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Geoingccd 7'echnas ltic Page 3 <br /> 3"'Quarter 2003 61oundwatet Moiiitosinb Repast <br /> Projeo No 507 2 <br /> Novciiibei 13, 2001 <br />' water table between the wells The calculation considers the slope of the water table and <br /> the distance in a down-giadient direction between the two wells used in the calculations <br />' J calculating the vertical groundwater <br /> Figure 2 shows the ]oc.ation of the well cluster used for c g <br />' gradient in this report, MW-9 and MW-109 Table 1 shows Summary of Water Level and <br /> Gradients Slope and 13earuig, and Table 2 shows the calculated vertical gradients The <br /> information used in the calculations is shown below <br /> Vertical giadicnt i,ah ulation formulas are as follows <br /> • Vertical -oi i e0ion toi gi adient [(gw gradient slope) x (distance) = vertical correction] <br />' • Vertical head [(head o I sleep well) - (head of shallow+ correction) = vertical head] <br /> Veitical gi adient [(vee ticat head) / (vertical distance) = vertical gradient] <br /> For the Septembei 2003 moiiitoting event a vertical gradient was calculated for the MW- <br /> 9/MW-109 paii 'I lie veitical giadient was negative (a downward direction) at 0 004 ft/ft <br /> and approximately I I times the inagnitude of the horizontal gradient of the water table <br /> (0 003) <br /> 1.2 Groundwatei Sampling Piocedure <br /> On Septeiiibei 11, 2003, Doti Light of Del-Tech mobilized to the site to conduct <br /> groundwatei monitoring of the site's eleven monitoring wells Before sampling was <br /> attempted, the wells were sounded for depth to water and then a clear disposable bailer was <br /> used to detem mic if1loatnig pioduct was present No free product was noted for this event <br /> The wells weds puttied of tit least three well volumes of stagnant water using a dedicated <br /> Wateita cheld,,-ball assembly and '/2 inch tubing Purging continued until the temperature, <br /> conductivity, find 1+1 of the gioundwater stabilized (<10% variation in three consecutive <br /> icadings), indicating that formation water representative of aquifer conditions was entering <br /> the wells These water duality parameters were measured at intervals of each well volume <br /> purged <br />' Once purging was complete, a water sample was collected from the Waterra tube Care was <br /> taken to minimize sample agitation Once the sample container was filled and capped, the <br />' bottle was invei led, tapped and checked for headspace bubbles The sample container was <br /> identified and labeled with a unique designation, inserted into a foam holder and placed into <br />' an ice chest t oolcd to 4°C 1oi tiansport to the laboratory <br /> All non-disposable Sampling equipment was decontaminated using a hot water washer and <br /> detergent Mote and between uses Disposable gloves were used by the technician to <br /> collect all samples anti wei c changed with each sample collection <br /> 1 <br />