Laserfiche WebLink
CeofaBicafTmgnics Inc. Page 2 <br /> City of Escalon <br /> Soil&Groundwater Report <br /> Project No. 750.2 <br /> March 15, 1999 p <br /> On February 23, 1999 three boreholes were drilled on site (HP-2, HP-3 & HP-6). The , <br /> boreholes were extended to the capillary fringe. A hydropunch type sampling tool was then <br /> advanced into the ground water to obtain a ground water sample. The depth to groundwater <br /> in this area was approximately 60-61 feet below grade. <br /> After the groundwater samples were collected, the boreholes were closed by pumping a neat <br /> cement grout, containing <4% bentonite to the surface by pumping the grout through the <br /> augers as they were removed from the borehole. <br /> Soil cuttings were added to the existing stockpile. Decontamination rinse water was <br /> !� containerized in DOT approved 55 gallon, steel drums and placed along side the building. <br /> 1.2 Sail Sampling Procedure <br /> During drilling, soil samples were collected for geological and analytical evaluation at five- <br /> foot intervals. Boring logs providing sediment description using the USCS and field <br /> observations were maintained by Ray Kablanow, a California Registered Geologist and <br /> �-+ Certified Hydrogeologist and Michael Niemi, geologist for GTI, working under the <br /> supervision of Ray Kablanow. Boring logs are attached in Appendix B. <br /> Soil samples were collected in 6.0-inch brass liners using a 2.0 inch modified California split <br /> spoon sampler. All soil samples were sealed with Teflon sheets, capped, labeled and placed ' <br /> -� in a cooler at 4° Celsius for transport to the laboratory following Chain of Custody protocol. <br /> Because every soil sample collected was not to be submitted for laboratory analysis, a <br /> screening process was used to gather additional information through field observation. The <br /> following was noted: <br /> sediment type, especially grain size and clay content <br /> 0 moisture content <br /> • visible evidence of contamination, i.e., color change due to reduction of iron or <br /> discoloration from hydrocarbons and other pollutants <br /> readings above background on a organic vapor meter(OVM) <br /> The OVM is a portable photo ionization detector that uses a 10.0 eV lamp to detect <br /> compounds with ionization potential below 10.0 eV (hydrocarbon range). <br /> 1.3 Groundwater Sampling i <br /> I <br /> Once the capillary fringe soil sample was collected, a hydropunch type groundwater <br /> sampling tool was advanced approximately four feet into the saturated zone. The tool was <br /> retracted approximately two feet to expose the screen. A narrow Teflon or stainless steel <br /> bailer was used to recover representative groundwater samples. Care was-taken to minimize <br /> sample agitation from the initial filling of the bailer to the transfer of the sample to the <br /> sample containers. Once the sample container was filled and capped, the bottle was inverted, <br /> tapped, and checked for head space bubbles. The sample container was identified and <br /> labeled with a unique designation, inserted into foam holders and placed in an ice chest <br /> cooled to 4°C for transport to the laboratory. <br /> � G <br />