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GeologicalTechnkslnc. Page 5 <br /> ' Well Installation and Quarterly <br /> Groundwater Monitoring Report <br /> . Project No. 1030.2 <br /> ' June 18,2002 <br /> The detection limits for these compounds are listed in the data table, Table 3 of Appendix <br /> ' A. A Chain of Custody was completed for all samples collected and tracked to ensure <br /> sample integrity. Laboratory data sheets are included in Appendix D. <br /> ' The laboratory data were submitted electronically to GeoTracker as required under AB2886 <br /> on May 16, 2002. The confirmation numbers for the electronic submittal are 1719836235 <br /> ' and 4668563485. <br /> 2.3 Groundwater Investigation. <br /> ' 2.3.1 Groundwater Sampling Procedure <br /> On May 8, 2002, 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 <br /> water level reading was recorded to an accuracy of 0.01 foot. If free floating product had <br /> been suspected, a clear disposable bailer would have been used to gauge the interface. No <br /> floating product was observed during this sampling event. <br /> On June 11, 2002, Del-Tech Geotechnical Support personnel arrived on-site and measured <br /> the depth to water with an electrically actuated sounding tape. The water level reading was <br /> recorded to an accuracy of 0.01 foot. The depth to water measurements taken on May 8, <br /> ' 2002, indicated that the groundwater bearing had changed dramatically. The faulty result <br /> was due to a computer error on the field logs from Del-Tech Geotechnical Support. <br /> Accurate measurements (Table 1) and field logs (Appendix C) are attached. <br /> ' Stagnant water in the well casing was purged using a dedicated Waterra pump. The rate of <br /> well purging was monitored. The well was purged of at least three casing volumes and also <br /> ' until the groundwater parameters (temperature, conductivity and pH) had stabilized <br /> (Appendix C) indicating that water representative of actual aquifer conditions was entering <br /> the well. Groundwater parameter stabilization was characterized by three successive <br /> ' readings within 10%. <br /> Before a sample was collected, the well's water level was allowed to recharge to at least <br /> ' 80% of its initial level. All water removed from the monitoring well and not used as a <br /> sample was placed in a 55 gallon DOT approved container that is properly labeled and <br /> temporarily stored on-site. <br /> A dedicated Waterra pump was used to collect each sample. Pump cleanliness was assured <br /> ' by collecting a bailer blank (pouring distilled water through the pump and collecting it in a <br /> VOA vial) prior to collecting the analytical sample. <br />