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a <br /> sandpack from approximately 15 feet below grade to approximately 34 feet below grade, the <br /> depth of completion The interior of the casing was packed with native soil due to sloughing <br /> of the excavation sidewalls into the open casing Efforts to remove the blockage were <br /> unsuccessful The licensed drilling contractor and RESNA personnel determined that the most <br /> practical and effective method to abandon the well was to proceed with backfilling activities, <br /> attaining 90% compaction, and subsequently repave the site These actions would effectively <br /> prevent any vertical migration of contaminants to the subsurface via the well remnant <br /> However, pursuant to on-site direction by PHS/EHD, RESNA placed a temporary conductor <br /> casing over the well remnant to provide access at a later date for overdrilling of the remaining <br /> portion of the well A 10-inch diameter steel conductor casing was placed over the well <br /> remnant using the excavator tractor Backfilling activities proceeded around the emplaced <br /> conductor casing <br /> On January 4, 1995, Spectrum Exploration Inc attempted to overdrill well remnant MW1 <br /> through the conductor casing for the purposes of installing a replacement well The well was <br /> overdrilled, but efforts to install a replacement well in the same location were unsuccessful due <br /> to unstable and shifting fill material The void created by overdrilling the well was filled with <br /> neat cement grout A replacement well (MW1R) was installed immediately east of the <br /> excavation pit on January 12, 1995 The location of the replacement well is shown on the site <br /> plan, Figure 2 The boring log and well construction details are depicted on Figure 3 <br /> GROUNDWATER MONITORING AND SAMPLING <br /> A RESNA technician measured the depth to groundwater in monitoring wells MWIR, MW2, <br /> MW3, and MW4 on January 17, 1995 using an electronic water level probe Groundwater <br /> was present in site wells at 12 34 to 14 39 feet below surface grade Groundwater generally <br /> flows to the southeast across the site A potentiometric surface map of the shallow water <br /> bearing zone is shown on Figure 4 The apparent groundwater mound around replacement <br /> well MW IR can be attributed to residual effects of recharge while the excavation was open to <br /> the elements Future trends in groundwater gradient will be monitored closely Groundwater <br /> monitoring data are summarized in Table 1 <br /> Subsequent to water level measurements, well MWIR was developed by pumping and hand <br /> bailing approximately 70 gallons of water Physical parameters (pH, conductivity, <br /> temperature) were monitored and allowed to stabilize prior to sampling The well purge log <br /> and groundwater monitoring data are included in Attachment 2 <br /> Groundwater samples were collected from well MWIR using a disposable bailer The samples <br /> were placed immediately on ice and transported to Argon Mobile Labs (DHS Cert #1873) and <br /> analyzed for benzene, toluene, ethylbenzene, and xylenes (BTEX), TPHg and total petroleum <br /> hydrocarbons as diesel (TPHd) using EPA methods 8020/8015 modified TPHg, xylenes, and <br /> 1500591SR051095 doc 2 <br />