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i y Y 4 i 07 January 2004 AGE-NC project No 00-0769 Page 3 of 7- rl In HU-I s I i Based on ground water elevation data collected to HU-1 Upper Zone(25 to S I feet bs the water flow forms a ridge, with the east limb#lowing to the southwest ata g)' ground 0 002 fl/fl and the southerly limb flowing to the east-southeast at a gradient o approximatelyop0 001 ft/ft(Figure 3) f al Based on groundwater elevation data collected in HU-2(112 to 125 feet bsg),the ground water flow forms akndge plunging to the east The northern limb flows to the north-northeast at a'gradient of ' approximately 0 0007 ft/ft and the southern limb flavus to the south-southeast at adle approximately 0 00171t/fl (Figure 4) nt of r s HU-3 Based on ground water elevation data collected in HU-3(140 to 160 feet bs the I k forms a ridge plunging west-northwest The northern limb flows slightly cast ofn h with aagradie t ' of approximately 0 004 ft/ft and the west limb flows to the west at a gradient of approximately 0 002 ft/ft(Figure`5) _ - HU-4 � 1 r r I a l w YI r Based on ground water elevation data collected in HU-4(160 to 175 feetg}the bs ground water flows north-northeast under a gradient of approximately 0 00$ ft/fl (Figure 6) u j, 11 1 I ( I, 1 I, 32 ANALYTICAL RESULTS OF GROUNDWATER SAMPLES I During the February 2003 sampling event, ground water,samples from 31 monitoring wells were collected from HU-1 through HU-5 and submitted for laboratory analysislfor the constituents listed in Section 2 2 Analytical Laboratory;results are summarized in Tables'2-5 ` k f 1 Ground water samples from wells MW-1,' MW-2B, MW-3B,`and "A" wells, MW-4A through MW-9A, were collected from HUI , g i i 1 p r Advanced CeeEovironmentnl,Inc I Ji '