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1-14 ` t 1 ' <br /> 23 December 2003,, <br /> NI <br /> r AGE-NC Project No 97-0333 t I <br /> Page 7 of 1=1 <br /> E downward gradient was observed between the upper and lower Second Zone Near neutral gradients ! <br /> I , were observed at all other locations ' <br /> _1 The 18 August 2003 groundwater elevation data collected from the Rainwater Car Wash site was <br /> plotted for the informal First Zone, Second Zone, Third `Zone and Primary Aquifer Zone f' <br /> hydrogeologic flow units, and are depicted in Figures 4 through 7 <br /> J I <br /> 3 5 1 1 First Zone Aquifer <br /> ' Ground water elevation data collected in the First Zone Aquifer (15 to 47'feet bsg) inferred an <br /> ` inward-radiating ground water flow towards a ground water depression in the area of wells EW-1 <br /> and MW-7A(Figure 4), ground water gradients ranged from 0 007 ft/ft or less to greater than0 025 <br /> ft/ft within the depression I <br /> II <br /> i� F i I <br /> 3 5 12 Second Zone Aquifer a s <br /> Ground water elevation data collected in the Second Zone Aquifer {58 to 92 feet bsg} inferred a <br /> west-northwest ground water flow direction Ground water gradients were approximately 0 001 ft/ft' <br /> 1 or less near,the site (Figure 5) 1 <br /> 1 r II <br /> 35 13 Third Zone Aquifer ' <br /> ;! Ground water elevation data collected in the Third Zone Aquifer (102 to 120 feet bsg) inferred a r E <br /> northwest ground water flow direction Ground water gradients were approximately 0 004 ft/ft or' ` f <br /> I � less near the site (Figure 6) I <br /> rl ' ! <br /> , <br /> 13'5 14 Primary Aquifer Zone I' <br /> c l Ground water elevation data collected in the Primary Aquifer Zone(128 6;150 feet bsg)inferred a <br /> northwest ground water flow�direction Ground water gradients were approximately 0 001 ft/tt or <br /> less'near the site (Figure 7) <br /> II <br /> I II I 7 1 1 t 'I I 1{11'1 <br /> i I i I <br /> r 4 al ! t I I <br /> ' I Ir <br /> Advanced GeoEnvironmental,Inc <br /> r ! I I Ir II I ! t I II r,l ' i 1 �! Ij i' I n !'r I•I ! ! 111 � ' �I <br />