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Geological rechnks/Ac Page 4 <br /> ' Groundwater Monitoring Report <br /> . Project No 723 2 <br /> March 21,2005 <br /> ' The following procedure is used to calculate vertical groundwater gradient <br /> ❑ Determine vertical distance between the two measuring devices by the distance from the <br /> crud-point between the top and bottom seal of the deep well (MW-201) and the mid-point <br /> ' between the groundwater elevation and the bottom seal in the shallow well (MW-3) <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 /> ' Figure 2 shows the location of the well pairs used for calculating vertical groundwater <br /> gradient in this report MW-3/MW-201, MW-8/MW-108 and MW-108/MW-208 Tables i - <br /> ' 4 show Summaries of Water Level and Gradients Slope and Bearing and Table 6 shows the <br /> calculated vertical gradients 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 /> For the January 2005 event <br /> ' o the vertical gradient for the MW-3/MW-201 pair was negative (or downward) at - <br /> 0 001 ft/ft <br /> o The MW-8/MW-108 and MW-108/MW-208 well sets also displayed downward <br /> ' gradients at -0 001 and -0 03 ft/ft, respectively <br /> o Previous calculations have revealed both positive and negative gradients at the site <br /> ' but additional monitoring is needed to determine long-term trends especially in the <br /> CMTm well sets <br /> ' 1.2 Groundwater Sampling Procedure <br /> On January 27, 2005, Del-Tech Geotechnical Support personnel arrived on-site, opened the <br /> ' wells and measured the depth to water with an electrically actuated sounding tape The water <br /> level readings were recorded to an accuracy of 0 01 feet In wells where free-floating product <br /> is suspected, a clear disposable bailer is used to gauge the interface During this monitoring <br /> ' no free product was noted (this procedure is not exercised in the CMTTM wells due to their <br /> limited diameter) <br /> ' Stagnant water in the well casing was purged using a Waterra pump as recorded in the field <br /> logs (Appendix C) The rate of well purging was monitored The wells were purged of <br /> approximately three casing volumes and until the groundwater parameters (temperature, <br /> conductivity and pH) had stabilized (Appendix C) indicating that water representative of <br />