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1 <br /> Geologual recluucs Inc Page 3 <br /> Groundwater Monitoring Report <br /> Project No 770 2 <br /> . April 30,2003 <br /> point between the groundwater elevation and the bottom seal in the shallow well (MW- <br /> 5) g ( <br /> 5) <br /> • Measure the head in both wells used in the calculations <br /> • If the lateral distance between the well pair is greater than a few feet, then calculations <br /> must be made to correct the down-gradient piezometric head to account for the sloping <br /> water table between the wells The calculation considers the slope of the water table and <br /> the distance in a down-gradient direction between the two wells used in the calculations <br /> 1 Figures�A &2B show the location of the well clusters, MW-5/105 and MW-6/406, used <br /> for calculating vertical groundwater gradient in this report Table 1 includes Summary of <br />' Water Level and Gradients Water Table Wells, Table 2 includes Summary of Water Level <br /> and Gradients Deep Wells, Table 3 shows the calculated vertical gradients, and Table 6 <br /> contains the well construction details The inforination used in the calculations is shown <br /> below <br />' Vertical gradient calculation formulas are as follows <br /> • Vertical correction for gradient [(gw gradient slope) x (distance) = vertical correction] <br /> • Vertical head [(head of deep well) - (head of shallow + correction) — vertical head] <br /> • Vertical gradient [(vertical head) I vertical distance) =vertical gradient] <br /> Vertical gradients were calculated for the MW-5/405 & MW-6/406 well pairs for both 0 <br /> quarter 2002 monitoring events The vertical gradient was positive (an upward direction) <br /> for the MW-5/-105 well pair on November 19 and negative (a downward direction) for the <br /> December 18 event The MW-6/406 well pair vertical gradients were the opposite of the <br /> MW-5/405 well pair for the two events These wells' gradients were negative (a <br /> downward direction) on November 19 and positive on December 18 <br /> Both positive and negative vertical gradients have been calculated for previous events <br /> Similar to the historical lateral directions, the direction of groundwater in the vertical plane <br /> also fluctuates at the site The magnitude of vertical groundwater flow direction ranged <br /> from—0 02 to 0 0097 for the last five monitoring events <br /> 1.2 Groundwater Sampling Procedure <br /> r <br /> On November 19, 2002, Don Light of Del-Tech Geotechnical Support Services mobilized to <br />' the site to measure depth to groundwater in the site's monitoring wells <br /> On December 18, 2002, Mr Light returned to the site to complete the quarterly groundwater <br /> r monitoring and sampling of the site's monitoring wells Before sampling was attempted the <br /> wells were sounded for depth to water and then a clear disposable bailer was used to <br /> . determine if floating product was present No free product was noted for the event however <br /> r <br /> r <br />