW-3 and MW-4 was calculated by EI to be at 17 08, 17 58, 17 12 and 17 22 <br /> • feet below mean sea level respectively, based upon casing elevation data from Kier & Wright <br /> rCivil Engineers and Surveyors <br /> r30 FINDINGS <br /> r3.9 Groundwater Level Measurements <br /> The elevation of groundwater in MW-1, MW-2, MW-3 and MW-4 was calculated by El to be at <br /> r30 10, 31 00, 29 96 and 29 57 feet below mean sea level respectively on 25 June 2002 _ <br />' El utilized the groundwater measurements to determine the direction of groundwater flow and <br /> the groundwater gradient present beneath the surface The groundwater direction of flow for the <br />' area was inferred northerly at a gradient of 0 002 ft/ft to 0 005 ft/ft <br /> The groundwater elevation at the site increased an average one (1)foot between March 2002 and <br />' June 2002 The gradient increased slightly during that period <br /> Groundwater elevations are listed in Table 1,-and shown graphically in Figur X s� <br />' 3.2 Groundwater Sample Analysis Results <br /> The groundwater was sampled on 25 June 2002 1\4W-1 continued to show diesel contamination <br /> at a level similar to that found in the previous quarter Gasoline contamination, however, has <br /> decreased No MTBE or BTEX was evident kb, 4AAJ�10 b Uf..A'OX `� \Ut t- �- y4ly nta 0 <br /> J'PY` <br /> MW-2 shows significant motor oil contamination as well as moderate contamination from diesel <br /> Minor contamination from gasoline, oxygenates and BTEX remains, but no MTBE <br /> contamination <br /> MW-3 is free from contamination once again <br /> MW-4 continued to showed gasoline, BTEX, DIPE and diesel contamination as well as an <br /> appearance of ethyl benzene and total xylenes contamination <br /> 1 <br /> All groundwater samples secured by EI were logged in a chain-of-custody form, placed in an on- <br /> Environeenng,Inc Project No 02.00716 page 3 <br />