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Ik � <br /> Soil and Groundwater Investigation <br /> Quik Stop No 121 <br /> Page 4 <br /> Subsurface soils were explored to depths ranging from 22 to 30 feet Continuous "direct push" cores <br /> were collected at each of the five sample locations by pushing a small diameter drive casing (3-inch <br /> outside diameter) from the surface to the total depth of each borehole Continuous soil cores were <br /> collected using a 3-foot long small diameter inner sample barrel lined with buterate tubing and 3-foot <br /> sections of A-rod After each 3-foot sampling run,the inner sample barrel containing three soil cores <br /> were removed from the hole The drive casing remained in the ground to prevent the borehole from <br /> collapsing and to prevent cross-contamination of subsequent soil samples In addition, the drive <br /> casing also prevents the entry of light nonaqueous phase liquid (LNAPL) into the borehole, which <br /> could contaminate groundwater in deeper zones Once the sample barrel was removed from the <br /> borehole, it was placed on a table and the 3-foot long buterate tubing containing a 3-foot core section <br /> was removed The soil inside the transparent tubing was then logged and selected 6-inch samples <br /> were then cut, capped with Teflon sheets and plastic caps, labeled, logged on a chain-of-custody <br /> form and stored in a chilled ice chest for preservation in the field and during transport to a state- <br /> certified laboratory CCI's soil sampling protocol is attached in Appendix A <br /> Grab groundwater samples were collected by installing 1-inch diameter PVC tubing into the open <br /> borehole Five to 10 feet of 0 010 slotted tubing was attached After allowing the water to <br /> equilibrate within the tubing, groundwater samples were collected using a '/z-inch diameter, <br /> stainless steel bailer equipped with a small ball valve Each groundwater sample was collected in <br /> appropriate laboratory-supplied bottles, labeled, logged on a chain-of-custody form and stored in a <br /> chilled ice chest for preservation in the field and during transport to a state-certified laboratory <br /> CCI's groundwater sampling protocol is attached as Appendix A <br /> During the investigation it was noted that groundwater was generally encountered at approximately <br /> 15 feet below the ground surface (bgs) At all five sample locations, groundwater flowed freely into <br /> each boring It should be noted that groundwater was not encountered until 20 feet at sample <br /> location GP-5 The groundwater at this location was under confined conditions and immediately <br /> rose to approximately 15 feet bgs <br /> Upon completion of the sampling at each GSS location, the holes were sealed with Portland cement <br /> using the l-inch PVC tubing as a tremmie pipe The cement was displaced to the surface, allowed <br /> to settle, topped-off, and the surface hole was then sealed with cold patch asphalt <br /> Subsurface Soil Conditions <br /> CCI explored subsurface soils to depths of 22 to 30 feet in the five GCCS locations In general, the <br /> upper 8 feet of soil encountered at the subject site consisted of brown to yellow-brown, silty sand <br /> The only exception was at GP-1,which was direct-pushed through the former tank excavation area <br /> and consisted of pea-gravel to a depth of 14 feet Below 9 feet, the subsurface soils became more <br /> granular, consisting of a yellow-brown, fine-to-coarse grain sand A sample (GP-2-15) was <br />