Laserfiche WebLink
1 <br /> roologkal T dmks Im Page 3 <br /> Groundwater Monitoring Report <br /> Project No 770 2 <br /> November 8,2001 <br /> ' • Determine vertical distance between the two measuring devices by the distance from the <br /> mid-point between the top and bottom seal of the deep well (MW-105) and the crud-point <br /> between the groundwater elevation and the bottom seal in the shallow well (MW-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 piezometnc 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 V YX it-0,11� <br /> Figures�& 3 show the location of the well clusters, MW-5/105 and MW-6/106, used for <br /> ' calculating vertical groundwater gradient in this report Table 1 includes Summary of Water <br /> Level and Gradients Water Table Wells, Table 2 includes Summary of Water Level and <br /> Gradients Deep Wells, Table 3 shows the calculated vertical gradients, and Table 6 contains <br />' the well construction details The information used in the calculations is shown 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) /vertical distance) = vertical gradient] <br /> Vertical gradients were calculated for the MW-5/105 & MW-6/106 well pairs for the 3`d <br /> quarter 2004 monitoring events The vertical gradient was negative (a downward direction) <br /> for the MW-5/105 well pair for all five sounding events completed in 2004 The MW-6/106 <br /> well pair vertical gradient was positive (an upward direction) on January 22 and February 26, <br /> and negative (a downward direction) on March 15, June 7, 2004, and August 19, 2004 _ <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 from <br /> —0 02 to 0 0097 for the site investigation <br /> 1.2 Groundwater Sampling Procedure <br />' On August 19, 2004, Del-Tech Geotechnical Support Services staff mobilized to the site to <br /> complete the quarterly groundwater monitoring and sampling of the site's monitoring wells <br /> Before sampling was attempted the wells were sounded for depth to water and then a clear <br />' disposable bailer was used to determine if floating product was present The recharge was <br /> poor in wells MW-5, MW-6, MW-7, and MW-8 However, other wells were purged of at <br /> least three well volumes of stagnant water using a dedicated Waterra check-ball assembly and <br />' '/2 inch tubing Purging continued until the temperature, conductivity and pH of the <br /> groundwater stabilized (<10% variation among three readings) indicating that formation <br />